2018년 고생물학
2018 in paleomammalogy
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이 고생물 목록에는 2018년에 기술된 새로운 화석 포유류 분류군과 그 해에 발생한 다른 중요한 고생물 발견 및 사건들이 기록되어 있다.
포유류 일반
- Jones et al. (2018)[1]는 비맘마적 시냅시드에서 척추 영역의 형태학적 다양성과 포유류 척추의 해부학적으로 다른 영역의 진화를 설명하기 위한 의미에 대한 연구를 발표했다.
- 포유동물 턱의 진화에 대한 연구는 라우텐슐라거 외 연구진(2018)에 의해 발표되었으며, 라우텐슐라거 외 연구진(2018)은 시노돈-모말리아 변환에서 주요 [2]비모말리아포름 분류군에서 동시에 턱관절 스트레스의 감소와 물어뜯는 힘의 증가에 대한 증거를 찾지 못했다.
- Crompton 외 연구진(2018)[3]은 현존하는 화석 포유동물과 비유상종 신노돈트의 데이터를 기반으로 한 단핵, 다핵동물 및 유골의 뇌 측벽 구조와 기원에 관한 연구를 발표했다.
- 포유류에 의해 건설되었을 가능성이 가장 높은 것으로 해석되는 척추동물의 굴은 새로운 이치노탁사 다이모넬릭스 마르티니와 프랙티세미타(후자는 사회성 있는 포유동물의 [4]굴을 나타내는 것으로 보이는)의 이름을 붙인 Raisanen & Hassiotis(2018)에 의해 상부 쥐라기 모리슨 층의 소금물 구성원(Utah, 미국)에서 기술되었다.
- 피레스 외 연구진(2018년)[5]은 백악기/팔레오겐 경계를 넘어 북미의 3대 포유류 군락(다중결핵, 메타테리어 및 유태인)의 다양화 역학에 관한 연구를 발표했다.
- Hell Creek [6]층과 포트 유니온 층의 툴록 멤버(미국 몬타나)의 4개 지역 데이터를 기반으로, 가장 이른 고생대 생물 회복 기간 동안 포유류의 동물 구성과 구조 변화에 대한 연구가 스미스 외 연구진(2018)에 의해 발표되었다.
- Leslie et al.(2018)[7]는 산후안 분지를 가로지르는 To2와 To3 물질 사이의 포유동물 교체에 대한 고해상도 연령 모델을 제시한다.
- 지난 125,000년에 걸친 5개의 기간에 걸친 포유류의 멸종 선택성, 대륙 크기 분포, 분류학적 다양성에 대한 연구는 Smith et al. (2018)에 의해 발표되었으며, Smith et al. (2018)는 더 큰 종의 포유류가 멸종 위기에 처해있다는 증거를 보고하였다.제4기 말기, 그리고 이 시기의 포유류 멸종 크기 선택성은 지난 6500만년 동안 포유류의 진화에서 [8]전례가 없는 것이었다.
- Kouvari & van der Geer(2018)[9]는 플라이스토세 후기와 홀로세기에 멸종된 섬 풍토 포유류 종과 그 체질량, 섬의 크기, 그리고 군도에 인간이 최초로 도착한 것 사이의 관계에 대한 연구를 발표했다.
- Castro-Insua 등(2018)[10]은 포유류의 다양화와 기후 틈새 진화 사이의 관계에 대한 연구를 발표했다.
- Tejada-Lara et al.(2018)[11]는 현존하는 나무늘보와 화석 나무늘보에 초점을 맞추고 단일 동위원소 농축 패턴이 모든 초식 포유류에게 유지된다는 가설을 평가하는 초식 포유류의 조직에 기록된 식이 동위원소 시그니처에 관한 연구를 발표했다.
- He et al.(2018)[12]은 신생대 동안 중국 내 포유류 동물군의 공간적 분화의 시간적 변화와 중국에서 현대적 공간구조화 포유류 동물군의 출현 시기에 관한 연구를 발표했다.
- Beck & Baillie(2018)[13]는 조상 또는 근조모형을 보존하는 화석 포유류의 발견이 포유류의 계통 발생의 형태학적 추정과 분자적 추정 간의 차이 해결에 미치는 영향에 관한 연구를 발표했다.
메타테리안
- Bennett 등(2018)[14]에 의해 새로운 메타테리언 화석 발생 데이터셋을 기반으로 시간에 따른 메타테리언의 글로벌 다양성 변화에 대한 연구가 발표됐다.
- Eodelphis Browni로 언급되는 새로운 치아 화석에 대한 설명과 스태건티드의 십이지장 적응의 진화에 대한 연구는 Brannick & Wilson(2018)[15]에 의해 온라인에 게재되었다.
- 남미 중생대 육식동물 길드의 구조에 대한 스파라소돈트의 형태학적 다양성과 그 의미에 대한 연구는 Croft et al.(2018)[16]에 의해 발표되었다.
- 팔로세 산타루시아층(볼리비아)의 알코키루스 오스트랄리스 두개골 부분과 이 종의 계통발생 관계에 대한 연구는 새로운 메타테리아의 슈퍼오더인 푸카델피다(Pucadelphyda)[17]로 명명된 de Muizon et al.(2018)에 의해 발표되었다.
- 호주 본토 태즈메이니아 데빌 화석의 나이와 호주 본토에서 두 종의 멸종 시기를 추정하는 데 미치는 영향에 대한 연구는 White et al.(2018)[18]에 의해 발표되었다.
- 화이트, 미첼, 오스틴(2018)[19]은 플라이스토세 후기와 홀로세 동안의 태아신 계통 지리학과 인구학적 역사에 대한 연구를 발표했다.
- 멸종된 본토와 현존하는 태즈메이니아 개체군을 대표하는 202마리의 게놈에 기초한 지난 30,000년 동안 호주 남부 태즈메이니아 데빌의 계통지리와 인구통계학적 역사에 대한 연구는 Brüniche-Olsen et al.(2018)[20]에 의해 발표되었다.
- Palaeopotorous Priscus의 계통발생적 관계에 대한 연구는 den Boer & Kear(2018)에 의해 발표되었으며, 이들은 이 분류군을 비대식동물성 [21]대식세포상 유대류로 해석하고 있다.
- 가나와마야와 남바루에 속하는 캥거루 화석의 분류학적 현황 수정은 버틀러 외 연구진(2018년)에 의해 발표되었으며, 버틀러 외 연구진도 가나와마야 쿠페리(옛 남바루속)와 가나와마야 아크리스,[22] 가나와마야의 새로운 화석 물질을 기술하고 있다.
- 지난 2500만 년 동안 캥거루의 진화에 대한 연구는 화석 이빨의 데이터를 바탕으로 쿠젠스 & 프라이도(2018)[23]에 의해 발표되었습니다.
- Thylacoleo carnifex의 골격에서 지금까지 누락된 요소에 대한 설명과 이 종의 두개골 후 골격의 해부학과 생체역학에 대한 연구는 Wells & Camens(2018)[24]에 의해 출판되었다.
| 이름. | 참신성 | 상황 | 작가들 | 나이 | 구성 단위 | 위치 | 메모들 | 이미지들 |
|---|---|---|---|---|---|---|---|---|
| 제너레이션 등 sp. nov. | 인쇄중 | 엥겔만, 아나야 & 크로프트 | 혼다 그룹 | 스파라소돈타의 일원.렙토그나투스속은 새로운 종을 포함한다.2018년에 발표, 2020년에 게재 예정인 기사의 최종판. | ||||
| 제너레이션 등 sp. nov. | 유효한 | 카르네이로, 올리베이라 & 고잉 | ||||||
| 제너레이션 등 sp. nov. | 유효한 | 카르네이로 | ||||||
| 제너레이션 등 sp. nov. | 유효한 | 엥겔만 외 | ||||||
| 제너레이션 등 sp. nov. | 유효한 | 초르노굽스키 외 | 중기 에오세 | 보나파르트헤리오상과와 프리피돌로피모르피아과에 속하는 폴리돌로피모르피아.이 속은 새로운 종인 C. cardonensis를 포함한다. | ||||
| 제너레이션 등 sp. nov. | 유효한 | 코헨 | 백악기 후기(터키) | 사슴과의 일원입니다.이 속은 새로운 종(F. pulveris)을 포함한다. | ||||
| 제너레이션 등 sp. nov. | 유효한 | Métais 등 | 중기 에오세 후기 | 우준차르시데레층 | 허페토테리아과의 일원입니다.모식종은 G. minor이다. | |||
| 11월 1일 | 유효한 | 카스 | ||||||
| 제너레이션 등 sp. nov. | 유효한 | 코헨 | 백악기 후기(터키) | 사슴과의 일원입니다.이 속은 새로운 종인 H. praeceps를 포함한다. | ||||
| 제너레이션 등 sp. nov. | 유효한 | 궁수 등 | 새로운 미니포스무과(Minipossumidae)에 속하는 팔랑게리다의 일원입니다.모식종은 M. notioplanetes이다. | |||||
| 제너레이션 등 sp. nov. | 유효한 | Métais 등 | 중기 에오세 후기 | 우준차르시데레층 | 아나톨리델로피스의 친척입니다.모식종은 O. nauta이다. | |||
| 11월 1일 | 유효한 | Travouillon & Phillips | 늘라보 평원 | |||||
| 제너레이션 등 sp. nov. | 인쇄중 | 고잉 등 | 아마도 폴리돌로피모르피아의 일원일 것이다.이 속은 새로운 종인 P. 에코포스를 포함한다.2018년에 발표, 2020년에 게재 예정인 기사의 최종판. | |||||
| 11월 1일 | 유효한 | 맥주 등 | 리버슬리 사이트 | 웜뱃. | ||||
| 11월 1일 | 유효한 | 카르네이로 | 스파라소돈타의 일원일 수도 있습니다. |
유테리아인
- Gearty, McClain & Payne(2018)[38]은 생물 및 화석 포유류의 체질량 데이터를 바탕으로 수중 포유류의 신체 크기 증가 원인에 대한 연구를 발표했다.
- Miosene Cerro Azul층(아르헨티나)의 대형 포유동물의 굴에 대한 연구는 Cardonatto & Melchor(2018)[39]에 의해 발표되었다.
- 헴필리호스 말갈매기, 다이노히푸스 멕시코, 프로토히푸스 기들레이, 곰포테리움 혼드렌시스, 산헤라르도 데 리모니시토(코스타리카)의 라마 헤미아우체니아 베라의 식단과 서식지에 대한 연구가 페레즈페에 의해 발표되었다.
- 카야 외 연구진(2018년)[41]은 네오겐의 구세계 사바나에 사는 포유동물 동물들의 진화와 상호 연관성에 대한 연구를 발표했다.
- 1500만 년에서 200만 년 전 이베리아 반도에서 온 포유류의 종 다양성 변화와 그 종 다양성에 영향을 미치는 다양한 요인의 조절 역할에 대한 연구는 칸탈라피에드라, 도밍고 & 도밍고(2018)[42]에 의해 발표되었습니다.
- 마케도니아 자연사 박물관 스코페에 보관된 화석으로 알려진 마케도니아 공화국의 미오세 포유류 동물군의 체계적 개정판은 Spassov et al.(2018)[43]에 의해 출판되었다.
- 화석이 있는 지층의 고자기 연대와 시닝 분지(중국 티베탄 고원)의 마이오세 후기 포유동물 화석에 대한 연구는 헨 외 연구진(2018)[44]에 의해 발표되었다.
- 믿음이(2018년)는 건조 지수, 화석 포유류 치아의 산소 동위 원소의 작문 일부 분류 군에게 술 마시는 행동(치아에 영향을 주는 산소 동위 원소 조성)식생활 개선보다는 물 부족에 의해 비롯된 것도 변경된다고 주장하는 지역 paleoclimate과 물 부족을 복원하는 널리 사용되는 기술을 측정한다.[45][46][47]
- 북와(우간다) 마이오세 유적지의 포유류 동물군의 개정과 이 동물의 나이에 대한 연구는 코트 외 연구진(2018)에 의해 발표되었으며, 코트 외 연구진은 이들의 발견을 2000만 년에서 1900만 [48]년 사이에 동아프리카에서 상당한 동물군 교체가 일어났을 수 있음을 시사하는 것으로 해석했다.
- 플리오센과 플라이스토세의 오모-투르카나 분지(동아프리카)에서 대형 포유류의 종과 속 수준의 다양성의 변화에 대한 연구는 Du & Alemseged(2018)[49]에 의해 발표되었다.
- 곤돌린 동굴(남아공)의 이른바 GD A 동물 집단에 대한 일차적인 설명과 분석은 애덤스(2018)[50]에 의해 출판되었다.
- Uno et al.(2018)[51]는 치아 마모와 화석 치아의 안정적인 동위원소 데이터로 알 수 있듯이 올두바이 협곡(탄자니아)의 플라이스토세 퇴적물에서 나온 대형 포유동물의 식단에 관한 연구를 발표했다.
- 올도완 현장 HWK EE(탄자니아 올두바이 협곡)에서 가장 풍부한 유제 분류군의 식단에 대한 연구는 치아의 마모와 안정적인 동위원소 분석으로 나타난다. (2018)[52]
- 올두바이 협곡 유적지의 새로운 포유동물과 어류에 대한 설명은 이 유적지의 포유동물 집단을 현재의 세렝게티 포유동물 군집과 비교하며, 약 170만-140만 년 전에 이 유적지의 고생태학적 재구성에 대한 의미에 대한 연구는 비비 외 연구([53]2018)에 의해 출판되었다.
- Pires et al.(2018)[54]는 현존 및 멸종한 포유동물의 종자 분산 거리와 플라이스토세 메가파우나의 멸종이 종자 분산에 미치는 영향에 관한 연구를 발표했다.
- Strani et al.(2018)[55]에 의해 발표된 치아 마모로 나타난 이탈리아 폰타나 라누치오(Pontana Ranuccio)의 중기 갱신세 유적지의 유제 식단과 서식지에 대한 연구가 발표됐다.
- Strani et al.(2018)[56]은 올리볼라(이탈리아 Aulla) 화석 집합체의 치아 마모 패턴과 습도성을 바탕으로 이탈리아 반도의 겔라시아와 칼라브리아 사이의 통로에서 발생한 환경 변화에 대한 대형 유제류의 반응에 관한 연구를 발표했다.
- Rodriguez & Mateos(2018)[57]는 유럽 후기 및 중기 갱신세 생태계의 유제류 및 육식동물 운반 능력에 대한 연구를 발표했다.
- 시닝 외 연구진(2018년)[58]은 북중국 평야에서 시추된 꽃가루 데이터와 함께 120만 년 전~070만 년 전 아시아 온대 지역의 식물 변화에 대한 연구를 발표했다.
- Zhu et al. (2018)[59]에 의해 저생식물의 생산성이 예상되는 매머드 스텝 생태계가 어떻게 대형 포유류 초식동물의 높은 다양성과 밀도를 지원할 수 있었는지를 평가하는 연구가 발표되었습니다.
- 멸종된 초식성 메가파우나 종은 인간에게 [60]최적의 서식지 패치 내에서 지속적으로 희귀했다고 주장하는 카로테누토 외 연구진(2018)에 의해 유라시아 플라이스토세 후기 24메가파우나 종과 호모 사피엔스의 서식 적합성에 대한 공간적 및 시간적 패턴을 모델링한 연구가 발표됐다.
- 호모 사피엔스의 출현 이전에 도구를 가진 육식 호미닌이 초대형 초식동물의 멸종에 기여했다는 가설을 검증하기 위해 지난 700만 년 동안 동아프리카 초식동물의 군집에 대한 연구가 페이스 외 연구진([61]2018년)에 의해 발표되었다.
- 플라이스토세 린이 파우나의 나이와 중국 황토 고원에 있는 포유류 동물군의 연대순서 배열을 확립하기 위한 의미에 대한 연구는 추 외 [62]연구진(2018)에 의해 발표되었다.
- Agadjanian & Shunkov(2018)[63][64]는 아누이 강 유역 및 차리시 강 유역의 구석기 유적지에서 포유동물 군집 구조에 관한 연구를 발표했다.
- 현존 및 멸종된 코끼리 및 하마의 두개골 형태에 관한 연구는 이들 그룹의 멸종된 섬 왜성 구성원의 두개골이 족보형이라는 가설을 평가한다. van der Geer et al. (2018)[65]가 발표했다.
- 남미 화석 기록에서 곰이 말 위에서 청소했다는 첫 번째 증거는 아빌라 외 연구진(2018)[66]에 의해 브라질 그루타 두 우르소 동굴의 플라이스토세 퇴적물에서 보고되었다.
- 플라이스토세 말기 북미 인류와 대멸종 이전의 대형 포유류의 개체 동태와 플라이스토세 말기 북미 대형 포유류의 멸종 원인을 추론하는 데 대한 연구(2018년)[67]가 발표됐다.
- 1929년에 스톡홀름 동물원에서 태어난 회색 바다표범과 고리 바다표범의 잡종 자손과 고생물학 연구에 대한 연구(2018년)는 두 분류군 사이의 형태학이 중간인 화석 표본이 잠재적으로 잡종일 수 있는지 평가하고 전반적인 교배 가능성을 추정한다.인간의 [68]조상을 포함한 포유류의 진화에서요.
Xenarthrans
- 상완골 모양과 필로사의 현존 및 화석 구성원 간의 기질 탐색 모드 간의 관계에 대한 연구는 de Oliveira & Santos(2018)[69]에 의해 발표되었다.
- 남미 플라이스토세 후기 화석 이종 15종의 종 분포에 대한 연구는 바렐라 외 연구진(2018년)[70]에 의해 발표되었다.
- 올리고세 나무늘보 오로포돈 하팔로이데스와 옥토돈테리움 그란데의 치아에 있는 마이크로파 패턴에 대한 연구와 이러한 분류군의 식단을 추론하는 의미에 대한 연구는 칼토프&그린([71]2018)에 의해 발표되었다.
- Glossotherium robustum의 귀 영역 해부학과 이종 관절의 내이 해부학의 진화에 대한 연구는 Boscaini et al.(2018)[72]에 의해 발표되었다.
- Glossotherium robustum 두개골의 내부 형태에 대한 연구는 Boscaini 등(2018)[73]에 의해 온라인으로 발표되었다.
- Proeremotherium속 멤버 또는 친척에 속하는 거성 나무늘보의 두개골은 Carlini 등(2018)[74]에 의해 Pliocene San Gregorio Formation(베네수엘라)에서 기술된다.
- Tambuso et al.(2018)[75]는 플라이스토세 땅나무의 전방 흉추 융합에 관한 연구를 온라인으로 발표했다.
- 화석 나무늘보 메가테리움과 에레모테리움의 발 해부학적 구조와 발이 습관적으로 뒤집힌 정도를 추론하는 의미에 대한 연구는 Toledo et al.([76]2018)에 의해 발표되었다.
- Megathericulus patagonicus의 새로운 잔해(skull 및 humeri)는 Brandoni et al.[77] (2018)에 의해 Miosene 중기의 케브라다 혼다(볼리비아) 화석 지역에서 기술되었다.
- 메가테륨 필홀리의 새로운 화석 유적은 부에노스아이레스주(아르헨티나)의 플라이스토세 후기 퇴적물에서 기술되었으며, 아그놀린 외 연구진(2018)은 M. 필홀리를 별개의 [78]종으로 재검증했다.
- 탈라소크누스의 두개골 구조와 멸종된 수생 나무늘보의 골질량 증가 진화에 대한 연구는 암슨, 빌렛 & 드 뮤종(2018)[79]에 의해 발표되었습니다.
- 아르헨티나 플라이스토세 말기 Mylodontidae의 두개골 후두부 해부학의 개체발생학적, 종내적, 종간적 변이에 대한 연구는 Brambilla & Ibarra(2018)[80]에 의해 발표되었다.
- 유사 유전학 및 핵 데이터에 기초한 Mylodon darwinii의 계통학적 관계에 대한 연구는 Delsuc et al.(2018)[81]에 의해 발표되었다.
- 남미 후기의 플레이스토세(Pleistose)에서 묘사된 글리토테륨의 첫 번째 어린 표본을 나타내는 그루타 두 우르소 동굴(브라질)의 글리토돈 골엽 형태와 조직학에 대한 연구는 루나 외 연구진(2018)[82]에 의해 발표되었다.
- Plohophorini 부족에 속하는 우루과이의 글리토돈 분류학적 개정판은 Torino & Perea(2018)[83]에 의해 출판되었다.
- 진단 차이와 잠재적 시너포맷을 식별하기 위해 남미 글리토돈과 글리토테륨 종의 형태학을 비교한 연구는 Zurita et al.(2018)[84]에 의해 발표되었다.
- Panochthus속(Panochthus)에 할당된 팜페안 지역(아르헨티나)의 루자니아 퇴적물에서 추출한 2개의 글리토돈티드 표본의 설골기구의 해부학적 구조에 관한 연구는 Zamorano et al.(2018)[85]에 의해 발표되었다.
- de Lima & Porpino(2018)[86]는 파녹투스, 글리토테륨 및 파키야마토리움을 포함한 대형 화생 싱게르트의 골엽, 카라파스 및 미관 조각에 벼룩 및 기타 피부 병변에 의한 기생 사례를 보고하였다.
| 이름. | 참신성 | 상황 | 작가들 | 나이 | 구성 단위 | 위치 | 메모들 | 이미지들 |
|---|---|---|---|---|---|---|---|---|
| 11월 1일 | 유효한 | Fernicola 등 | 마이오세 후기 | Cingulata 멤버입니다. | ||||
| 제너레이션 등 sp. nov. | 유효한 | 린콘 외 | 마이오세 후기 | |||||
| 제너레이션 등 sp. nov. | 유효한 | 린콘 외 | 마이오세 후기 | |||||
| 11월 1일 | 유효한 | 슈타인스벡, 프레이 & 슈타인스벡 | 플라이스토세 후기 |
아프로테리아인
- 튀니지 에오세 화석의 알려진 그리고 새롭게 기술된 유골에 기초한 코끼리 랫드인 Chambius kasserinensis의 해부학적 및 계통학적 관계에 대한 연구는 Tabuce(2018)[90]에 의해 발표되었다.
- Mason, Bennett & Pickford(2018)[91]는 나미비아의 Palaeogen에서 온 황금두더지 Namchloris 아레나탄스의 중이와 내이의 해부학적 구조를 발표했다.
- 도미닝(2018년)[92]은 미국 동부 마이오세 체서피크 그룹의 사이렌 화석과 분류군의 개정판을 발표했다.
- 두개골 유해를 바탕으로 멸종한 주코시데스의 체질량을 추정하는 방법은 주카, 라이온스, 우헨(2018)[93]에 의해 제시되었다.
- Sanders(2018)[94]는 코끼리 모양의 주걱턱에서 볼 치아의 변위 메커니즘의 진화에 관한 연구를 발표했다.
- Choerolophodon corrugatus의 새로운 화석 물질은 Abbas 외 연구진(2018)[95]이 Dhok Pathan Formation(파키스탄)에서 기술했다.
- Miose Halamagai Formation(중국 북부 중가르 분지)의 Gomphotherium connexum 및 Gomphotherium steinheimense 표본의 치석학에서 보존된 피토석은 G. connexum이 필수 브라우저 또는 혼합 공급기였던 것을 나타내는 것으로 그들의 발견을 Wu 등(2018)에 의해 기술되었다.초식 위주의 먹이를 선호했고, 주로 방목하는 [96]습성을 가진 가장 이른 것으로 알려진 주둥아리과 동물이었다.
- 중앙 칠레의 Notiomastodon platensis의 식단과 서식지에 대한 연구는 Gonzales-Guarda et al.(2018)[97]에 의해 발표되었다.
- Smith & Desantis(2018)[98]는 치아 마모로 나타나는 콜롬비아 매머드, 피그미 매머드 및 아메리카 마스토돈의 식단에 대한 연구를 발표했다.
- Stegodon Orientalis 화석과 아시아 코끼리(Elephas maximus)를 포함한 후기 플라이스토세 원시 화석은 Tong 외 연구진(2018)[99]에 의해 양자완 동굴(중국 장시)에서 기술되었다.
- Archidiskodon meridionalis gromovi 분류군의 유효성을 평가하는 연구는 Baygusheva & Titov(2018)[100]에 의해 발표되었다.
- 서부 시베리아 남부(쿠즈네츠크 분지)의 플레이스토세 하층 퇴적물의 아르키디스코돈속 구성원과 아르키디스코돈-마무투스 혈통의 초기 진화에 대한 영향에 대한 연구는 Foronova(2018)[101]에 의해 발표되었다.
- 남부 매머드에 대한 재설명은 플라이스토세 유적지 휴에스카르-1(스페인 그라나다주 바자 분지)에서 이루어졌으며, 초기 플라이스토세 말까지 남부 매머드가 스텝 매머드에 의해 대체된 시기와 방식을 추론하기 위한 이들 유적의 의미에 관한 연구(2018년)[102]가 발표됐다.
- 연구 대상 표본의 털 표본에서 테스토스테론 측정을 목적으로 영구 동토층 보존 시베리아 털 매머드에 대한 연구는 Koren et al.(2018)[103]에 의해 발표되었습니다.
- 시베리아 북동부의 베렐료크 매머드 유적지의 나이와 기원에 대한 연구는 로즈킨 앤 앤더슨(2018년)[104]에 의해 발표되었으며, 이 연구는 피툴코 외 연구진([105][106]2019년)에 의해 비판을 받고 있다.
- MIS 2 기간 동안 유럽에서 털복숭이 매머드 범위의 변화에 대한 연구는 Nadachowski et al.(2018)[107]에 의해 발표되었다.
- 후기 구석기시대 유적지 크라쿠프 스파지스타(폴란드)의 털복숭이 매머드의 생활조건에 대한 연구는 헤인즈, 클리모비츠 & 보이탈([108]2018)에 의해 발표되었다.
- 메지리히 에피그라베티안 유적지와 부잔카 2, 엘리세비치, 유디노보 유적지의 매머드 뼈의 탄소 및 질소 동위원소 조성에 관한 데이터에서 알 수 있듯이 멸종 직전 중부 동유럽 평원에서 매머드의 특정 틈새에 대한 연구는 출판되었다.Hed by Drucker et al. (2018)[109]
- 털북숭이 매머드 표본에서 발견된 기생충의 개요는 Serdyuk & Maschenco (2018)[110]에 의해 출판되었다.
- 시베리아 영구 동토층에서 발견된 여러 냉동 매머드의 지방 및 호미닌에 대한 매머드의 문화적 중요성에 대한 데이터에서 알 수 있듯이 구석기 사회에서 매머드의 식생활 오메가-3 지방산 공급원으로서의 중요성에 대한 연구는 Guil-Guerrero 등([111]2018)에 의해 발표되었다.
- Palkopou et al.([112]2018)는 현존하는 코끼리과 화석 코끼리과와 미국 마스토돈의 14개 게놈에 기초한 코끼리과의 진화사에 관한 연구를 발표했다.
| 이름. | 참신성 | 상황 | 작가들 | 나이 | 구성 단위 | 위치 | 메모들 | 이미지들 |
|---|---|---|---|---|---|---|---|---|
| 11월 1일 | 논쟁의 여지가 있다 | 테오도로우 외 | 세팔로니아 섬에서 온 왜소한 풍토적인 중형 코끼리.Athanassiou, van der Geer & Lyras(2019)는 이 종을 곧게 뻗은 코끼리(Palaeoloxodon antiquus)[114]의 하위 동의어로 간주했다. | |||||
| 제너레이션 등 sp. nov. | 유효한 | 마이오세 초기 | 엘리자베스 베이 포메이션 | 텐렉.모식종은 P. namibiensis이다. | ||||
| 제너레이션 등 sp. nov. | 유효한 | 디아즈-베렌게르 외 | 계통 발생학적 위치가 불분명한 사이렌입니다.모식종은 S. cardieli이다. | |||||
| 제너레이션 등 sp. nov. | 유효한 | 게어브란트, 슈미트 & 코시스 | 엠브레티토포다 초기 멤버.모식종은 S. minor이다. |
박쥐
- Amador et al.(2018)[118]은 현존하는 박쥐뿐만 아니라 Eocene 박쥐의 세사모이드 분포와 Eoconycoronycteris finneyi와 Icaronycteris 지수.
- 타바레스 외 연구진(2018년)[119]은 이 집단이 앤틸리스와 미국 본토 중 어느 지역에서 유래했을 가능성이 더 높은지 평가하는 현존 및 화석 짧은 얼굴 박쥐(Stenodermatinae 아과와 Stenodermatina에 속하는 잎코 박쥐)의 계통 발생에 관한 연구를 발표했다.
- 예외적으로 보존된 이집트 과일 박쥐의 성체 표본은 동아프리카 또는 중동 개체군보다 형태학적으로 이집트와 더 유사하며, 반 담메 외 연구진([120]2018)에 의해 호크 동굴(예멘 소코트라 섬)의 초기 홀로세 퇴적물에서 기술되었다.
| 이름. | 참신성 | 상황 | 작가들 | 나이 | 구성 단위 | 위치 | 메모들 | 이미지들 |
|---|---|---|---|---|---|---|---|---|
| 제너레이션 등 sp. nov. | 유효한 | 존스 등 | 우준차르시데레층 | Palaeochiropterygidae과의 일원입니다.모식종은 A. insularis이다. | ||||
| 11월 1일 | 유효한 | 거넬 & 맨티 | 카나포이 사이트 | 먼지의 일종입니다.2018년 발표, 2020년 기사명 최종판 게재. | ||||
| 11월 1일 | 유효한 | 거넬 & 맨티 | 카나포이 사이트 | 먼지의 일종입니다.2018년 발표, 2020년 기사명 최종판 게재. | ||||
| 11월 1일 | 유효한 | Van Den Hoek Ostende, Van Oijen & Donovan | 플라이스토세 후기 | 프테로노투스의 일종입니다. | ||||
| 11월 1일 | 유효한 | 거넬 & 맨티 | 카나포이 사이트 | 루세투스의 일종입니다.2018년 발표, 2020년 기사명 최종판 게재. | ||||
| 11월 1일 | 유효한 | 거넬 & 맨티 | 카나포이 사이트 | 사콜라이무스의 일종입니다.2018년 발표, 2020년 기사명 최종판 게재. | ||||
| 제너레이션 등 sp. nov. | 유효한 | 거넬 & 맨티 | 카나포이 사이트 | 프테로푸스와 히프시그나투스 이외의 현존하는 모든 과일 박쥐보다 큰 매우 큰 과일 박쥐.속은 새로운 종인 T.harrisi를 포함한다.2018년 발표, 2020년 기사명 최종판 게재. | ||||
| 제너레이션 등 sp. nov. | 유효한 | 핸드 등 | 마이오세 초기 | 배녹번 대형 |
홀수발가락유제류
- 중국 엘리안 분지([125]Erlian Basin)의 고생대 발끝 홀수 유제류 종의 시간적, 공간적 분포에 대한 연구는 Bai et al.(2018)에 의해 발표되었다.
- Miocene 코뿔소 Prosantorhinus germanicus의 두 어린 표본의 치아 이상은 Böhmer & Rössner(2018)에 의해 기술되었으며, 이들은 이러한 [126]기형의 가능한 원인을 논의했다.
- Stephanorhinus kirchbergensis의 턱은 러시아 사하공화국 야나강 무스카야 지역에서 유래한 것으로 Shpansky & Boeskorov(2018년)에 의해 기술되어 있으며, 이 종의 최북단 발생을 나타내고 있다.저자들은 코엘로돈타 자코티쿠스를 양털코뿔소(코뿔소)의 하위 동의어로 해석하기도 한다.
- 중국 에오세 시대의 새로운 유적을 바탕으로 한 텔레오로푸스 두개골 후골격의 형태학에 관한 연구는 바이, 왕, 멍([128]2018)에 의해 발표되었다.
- Miose Linxia Basin(중국 간수) 시료의 치석( calculus石)에서 발견된 녹말 과립의 데이터에서 알 수 있듯이 Miose 코뿔소 Diceros gansuensis의 식단에 대한 연구는 Chen et al.(2018)[129]에 의해 발표되었다.
- Elasmotherium pei의 새로운 화석 물질은 중국 산셴미아오즈이 유적지(니허완 분지)의 하부 플라이스토세(2018년)[130]에서 기술되었다.
- 말의 진화에서 자리 감소에 대한 연구는 Solounias et al.(2018)[131]에 의해 발표된다.
- 북미의 화석 말에서 대규모 서식지의 분할 존재에 대한 연구 테스트는 Parker, McHorse & Pierce(2018)[132]에 의해 발표되었다.
- Sun et al.(2018)[133]에 의해 중국에서 온 Miocene hipparionine 종인 Sivalhipus ptychodus와 S. platyodus의 해부학에 대한 수정된 진단 및 설명이 발표되었다.
- 도밍고 외 연구진(2018년)[134]은 Cerro de los Batallones(스페인)의 히파리온속 구성원의 포스트카닌 치아의 개체 발생(광물화, 분출, 치환 패턴)에 관한 연구를 발표했다.
- 골조직학에서 나타난 다양한 크기의 히파리오닌의 뼈 성장 패턴에 대한 연구 및 마이오세 말기의 유럽 히파리오닌의 크기 감소의 가능한 메커니즘과 근본 추세를 추론하는 의미에 대한 연구는 Orlandi-Oliveras 등(2018)[135]에 의해 발표되었다.
- Lac Karr(알제리아)의 플라이스토세 유적지에서 발견된 에쿠스과 화석의 리뷰는 샘(2018)[136]에 의해 출판되었다.
- 탄소 및 산소 동위원소 데이터로 나타나는 미국 남부, 멕시코 및 남아메리카의 플레이스토세 구성원 식단과 서식지에 대한 연구는 Pérez-Crespo et al.(2018)[137]에 의해 발표되었다.
- 관한 연구 말 시간을 통해 후기 홍적세와 홀로세에 바뀌는 지리학적인 유통, 그리고 고고학적은 고생물학적으로 말에 근거한 유라시아의 전체와paleoenvironmentalpaleoclimatic의 재구축과 함께 후기 제4기를 위해 협회에서 평가를 가로질러 찾는다며 지금(알.(2018년)에 의해 출판되었다.[138]
| 이름. | 참신성 | 상황 | 작가들 | 나이 | 구성 단위 | 위치 | 메모들 | 이미지들 |
|---|---|---|---|---|---|---|---|---|
| 11월 1일 | 유효한 | 바이, 왕, 장 | 에오세 후기 | 히라코돈과의 일원입니다. | ||||
| 11월 1일 | 유효한 | 손, 리, 덩 | 마이오세 후기 | |||||
| 11월 1일 | 바이, 왕, 멍 | 초기 에오세 | 헝양 분지 | 브론토테리아과(Brontotheriidae | ||||
| 11월 1일 | 유효한 | 리 | 에오세(이르딘만한) | 브론토테리아과(Brontotheriidae | ||||
| 제너레이션 등 sp. nov. | 바이, 왕, 멍 | 초기 에오세 | 에쿠스과의 일원입니다.모식종은 E. tingae이다. | |||||
| 11월 1일 | 유효한 | 왕 외 | 이르딘 만하층 | |||||
| 11월 1일 | 유효한 | Sun 등 | 우산 부분지 | |||||
| 제너레이션 등 sp. nov. | 유효한 | Averianov 등 | 에오세 후기 | 브론토테리아과(Brontotheriidae모식종은 M. paganus이다. | ||||
| 일반 빗새출발 | 유효한 | 티시에 외 | 아미노돈과의 일원입니다.모식종은 "Cadurcodon" zimborensis Codrea & Shuraru(1989)이다. | |||||
| 일반 빗새출발 | 유효한 | 베르노르 등 | 마이오세 후기 |
짝수발톱유제류
- Merycoidodontoidea의 계통학에서 전형적으로 사용되는 종류의 치아 측정이 유사한 크기의 관련된 짝수 발가락 유제류 사이를 진단할 수 있는지 여부를 평가하는 연구가 Emery-Wetherell & Davis([148]2018)에 의해 발표되었다.
- 티게니프(알제리아)의 플라이스토세 지역 낙타종 카멜루스 토마스 화석물질과 이 종의 계통발생 관계에 대한 연구는 마르티니 & 제라드(2018)[149]에 의해 발표되었다.
- 치아 마이크로파 및 안정적인 탄소 동위원소에서 알 수 있듯이 마이오세 말기부터 플라이스토세 전반에 걸쳐 플로리다에서 멸종된 페커리의 식단에 대한 연구는 Bradham et al.(2018)[150]에 의해 발표되었다.
- 페커리 Mylohyus elmorei와 Prosthennops serus의 화석은 Douty et al.(2018)에 의해 회색 화석 사이트(미국 테네시주)에서 기술되어 지금까지 [151]보고된 애팔래치아에서 이들 종의 첫 발생을 나타낸다.
- Metridiochoerus속에 속하는 수체의 부분 두개골은 Lazagabaster 등(2018)[152]에 의해 말라파 화석지(남아공)에서 기술되었다.
- Cherin et al. (2018년)[153]는 이탈리아 중부 판탈라(Pantalla)의 초기 플라이스토세(Pleistose)의 새로운 하악골에 대한 설명과 함께, 유라시아와 아프리카 수내 화석 구성원의 계통학적 관계에 대한 연구를 발표했다.
- 반추동물의 계통발생학, 추정 조상 반추동물의 식단과 서식지, 초원의 화석 기록으로 나타나는 반추동물의 저밀도 진화에 관한 연구는 Toljagich et al.(2018)[154]에 의해 발표되었다.
- Rossi, Mello & Schrago(2018)[155]는 반추동물과 태반 포유류의 다른 계통의 진화 중 다양화 속도의 배타성과 변화를 비교한 연구를 발표했다.
- 두개골과 이빨을 포함한 시보레 도르카테리움 크라섬 화석은 Menecart 등(2018년)[156]에 의해 파룬 오거 채석장(프랑스 콘트르)의 미오세(랑히안)에서 발견되었다.
- Croitor, Sanz & Daura(2018)는 코바 델 리노세롱(스페인)[157]의 후기의 고유 사슴 하플로이드케로스 메디테라네우스 유골의 형태학적, 인구학적 분석 결과를 보고한다.
- Rotti et al.(2018)[158]는 치아 에나멜 전자레인지로 나타나는 모렐라푸스의 섭식 습관에 대한 연구를 발표했다.
- Berlioz et al.(2018)[159]는 유럽의 8개 중후기 빌라프란치아 지역의 Eucladoceros ctenoides 표본의 식가소성에 대한 연구를 발표했다.
- 와피티(Cervus canadensis)의 앤틀러 유적은 Croitor & Obada(2018)에 의해 후기 구석기시대 클리머우시II(몰도바) 유적에서 기술되어 유라시아 [160]서부 플레이스토세 후기에 와피티가 존재했음을 확인시켜 준다.
- Pfeifer-Deml(2018)은 휴면 사슴 다마 가이젤라나 화석을 별도의 종으로 키우고 뿔과 골격 특성을 다른 화석 [161]및 최근의 휴면 사슴과 비교한다.
- 북해의 모래 퇴적물에서 발견된 어금니의 깊은 주름에 보존된 매스틱화 식물의 데이터에 나타난 아일랜드 고라니(Megaloceros giganteus)의 식단에 관한 연구는 van Geel et al.(2018)[162]에 의해 발표되었다.
- 나미비아 마이오세의 프로팔레오릭스 스트로메리의 새로운 화석, 프로팔레오릭스의 두개골 해부학적 재기술, 그리고 이 분류군의 계통발생 관계에 대한 연구는 Sannchez et al.(2018)[163]에 의해 출판되었다.
- Merceron, Collyn & Geraads(2018)[164]는 치아 마이크로파로 나타나는 기라피과의 현존 및 화석 구성원의 식생활 선호도에 대한 연구를 발표했다.
- 기린 흔적은 헬름 외 연구진(2018년)에 의해 플라이스토세 웬후이스크랜스 형성(남아공, 브레다스도르프 그룹)에서 기술되어 알려진 [165]기린의 역사적 범위를 증가시키고 있다.
- 치아 에나멜 탄소 및 산소 동위원소 관계로 나타나는 에오세(Uintan) 욜로메카틀 형성(Mexico)의 렙토메릭스의 식단과 서식지에 대한 연구는 Ferusquia-Villafranca et al.(2018)[166]에 의해 발표될 것이다.
- 치아 마모로 나타난 플리오-플라이스토세 슝구라층(에티오피아 오모밸리 하부)의 트라겔라피니 부족 구성원의 식생활 선호도에 대한 연구는 Blondel et al.(2018)[167]에 의해 발표되었다.
- 칭양(중국 간수) 지역의 마이오세 말기 가젤 화석과 이 지역에서 알려진 가젤 종의 분류에 대한 리뷰는 Li et al.(2018)[168]에 의해 출판되었다.
- 봄복의 멸종된 친척인 안티도르카스 본디의 식생활 생태에 관한 연구(2018년)[169]는 에커앤리-토프(Eker & Lee-Thorp)에 의해 발표되었다.
- Martin, Mead & Barboza(2018)[170]는 현존 바이슨 및 화석 바이슨 데이터를 바탕으로 기후 변화가 바이슨속 구성원의 신체 크기 진화에 미치는 영향에 대한 연구를 발표했다.
- 치아 마모로 나타나는 바이슨 안티쿠스의 멕시코 표본 3개의 식생활 선호도와 서식지 사용에 대한 연구는 디아즈-시바하 외 연구진(2018)[171]에 의해 발표되었다.
- 다양한 섭식 선호도를 가진 현존하는 소의 하악골 형태 변화와 라에톨리(탄자니아)의 상층 라에톨리(Upper Laetolil Beds)와 상층 은돌라니야(Upper Ndolanya)의 화석 소의 식생 적응과 초기 호민 점령 기간 동안 라에 덮인 식생 정도에 대한 연구, 플럼이 발표했다.er & Raaum (2018)[172]
- 술라웨시 섬(인도네시아)이 언제 현대적인 형태와 크기를 얻었는지 평가하고, 이 섬에서 가장 큰 세 가지 고유 포유류(바비루사, 셀레베스 사마귀 돼지, 아노아)의 다양화 시기를 결정하는 연구는 Frantz et al.([173]2018)에 의해 발표되었다.
| 이름. | 참신성 | 상황 | 작가들 | 나이 | 구성 단위 | 위치 | 메모들 | 이미지들 |
|---|---|---|---|---|---|---|---|---|
| 11월 1일 | 유효한 | 고디노트 등지의 에르푸르트 | 디코부나과의 일원입니다. | |||||
| 11월 1일 | 유효한 | 메네카르트 외 | Tragulina와 Bachitheriidae에 속하는 초기 반추동물. | |||||
| 11월 1일 | 유효한 | 판 데르 기어 | 플라이스토세 후기 | 구세계 사슴입니다. | ||||
| 11월 1일 | 유효한 | 판 데르 기어 | 플라이스토세 후기 | 구세계 사슴입니다. | ||||
| 11월 1일 | 유효한 | 판 데르 기어 | 플라이스토세 후기 | 구세계 사슴입니다. | ||||
| 11월 1일 | 유효한 | 산체스 외 | 중기 마이오세 | 쉐보탱. | ||||
| 11월 1일 | 유효한 | 고디노 등 | 쵸오로타과의 일원입니다. | |||||
| 제너레이션 등 sp. nov. | 유효한 | 픽포드 & 모랄레스 | 마이오세 초기 | |||||
| 제너레이션 등et comb.새출발 | 유효한 | 셔러, 리호로 & 베커 | 안트라코테리온 하마.모식종은 P. bergeri이다; 속은 또한 하마의 Rütimeyer(1857)와 Strategyus Forster-Cooper(1913)를 포함한다. | |||||
| 11월 1일 | 유효한 | 비비 등 | 올두바이 협곡터 | |||||
| 11월 1일 | 유효한 | 고디노트 등지의 에르푸르트 | 디코부나과의 일원입니다. | |||||
| 11월 1일 | 크로이터 | 갱신세 초기 | 루세르부스의 한 종입니다. | |||||
| 11월 1일 | 크로이터 | 갱신세 초기 | 루세르부스의 한 종입니다. | |||||
| 제너레이션 등 sp. nov. | 유효한 | 코스타풀로스 & 수비세 | 마이오세 후기 | 보비대과의 일원입니다.속은 새로운 종인 S. exophthalmon을 포함한다. |
고래류
- Bebej & Smith(2018)[183]는 고고학에서 요추 이동성을 평가하는 연구를 발표했다.
- 토고 에오세 화석에서 나타난 원형동물 두개골 청각 영역의 해부학적 구조에 대한 연구는 Moulam & Orliac(2018)[184]에 의해 발표되었다.
- 네오겐을 통해 치아 간결화 경향을 확인하려는 화석과 살아있는 고래의 치아 복잡성에 대한 연구는 Peredo, Peredo & Pyenson(2018)[185]에 의해 발표되었다.
- Churchill et al. (2018년)[186]에 의해 이빨고래의 두개골 망원경(얼굴뼈가 서로 미끄러지는 것과 거의 같은 방식으로 긴 부분들이 짧은 부분 위로 미끄러지는 것)의 양적 분석과 진화에 대한 연구가 발표되었습니다.
- 현존 고래와 화석 이빨 고래의 뼈 미로의 형태학에 대한 연구는 Costeur et al.(2018)에 의해 발표되었으며, 이들은 뼈 미로가 이 고래 [187]그룹의 구성원들의 계통 발생과 서식 선호도에 대한 중요한 정보를 제공하는 것으로 그들의 발견을 해석했다.
- 아고로피우스속 구성원의 새로운 화석은 Boessenecker & Geisler(2018)가 Oligose Chandler Bridge Formation(미국 사우스캐롤라이나주)에서 기술하고 있으며, [188]아고로피우스의 개체 발생학적 변화와 감각 해부학에 대한 새로운 정보를 제공한다.
- 리 크릭 광산(미국 노스캐롤라이나주)에서 치아 검사를 바탕으로 알려진 피세테로아목 네오진 구성원의 생명력과 생태에 관한 연구는 길버트, 이바니 & 유헨(2018)[189]에 의해 발표되었습니다.
- 페루의 미오세(토르토니아)에서 발견된 줄기 부리 고래 메사피세투스 그레가리우스의 두개골 후 유골에 대한 설명은 Ramassamy et al.(2018)에 의해 발표되었으며, 이들은 또한 이 종의 [190]목과 앞다리의 근육 구조를 재구성할 것을 제안한다.
- Llanocetus denticrenatus의 거의 완전한 두개골은 에오세 라 메세타 형성(Antarica)에서 기술되었으며, Fordyce & Marx(2018)는 또한 이 종의 계통학적 관계와 가능성 있는 먹이 전략, 그리고 [191]수염고래의 기원과 자이언티즘의 기원을 추론하는 의미를 연구했다.
- 아디게아(러시아)의 미오세 후기 수염고래를 중심으로 멸종 및 현존하는 수염고래와 그 조상의 막질 미로의 형태학에 관한 연구는 Tarasenko et al.(2018)[192]에 의해 발표되었다.
- Herpetocetus의 개체학적으로 어린 표본은 다나카 & 와타나베(2018)에 의해 호로카오시라리카층(일본 홋카이도) 하부에서 기술되어 지금까지 보고된 [193]서태평양의 Miosen Herpetocetinae의 유일한 기록이다.
- 호주 남부의 최신 마이오세(2018년)에서 발견된 카프레아속 구성원의 부분 페리오틱 뼈는 지금까지 보고된 [194]이 속 중 가장 오래된 기록이다.
- 현존 고래와 멸종 고래의 달팽이관 해부학, 고래가 듣는 달팽이관 형상과 주파수 범위의 관계, 그리고 화석 수염고래에서 매우 낮은 주파수와 초저주파 청력의 발생을 결정하기 위한 이들의 의미에 대한 연구는 Ritshe et al.(2018)[195]에 의해 발표되었습니다.
- 아풀리아(이탈리아)의 초기 플라이스토세 퇴적물에서 채취한 고래 등딱지 표본의 산소 동위원소 분석은 콜라레타 외 연구진(2018)에 의해 발표되었으며, 이 연구결과는 지중해의 [196]고위도 지역으로 계절적으로 이주한 고래류에서 서식했음을 나타낸다.
| 이름. | 참신성 | 상황 | 작가들 | 나이 | 구성 단위 | 위치 | 메모들 | 이미지들 |
|---|---|---|---|---|---|---|---|---|
| 제너레이션 등 sp. nov. | 유효한 | 비글리노 외 | 마이오세 초기 | 플라타니스토이데아의 일원입니다.모식종은 A. talen이다. | ||||
| 제너레이션 등 sp. nov. | 유효한 | 골딘 | 중기 마이오세 | 세토테리아과의 일원입니다.모식종은 C. davidi이다. | ||||
| 제너레이션 등 sp. nov. | 유효한 | 올브라이트, 샌더스 & 가이슬러 | ||||||
| 11월 1일 | 유효한 | 키무라, 하세가와 & 고노 | 갱신세 초기 | 회색 고래의 친척입니다. | ||||
| 제너레이션 등 sp. nov. | 유효한 | 이치시마 외 | 초기 플리오센 | 모노돈과의 일원입니다.이 속은 새로운 종인 자포닉스를 포함한다. | ||||
| 11월 1일 | 유효한 | 램버트 등 | 불확실, 아마도 마이오세 | 케르구엘렌 제도까지 370km SWW 해저 | 부리고래아과에 속하는 부리고래. | |||
| 제너레이션 등 sp. nov. | 유효한 | 램버트 등 | 마이오세 후기 | 이끼과의 일원입니다.모식종은 K. khoisani입니다. | ||||
| 제너레이션 등 sp. nov. | 유효한 | 비앙누치 등 | 스쿠알로델피니과의 일원입니다.모식종은 M. ukupachai입니다. | |||||
| 제너레이션 등 sp. nov. | 유효한 | 페레도 등 | 초기 수염 고래.모식종은 M. nesbittae이다. | |||||
| 제너레이션 등 sp. nov. | 유효한 | 페레도 & 피엔슨 | 올리고세 후기 | 멧돼지과의 일원입니다.모식종은 S. midi이다. | ||||
| 제너레이션 등 sp. nov. | 유효한 | 다나카 안도 사와무라 | 중기 마이오세 | |||||
| 제너레이션 등 sp. nov. | 유효한 | 에르난데스 시스네로스 | 올리고세 후기 | 계통 발생학적 위치가 불분명한 채오미스티세티 멤버.모식종은 T. guaycurae이다. | ||||
| 제너레이션 등 sp. nov. | 유효한 | 차이앤포다이스 | 오래된 수염 고래입니다.모식종은 T. waitaki입니다. | |||||
| 제너레이션 등 sp. nov. | 유효한 | 페레도, 우헨, 넬슨 | 마이오세 초기 | 켄트리오돈과의 일원입니다.치누켄시스속은 새로운 종을 포함한다. |
육식동물
- 발리시 외 연구진(2018년)[211]은 헴필리언 메어텐 층(미국 캘리포니아)의 개과 개과 개과 개과의 체계적인 검사를 발표했다.
- Balisi, Casey & Van Valkenburgh(2018년)[212]는 신체 크기와 식생활 전문화와 관련된 두개골 및 치아 특성의 발생이 북미 개과의 종 지속 기간 및 지역 범위와 관련이 있는지를 평가하는 연구를 발표했다.
- Tanis, De Santis & Terry(2018)[213]는 현존하는 회색 늑대와 코요테의 치아 마이크로파 및 그것이 현존하는 개과 화석의 식생활 연구에 미치는 영향에 대한 연구를 발표했다.
- Borophagus parvus에 의해 생산되었을 가능성이 있는 Upper Miosene Mehrten Formation(미국 캘리포니아 주)의 코프로라이트 샘플 설명과 이 종의 식단을 추론하는 의미에 대한 연구는 Wang et al. (2018)[214]에 의해 발표되었다.
- 자바 개화석의 분류법과 상대 연령에 대한 개정판은 판 데르 기어, 리라스 & 볼머(2018)[215]에 의해 발표될 예정이다.
- Zrzav et et al.(2018)[216]에 의해 Caninae 아과의 현존 및 화석 구성원의 계통학적 관계에 대한 연구가 발표되었다.
- 레이나(스페인)의 플리오센 유적지에서 발견된 Nycterutes속 구성원의 새로운 화석과 유라시아의 Nycterutes의 진화사를 추론하기 위한 그들의 의미에 대한 연구는 Bartolini Lucenti, Rook & Morales(2018)[217]에 의해 출판되었다.
- 자칼과 유사한 포식자의 화석 발자국은 맥캔 외 연구진(2018)[218]이 소르바스 분지(스페인)의 소르바스 멤버로부터 기술했다.
- C. variabilis를 Canis mosbacensis의 [219]아종으로 간주한 Jiangzuo et al.(2018)는 Canis variabilis의 화석과 Canis속 플레이스토세 구성원의 형태형 변화에 대한 연구를 발표했다.
- 화석과 현대 북미 회색 늑대의 사지뼈 형태학적 다양성에 대한 연구는 토미야 & 미헨(2018)[220]에 의해 발표되었다.
- 메코지와 바르톨리니 루센티(2018년)[221]는 이탈리아 북부 및 남부 지역의 다른 개체군과 비교하여 아베트라나(이탈리아)에서 온 플레이스토세 후기 회색 늑대의 형태학적 및 형태학적 변동성에 대한 연구를 발표했다.
- Ni Leathlobhair et al. (2018)[222]는 9000년에 걸친 고대 북미 및 시베리아 개로부터 추출된 미토콘드리아 및 핵 게놈의 염기서열 데이터를 바탕으로 유럽 식민지 도래 이전 아메리카에 살았던 개들의 진화 역사에 대한 연구를 발표했다.
- 신석기 시대에 근동 농부와 관련된 개가 다른 가축과 함께 유럽으로 유입되었다는 가설을 실험한 유라시아 전역의 37개 고고학 유적지(상기 구석기 시대부터 청동기 시대까지)의 고대 개들의 미토콘드리아 DNA 염기서열에 대한 연구는 올리비에 외 연구진([223]2018)에 의해 발표되었다.
- Balme, O'Connor & Fallon(2018년)[224]은 호주 늘라보 평원에 있는 마두라 동굴의 딩고 뼈의 나이와 도착 지점에서 호주 전역에 퍼질 가능성이 있는 딩고 비율을 추론하는 데 미치는 영향에 대한 연구를 발표했다.
- 중국 광시(廣西)시 레이(ye)현에서 발견된 약 22,000년 된 자이언트 판다 표본의 완전한 미토콘드리아 게놈은 고 외 연구진(2018년)[225]에 의해 배열되었다.
- 펠루시다 동굴(캐나다 밴쿠버 섬)의 짧은 얼굴 곰(Arctodus simus)과 불곰(Ursus arctos) 화석의 연대에 대한 연구는 Steffen & Fulton(2018)[226]에 의해 발표되었다.
- 폴란드 클레트노(Kletno)의 Jaskinia Niedwwiedzia(곰 동굴)에서 발견된 플레이스토세 곰(Ursus ingressus)의 생활 조건에 대한 연구는 그들의 뼈에 해리스 라인의 빈도로 나타나 있다. (2018)[227]
- 동위원소 데이터에 기초한 카르파티아 산맥의 4개 MIS 3 현장의 동굴 곰의 식단에 대한 연구는 Robu 등(2018)[228]에 의해 발표되었다.
- 플레이스토세 후기 동굴 곰 4마리에서 나온 여러 가지 게놈 데이터는 동굴 곰이 플레이스토세 기간 동안 갈색 곰과 교배되었으며 동굴 곰의 DNA 조각이 여전히 살아있는 갈색 [229]곰의 게놈에 남아 있다고 보고한 바로우 외 연구진(2018)에 의해 제시되었다.
- Zhoukoudian의 [230]곰 화석은 Jiangzuo et al.(2018)에 의해 수정본으로 발표되었으며, Jiangzuo et al.(2018)은 Zhoukoudian의 Loc. 1에 Ursus deningeri의 존재를 명확히 확인했다.
- 동굴 곰 대퇴골의 뼈 조직학과 동굴 곰의 성장과 생활 이력 변수를 추론하기 위한 의미에 대한 연구는 Veitschegger et al.(2018)[231]에 의해 발표되었다.
- 바리쉬니코프, 푸자첸코, 바리쉬니코바(2018)[232]는 동굴과 불곰의 하악골과 그 조상(우르수스 미니무스와 우르수스 에트루쿠스)의 형태학적 변동성에 대한 연구를 발표했다.
- Law, Slater & Mehta(2018)[233]는 현존하는 화석 분류군 데이터를 바탕으로 족장육식동물 진화에 따른 혈통 다양화와 체질량 및 길이의 다양성에 관한 연구를 발표했다.
- Tarquini et al.(2018)[234]에 의해 화석 프로키오나스과, 파라히에노돈, 테트라프로토모의 체질량을 추정하는 연구가 발표되었다.
- 나수아속과 프로키온속 화석은 지금까지 [235]보고된 남미의 프로키온류 중 가장 오래된 기록인 루이즈-라모니, 린콘, 몬테라노-발레스테로스(2018)에 의해 오로쿠알 지방의 엘 브렐(베네수엘라)의 마르플라탄 단계에서 기술되었다.
- 잘 보존된 첫 번째 유골 렙타르크투스 오리건엔시스 화석은 칼레드, 켈 & 데이비스(2018)[236]에 의해 Miocene Mascall Formation(미국, Oregon)에서 발견되었다.
- Miosene 유스텔리드 종 Semantor macruus의 뒷다리 관절 형태학 및 이동성에 대한 연구는 Lavrov, Tarasenko 및 Blasenco(2018)[237]에 의해 발표되었다.
- 스페인 마이오세 초기 이베리티스 아잔제(I. Buloti)의 새로운 화석 물질에 대한 기술, 이베리티스 해부학에 대한 새로운 정보를 제공하고, 이 속들의 계통학적 관계에 대한 연구는 발렌치아노 외 연구(2018)[238]에 의해 온라인에 게재되었다.
- Boessenecker(2018년)에 의해 중기의 플레이스토세 메르세드 형성(미국 캘리포니아)에서 해달의 친척인 엔히드라속(Enhydra)의 대퇴골이 기술되어 지금까지 [239]보고된 강력한 지질 연대 제어와 함께 태평양에서 엔히드라에 대한 가장 오래된 기록을 나타낸다.
- 에날리아르콕토스속 새 표본은 미오세 스쿠너 걸치층(미국 캘리포니아), 올리고세 야키나층(미국 오레곤), 미오세 아스토리아층(미국 오레곤)에서 Poust & Boessenecker에 의해 설명되며, 2018년 지리적으로 확장된다.
- Enaliarctos diaci와 현존하는 포카인 귀없는 물개의 앞다리 형태학, 현존하는 포카인 물개에 의한 먹이 확보 및 찢기 위한 앞다리 사용, 초기 피니피드의 먹이행동 유추에 관한 연구는 Hocking et al.(2018)[241]에 의해 발표되었다.
- 슬로바키아의 미오세 때 발견된 귀 없는 물개 데비노포카 클레이튼이의 첫 번째 하악골에 대한 해부학적 설명은 Rahmat & Koretsky(2018)[242]에 의해 출판되었다.
- 모나키아과에 속하는 귀 없는 바다표범의 상완골은 북해의 [243]최신부터 후기까지의 최초의 모나키네 표본을 나타내는 드와엘, 램버트, 루위(2018)의 플라오센(Piacenzian) 릴로 형성(벨기에)에서 기술된다.
- 스페인 플리오센에서 호미포카속으로 분류된 화석 표본이 Rahmat et al.(2018)에 의해 기술되어 있으며, 플리오센속 [244]최초의 유럽 기록이다.
- 벨레스-후아베(2018)[245]는 오도베니드 네오테리움 미룸의 하악골 형태학 및 다른 피니피드를 대표하는 캘리포니아의 Miose Sharktooth Hill Bonebed의 하악골 친화성에 대한 연구를 발표했다.
- 온토세투스 에몬시의 새로운 표본은 Boessencker, Boessencker & Geisler(2018)가 오스틴 샌드 피트(미국 사우스캐롤라이나주 리치빌)에서 설명한 것으로,[246] 지금까지 보고된 대서양 연안 평야에서 발견된 O. 에몬시의 가장 어린 기록을 나타낸다.
- 플라이스토세 하이에나가 작은 설치류를 잡아먹는 증거는 윌리엄스 외 연구진(2018)[247]에 의해 Bois Roche 동굴 사이트(프랑스)에서 보고되었다.
- 자소브스카 동굴(슬로바키아)의 청소년 동굴 하이에나의 외부 뇌 형태에 대한 연구는 페트로비치 외 연구진(2018)[248]에 의해 발표되었다.
- 쿠거의 두개골은 치멘토 & 돈다스(2018)가 아르헨티나의 플레이스토세(엔세나단)에서 기술한 것으로,[249] 남미 플라이스토세 말기 이전의 쿠가에 대한 최초의 명확한 기록을 나타낸다.
- 의 모양과 뼈가 앙상하전정계의 치수에 치타의 내이에 관한 연구, 다른 현존하는 felids과 멸종된 거대한 치타(Acinonyx pardinensis)과 프로아 일루 루스 lemanensis에서 전정 시스템이 맡았고, 치타의 전정계 Grohé, 리가 출판의 발전에와 그것을 비교함;플린(.2018년를 참조해 주세요.[250]
- 이전에 판타라 곰바조엔시스 종으로 분류된 몬테아르젠타리오(이탈리아)의 후기 빌라프란치아 유적지에서 발견된 대형 펠리드의 일부 두개골에 대한 설명은 Cherin et al.(2018)에 의해 발표되었으며, Cherin et al.(2018)는 이 표본(기존에는 P곰바조엔시스 종으로 언급되었던 일부 이탈리아 자료)을 P.[251]
- 자파드네 타트라 산맥(슬로바키아)의 메드베디아 동굴에 있는 적어도 4마리의 성인 동굴 사자(판테라 스펠레아)의 화석과 이 분류군의 구성원의 범위와 사회적 행동에 대한 연구는 사볼, 굴라르 & 호바트(2018)[252]에 의해 출판되었다.
- 유라시아에서 가장 큰 화석 사자 매장지 중 하나인 남우랄의 이마나이 동굴에서 발견된 최소 11명의 화석 사자 개인에 속하는 뼈에 대한 연구는 Gimranov 등([253]2018)에 의해 발표되었다.
- 두개골 길이 면에서 미국 사자의 큰 표본에 필적하고 현존하는 사자의 알려진 두개골보다 상당히 큰 사자의 두개골은 케냐의 플라이스토세(2018년)[254]에 의해 기술되었다.
- Pajmans et al. (2018년)[255]는 현대 표범 분포 전체에 걸친 역사적 표본의 미토게놈 염기서열 데이터와 코카서스와 중앙유럽의 플라이스토세 후기의 유적에 기초한 표범의 역사적 생물지리학에 관한 연구를 발표했다.
- 아르헨티나에서 온 이 재규어의 최북단 화석 기록은 로드리게스 외 연구진([256]2018년)에 의해 플라이스토세 후기-홀로세 초기 리오 베르메호 층(포르모사 주)에서 보고되었다.
- 피라스 외 연구진(2018)[257]은 검치 고양이 하악골의 형태학적 다양성 진화와 검치 고양이 진화의 특이성 및 멸종률에 관한 연구를 발표했다.
- Harano & Kutsuke(2018)[258]에 의해 화석 검치 고양이와 현존하는 구름무늬 표범으로 이어지는 펠리드 계통의 상위 개 길이의 진화에 관한 연구가 발표되었습니다.
- 비슬로보코바(2018)가 몬테네그로 트리카 동굴에서 메간테레온 화이트이의 개 한 마리를 보고했는데, 이는 이 아프리카 종이 [259]발칸반도에 처음으로 침투한 것을 반영한다.
- Smilodon fatalis의 거의 완전한 두개골은 플라이스토세 Sopas Formation(Uruguay)에서 Manzuetti et al.(2018)에 의해 설명될 것이며, 이는 남미 [260]동부 지역에서 최초로 알려진 Smilodon fatalis에 대한 기록을 나타낸다.
- Smilodon fatalis와 Homotherium serum의 두개골 강성과 유연성에 대한 연구 및 이러한 고양이의 살처분 행동을 추론하는 의미에 대한 연구는 Figueirido et al.(2018)[261]에 의해 발표되었다.
| 이름. | 참신성 | 상황 | 작가들 | 나이 | 구성 단위 | 위치 | 메모들 | 이미지들 |
|---|---|---|---|---|---|---|---|---|
| 11월 1일 | 유효한 | 보세네커 & 처칠 | ||||||
| 11월 1일 | 유효한 | 토노모리 외 | 중기 마이오세 | |||||
| 제너레이션 등 sp. nov. | 유효한 | 드와엘 등 | ||||||
| 서브스펙 11월 | 유효한 | 앤젤리시 & 로시 | 늑대의 아종. | |||||
| 11월 1일 | 유효한 | 포벨 | 플리오센-플라이스토세 전이 | 아프리카 사향고양이의 친척. | ||||
| 11월 1일 | 유효한 | 루크 등 | ||||||
| 일반 빗새출발 | 유효한 | 드와일, 람베르 & 루위 | 마이오세 후기 | 아마 디에스트 형성 | Phocinae 아과에 속하는 귀 없는 바다표범.모식종은 "Monotherium" oraratum Van Beneden(1876년)이다.속은 "Monotherium" 아핀 반 베네덴(1876년)도 포함한다. | |||
| 11월 1일 | 유효한 | 사무엘스, 브레드호프트 & 월리스 | 울버린의 친척입니다. | |||||
| 제너레이션 등 sp. nov. | 유효한 | Adrian, Werdelin & Grossman | 마이오세 초기 | 로티독 포메이션 | 멧돼지과의 일원입니다.모식종은 K. 나이팅게일입니다. | |||
| 11월 1일 | 유효한 | Adrian, Werdelin & Grossman | 마이오세 초기 | 로티독 포메이션 | Paradoxurinae 아과에 속하는 비버리다과. | |||
| 일반 빗새출발 | 유효한 | 바르톨리니 루센티 | ||||||
| 11월 1일 | 유효한 | 장쩌오 등 | 갱신세 초기 | |||||
| 제너레이션 등 sp. nov. | 유효한 | 벨레스후아르베&살리나스마르케스 | 바다코끼리의 친척.모식종은 N. arandai입니다. | |||||
| 11월 1일 | 유효한 | 에머트 및 쇼트 | 나수아의 한 종입니다. | |||||
| 일반 빗새출발 | 유효한 | 드와일, 람베르 & 루위 | ||||||
| 11월 1일 | 유효한 | 루크 등 | ||||||
| 11월 1일 | 유효한 | Stinnesbeck 등 | 판데라의 한 종입니다.2018년 발표, 2020년 기사명 최종판 게재. | |||||
| 11월 1일 | 유효한 | 에머트 및 쇼트 | 프로시온의 일종입니다. | |||||
| 11월 1일 | 유효한 | 에머트 및 쇼트 | 프로시온의 일종입니다. | |||||
| 제너레이션 등 sp. nov. | 유효한 | 드 보니 등 | 마이오세 후기 | |||||
| 제너레이션 등 sp. nov. | 유효한 | 마갈란 등 | 마이오세 후기 | 바다코끼리의 친척.모식종은 T. orangeensis이다. | ||||
| 제너레이션 등 sp. nov. | 유효한 | 드와엘 등 | Eastover Formation 또는 Yorktown Formation |
설치류
- 이베로시타니아 지역(이베리아 반도 및 프랑스 남부)의 마이오세 말기 설치류에 대한 연구는 설치류 메타군을 식별하고 환경 변화에 대한 반응을 분석하는 것을 목적으로 한다. Blanco et al. (2018)[278]
- 히스파니올라에서 멸종된 고유 설치류의 생태와 식생활 선호도에 대한 연구는 쿡앤크롤리(2018)[279]에 의해 발표되었습니다.
- 탐콰미스의 운동 적응과 라이프스타일의 재구성을 목적으로 한 중국 에오세시대 탐콰미스속 탐콰미스속 2종의 견골골 형태에 관한 연구는 포스토위츠-프렐릭, 리앤니([280]2018)에 의해 발표되었다.
- Rinderknecht, Bostelmann 및 Ubilla(2018)[281]에 의해 Miosene Camacho Formation(우루과이)에서 Dinomyd laurillardi의 새로운 성인 및 청소년 표본이 기술되었다.
- 완모식표본과 새로운 표본의 데이터를 기반으로 한 테트라실루스 발테리의 해부학적 및 계통발생적 관계에 대한 연구는 Kerber et al.(2018)에 의해 온라인으로 발표되었으며, 이들은 이 분류군을 유효한 [282]종으로 간주한다.
- 중앙아르헨티나 마이오세 말기의 잘 보존된 표본에 기초한 Cardiomys의 두개골 후두개(post cranium)에 대한 첫 번째 설명과 이 분류군의 고생물학과 계통학에 대한 연구는 칸델라, 무뇨즈, 가르시아-에스폰다(2018)[283]에 의해 발표되었다.
- 지금까지 [284]보고된 멸종된 남미 카보모형의 가장 최근의 기록인 Verzi et al.(2018년)에 의해 홀세네 삼바키 드 푸에르토 란다 유적지(아르헨티나 엔트레 리오스 주)에서 에우리요마토미인 에키미드 디콜포소르의 하악골 조각이 기술되었다.
- 그 산 펠리페:베네수엘라 동북부 hutia(Mesocapromys sanfelipensis)의 최초로 알려진 화석(거의 완전한 두개골)Cueva 델 Indio(Mayabeque도, 쿠바)내에 Viñola의 로페즈 가리도 및에 의해 동굴 방에서;설명되어 있는 과거의 이 종의 현대 인구가 한계 유물의 표시로 그들의 발견을 해석하 Bermúdez(2018년),. dist제4기 중의 늑골.[285]
- 엔트레리오스주(아르헨티나) 마이오세 말기 포베로미스속 구성원의 화석 개정과 이들의 계통학 및 계통학적 관계에 대한 연구가 Rasia & Candela(2018)[286]에 의해 발표되었다.
- 코엔두 마그누스 종에 속하거나 관련된 신세계 고슴도치 화석은 Vezosi & Kerber(2018)[287]에 의해 산타페 주(아르헨티나)의 상부 플라이스토세부터 기술되었다.
- 문제가 된 신진스키우루스속 시노타미아스의 개정판은 시니차(2018)[288]에 의해 출판되었다.
- Miosene Clarkia 화석층(미국 아이다호주 Latah Formation)에서 Calede 외 연구진(2018)이 다람쥐과 동물 한 마리가 보고되었으며, 이는 이 라거스테테에서 [289]보고된 최초의 네발동물이다.
- Miopetaurista neogrivensis의 11.63 만년 정도 나이와 함께 화석은 Casanovas-Vilar(알.(2018년)에 의해 Abocador 들 수 있마타 사이트 ACM/C5-D1(엘스 Hostalets 드 Pierola, 스페인 카탈로니아), 표시는gliding-related 진단 기능을 현존하는 형식에 의해 공유된 날다람쥐의 가장 오래된 화석을 대표하는 경기에서 기술되어 있다.[290]
- 현존하는 마운틴 비버의 첫 번째 가상 내생동물과 아플로돈티아과의 세 가지 화석 구성원은 Bertrand et al.(2018)[291]에 의해 기술되었다.
- Nowakowski et al. (2018)[292]는 아노말로미스 갈라르디 종과 플리오스팔락스속에 속하는 우크라이나 현존 및 화석 스팔락스의 어금니의 에나멜 초미세구조에 관한 연구를 발표했다.
- 아르헨티나와 볼리비아의 플라이스토세(Pleistose)에서 발견된 Nectomys속 추정화석 수정본은 Pardinas & Barbiér(2018)[293]에 의해 발표되었다.
- 칠레 남부의 플레이스토세 빙하기 동안 아브로트릭스 마니의 인구통계학적 역사에 대한 연구는 발데즈 & 데리아(2018)[294]에 의해 발표되었다.
- 몬쿠닐솔레, 조르다나, 쾰러(2018년)[295]는 이탈리아 마이오세 설치류 미크로티아의 체질량과 진화에 관한 연구를 발표했다.
- 화석 기록의 철저한 검토를 바탕으로 9가지 강력한 화석 제약을 구현한 쥐류 설치류의 계통발생 관계에 대한 연구는 아고바 외 연구진(2018)[296]에 의해 발표되었다.
| 이름. | 참신성 | 상황 | 작가들 | 나이 | 구성 단위 | 위치 | 메모들 | 이미지들 |
|---|---|---|---|---|---|---|---|---|
| 제너레이션 등 sp. nov. | 유효한 | 리 등 | 잔다 분지 | 햄스터.이 속은 새로운 종인 A. liuae를 포함한다. | ||||
| 11월 1일 | 유효한 | 리 | 디포디과의 일원입니다. | |||||
| 제너레이션 등 sp. nov. | 유효한 | 루이스 등 | ||||||
| 제너레이션 등 sp. nov. | 유효한 | 드 브루인 외 | ||||||
| 11월 1일 | 유효한 | 세르데뇨 외 | 마이오세 후기 | 카피바라의 친척입니다.2018년 발표, 2019년 기사명 최종판 게재. | ||||
| 제너레이션 등 sp. nov. | 유효한 | 페레스 외 | 살라 침대 | 신세계 고슴도치.테트라로포돈타속은 새로운 종을 포함한다. | ||||
| 11월 1일 | 유효한 | Ferusquia-Villafranca 등 | 쥐과 동물입니다. | |||||
| 11월 1일 | 유효한 | 보이빈 등 | 올리고세 초기 | 친칠로아목의 일종으로 추정됩니다. | ||||
| 11월 1일 | 유효한 | 보이빈 등 | 올리고세 초기 | 친칠로아목의 일종으로 추정됩니다. | ||||
| 11월 1일 | 유효한 | Pelaez-Campomanes 등 | 마이오세 초기 | 쥐과의 일원입니다. | ||||
| 11월 1일 | 유효한 | 뫼르스와 토미 | 마이오세 초기 | 나카무라층 | 카스토리아과의 일원입니다. | |||
| 11월 1일 | 유효한 | 히메네스히달고, 게레로아레나스 & 스미스 | 에오세(카드로니아) | Geomyidae의 일원입니다. | ||||
| 11월 1일 | 유효한 | 로페스-안토냥자스 외 | 캐리도미스의 일종입니다. | |||||
| 제너레이션 등 sp. nov. | 유효한 | 보이빈 등 | 올리고세 초기 | 에레시존토아목의 일원입니다.모식종은 K. raimondii이다. | ||||
| 일반 빗새출발 | 유효한 | 바르비에르, 오르티스 & 파르디냐스 | 지그모돈틴 설치류, 포모수스 레이그(1978)의 새로운 속. | |||||
| 제너레이션 등 sp. nov. | 유효한 | 페레스 외 | 살라 침대 | |||||
| 11월 1일 | 유효한 | Cramb, Price & Hocknull | 연령 불명, 갱신세 중후기일 가능성이 있음 | 레가디나의 일종입니다. | ||||
| 11월 1일 | 유효한 | Cramb, Price & Hocknull | 중기의 갱신세 | 레가디나의 일종입니다. | ||||
| 제너레이션 등 sp. nov. | 유효한 | 보이빈 등 | 올리고세 초기 | 계통 발생학적 위치가 불분명한 옥토돈토아과의 일원입니다.모식종은 M. fuccurnens이다. | ||||
| 파. nov | 유효한 | 도슨&Constenius | 중기 에오세 | |||||
| 파. nov | 유효한 | 페레스 외 | Salla 대지 | |||||
| 제2세대 외 11월 | 유효한 | 웨슬스 등 | Melissiodontinae아과에 속하는 Muridae과.모식종은 M. milosi이고, 속은 M. lautus도 포함한다. | |||||
| 제너레이션 등 sp. nov. | 유효한 | 마인 & 픽포드 | 검은 까마귀 석회암 | 아마도 Reithroparamys의 친척일 것이다.모식종은 N. inspectatus이다. | ||||
| 11월 1일 | 유효한 | 리 등 | 햄스터. | |||||
| 11월 1일 | 유효한 | 마도조-야엔 외 | Caviinae의 일원입니다. | |||||
| 제너레이션 등 sp. nov. | 유효한 | 마틴 등 | 갱신세 초기 | 알비콜라과의 일원입니다.속은 새로운 종인 O. giberti를 포함한다. | ||||
| 11월 1일 | 유효한 | Van de Weerd 등 | 올리고세 초기 | Paracricetodontinae아과에 속하는 Muridae과. | ||||
| 11월 1일 | 유효한 | Van de Weerd 등 | Paracricetodontinae아과에 속하는 Muridae과. | |||||
| 11월 1일 | 유효한 | 왕 | 마이오세 후기 | 린샤 분지 | ||||
| 11월 1일 | 유효한 | 왕 | 마이오세 후기 | 린샤 분지 | ||||
| 11월 1일 | 유효한 | 반 콜프쇼텐, 테사코프 & 벨 | ||||||
| 11월 1일 | 유효한 | 페레스 외 | 살라 침대 | |||||
| 제너레이션 등 sp. nov. | 유효한 | Ferusquia-Villafranca 등 | 중기 에오세 후기 | 제타미스의 친척으로, 새로운 제타미과에 할당되어 있으며, 카비오모르파(Caviomorpha)의 일원일 가능성이 있습니다.이 속은 새로운 종인 P. mixtecus를 포함한다. | ||||
| 제4세대 외 11월 | 유효한 | 왕 | 마이오세 후기 | 린샤 분지 | 타키요릭토이드아과와 파라히조미니족에 속하는 스팔라과.이 속은 새로운 종인 P. Indigenus, P. gansuensis, P. planus 및 P. pristinus를 포함한다. | |||
| 11월 1일 | 유효한 | 페레스 외 | 살라 침대 | |||||
| 제너레이션 등 sp. nov. | 유효한 | 보이빈 등 | 올리고세 초기 | 계통 발생학적 위치가 불분명한 옥토돈토아과의 일원입니다.모식종은 S. paulus이다. | ||||
| 제너레이션 등 sp. nov. | 유효한 | 보이빈 등 | 올리고세 초기 | 에레시존토아목의 일원입니다.모식종은 라보센시스입니다. | ||||
| 11월 1일 | 유효한 | 프리토 등 | 겨울잠쥐. | |||||
| 제2세대 외 11월 | 유효한 | 보이빈 등 | 올리고세 초기 | 계통 발생학적 위치가 불분명한 Caviomorpha의 구성원.모식종은 T. subandinus이다.속은 T. mayoensis도 포함한다. | ||||
| 제너레이션 등 sp. nov. | 유효한 | 검은 까마귀 석회암 | Zegdoumyidae과의 일원입니다.모식종은 T. calcareus이다. | |||||
| 제너레이션 등 sp. nov. | 유효한 | 에오클리프 석회암 | ||||||
| 11월 1일 | 유효한 | 시니차&네신 | 마이오세 후기 | Leithiinae아과에 속하는 겨울잠쥐. | ||||
| 11월 1일 | 유효한 | 드 브루인 외 |
영장류
- Rossie et al.(2018)[323]에 의해 현존 및 고생대 스트렙시린과 하플로린에서 비루관 및 관의 형태학 및 고생대 영장류의 계통발생적 관계를 추론하는 의미에 관한 연구가 발표되었다.
- 프로포토 리케이의 해부학적 및 계통발생적 관계에 대한 연구는 Gunnell et al.(2018)에 의해 발표되었으며, Gunnell et al.(2018)는 프로포토 리케이와 플레시오피테쿠스 모두를 에이에이의 [324]친척으로 간주했다.
- 마다가스카르산 아화석 여우원숭이의 턱 근육과 물어뜯는 힘, 그리고 이들 여우원숭이의 식단을 추론하는 의미에 대한 연구는 페리(2018)[325]에 의해 발표되었다.
- A study on the early evolution of North American adapids and omomyids, comparing reconstructed dietary niches of these primates and other animals from their guild to establish the nature of the competitive environment surrounding primate origins in North America, is published by Stroik & Schwartz (2018).[326]
- Description of isolated phalanges from four early Eocene localities in Wyoming (United States), indicative of presence of grooming claws in five genera of early haplorhine primates (including Teilhardina), is published by Boyer et al. (2018).[327]
- A study evaluating whether the locomotor behaviour of extant New World monkeys can be inferred from their talus morphology, and applying machine learning algorithms trained using both the biomechanical and morphometric data from the extant taxa to infer the possible locomotor behaviour of Miocene New World monkeys from Argentina, Chile, Peru, Colombia and Cuba, is published by Püschel et al. (2018).[328]
- Partial mandible of Homunculus patagonicus from the early Miocene sediments in the Coyle river area (Santa Cruz Province, Argentina), providing new information on the morphology of the mandible and teeth of Homunculus, and two teeth of Mazzonicebus almendrae from Colhue-Huapi (Chubut Province, Argentina), providing the first evidence of the deciduous dentition of Mazzonicebus, are described by Novo, Tejedor & González Ruiz (2018).[329]
- A study on the phylogenetic relationship of the Jamaican monkey (Xenothrix mcgregori), as indicated by ancient DNA data, is published by Woods et al. (2018).[330]
- A tibia of a large-bodied arboreally adapted Old World monkey (a member or a relative of the genus Rhinocolobus) is described from the Australopithecus afarensis-bearing Upper Laetolil Beds (~3.7 Ma) of Laetoli (Tanzania) by Laird et al. (2018), who also study the implications of the specimen for inferring the paleoenvironment of the Upper Laetolil Beds.[331]
- A skull of a large papionin monkey is described from the Lower Pleistocene site of Dafnero-3 (Greece) by Kostopoulos et al. (2018), who interpret the anatomy of this skull as indicating that the specimen could equally be ascribed to either the Eurasian genus Paradolichopithecus or to the East Asian Procynocephalus, and argue in favor of the synonymy of these genera.[332]
- A study on the phylogenetic relationships of living and fossil African papionins is published by Pugh & Gilbert (2018).[333]
- A study on the fossil members of the genus Papio from across Africa, focusing on their distinguishing features and distribution, is published by Gilbert et al. (2018).[334]
- A study on the feeding ecology of Plio-Pleistocene members of the genera Papio and Theropithecus from the Shungura Formation (Ethiopia) is published by Martin et al. (2018).[335]
- Three specimens of the Barbary macaque are described from the Pleistocene of the Netherlands by Reumer, Mol & Kahlke (2018).[336]
- A study evaluating whether climatic and environmental changes were the main cause of extinction of Oreopithecus bambolii is published by DeMiguel & Rook (2018).[337]
- A study on the body mass sexual dimorphism in Nacholapithecus kerioi is published by Kikuchi et al. (2018).[338]
- Description of the anatomy of the forelimb long bones of the holotype specimen of Nacholapithecus kerioi is published by Takano et al. (2018).[339]
- Fragment of the maxilla of a member of the genus Sivapithecus is described from the Miocene of the Tapar locality (Gujarat, India) by Bhandari et al. (2018), representing the first record of a hominoid from the Neogene of the Kutch Basin.[340]
- A review of the paleontological, archeological, genetic and behavioral evidence of the impact of at least 70,000 years of human influence on orangutan distribution, abundance and ecology is published by Spehar et al. (2018).[341]
- Description of tooth decay affecting the type specimen of Dryopithecus carinthiacus, and a study on its implications for inferring the diet of this specimen, is published by Fuss, Uhlig & Böhme (2018).[342]
- A study on the phylogenetic relationships of Graecopithecus published by Benoit & Thackeray (2017), aiming to refute the hypothesis that Graecopithecus is a member of the hominin clade,[343] is criticized by Fuss et al. (2018).[344]
- A study evaluating whether machine learning methods can accurately classify extant apes based on dental data, and using this classification method to explore the affinities between dentitions of Miocene hominoid fossils and living apes, is published by Monson, Armitage & Hlusko (2018).[345]
- A study on the utility of enamel thickness, enamel-dentine junction shape and crown development for determining the taxonomic affiliation of isolated teeth of hominins and pongines from the Asian Pleistocene is published by Smith et al. (2018).[346]
General paleoanthropology
- Estimations of body mass in Pliocene and Pleistocene hominins based on lower limb bones dimensions are presented by Ruff et al. (2018).[347]
- A study on the evolution of the brain size in hominins is published by Du et al. (2018).[348]
- A study on the evolution of the mandible shape in hominins, based on an analysis of the mandibular shape variation in a large sample of plesiadapiforms and primates, is published by Raia et al. (2018).[349]
- A study on the cervical kinematics in early fossil hominins, based on an analysis of uncinate processes in the vertebrae of fossil hominins, Homo sapiens and extant nonhuman primates, is published by Meyer et al. (2018).[350]
- A study on the intra-specific variation of patterns of metatarsal robusticity (a measure reflecting habitual stresses in long bones, and in particular, loads experienced over an animal's lifetime) in modern humans and extant African apes, and its implications for inferring whether the Olduvai Hominid 8 foot was biomechanically similar to the feet of modern humans, is published by Patel et al. (2018).[351]
- A study on the bony shape variables in the metatarsals of extant anthropoid primates and fossil hominins, and on their importance to the evolution of terrestrial bipedalism in hominins, is published by Fernández et al. (2018).[352]
- Domínguez-Rodrigo & Baquedano (2018) evaluate the ability of successful machine learning methods to compare and distinguish various types of bone surface modifications (trampling marks, crocodile bite marks and cut marks made with stone tools) in archaeofaunal assemblages.[353]
- Taphonomic study on the ca. 1.84 million year old bovid fossils (preserving evidence of meat eating by early hominins) from Olduvai Gorge (Tanzania), evaluating whether hominins had early access to fleshed carcasses through hunting or active scavenging, or late access to largely defleshed carcasses through passive scavenging, is published by Parkinson (2018).[354]
- The study published by Gierliński et al. (2017), reporting putative tetrapod footprints with hominin-like characteristics from the late Miocene of Crete (Greece),[355] is criticized by Meldrum & Sarmiento (2018).[356]
- A study aiming to estimate body mass of Orrorin tugenensis and Ardipithecus ramidus is published by Grabowski, Hatala & Jungers (2018).[357]
- A study comparing the calcar femorale of Orrorin tugenensis and other hominoids is published by Kuperavage et al. (2018), who interpret their findings as indicating that O. tugenensis was an early bipedal hominin.[358]
- A study on the hydrological changes in the Limpopo River catchment and in sea surface temperature in the southwestern Indian Ocean for the past 2.14 million years, and on their implications for inferring the palaeoclimatic changes in southeastern Africa in this time period and their possible impact on the evolution of early hominins, is published by Caley et al. (2018).[359]
- A study on the behavioral features which might have contributed to the demographic success of early hominids such as Australopithecus, based on comparison with macaques, is published by Meindl, Chaney & Lovejoy (2018).[360]
- A study on the diversity dynamics of early hominins, evaluating whether the observed patterns of early hominin diversity can be better explained by sampling biases or genuine evolutionary processes, is published by Maxwell et al. (2018).[361]
- A study on the pelvic morphology in Ardipithecus and Australopithecus, evaluating the hypothesis that early hominins retained ischial proportions and orientation that favored greater force production during climbing but limited their ability to hyperextend the hip and walk as economically as modern humans, is published by Kozma et al. (2018).[362]
- Endocrania of two specimens of Australopithecus africanus from Sterkfontein Member 4 (South Africa) are virtually reconstructed by Beaudet et al. (2018).[363]
- A study on the paleoenvironment and diet of Australopithecus africanus and Paranthropus robustus as indicated by tooth microwear is published by Peterson et al. (2018).[364]
- A study on the relationship between root splay and overall morphology of first maxillary molars and jaw kinematics in South African Australopithecus africanus and Paranthropus robustus, and on its implications for inferring the dietary niches of these species, is published by Kupczik, Toro-Ibacache & Macho (2018).[365]
- A study on the variation in trabecular bone structure of the femoral head in fossil hominins attributed to the species Australopithecus africanus, Paranthropus robustus and to the genus Homo, attempting to reconstruct hip joint loading conditions in these fossil hominins, is published by Ryan et al. (2018).[366]
- A study on the habitats and diets of Paranthropus boisei and Homo rudolfensis from the Early Pleistocene of the Malawi Rift is published by Lüdecke et al. (2018).[367]
- A study on the strontium isotope data derived from three studies of teeth of Paranthropus robustus, and on its implications for inferring habitat, mobility and growth of this species, is published by Sillen & Balter (2018).[368]
- The skull of 'Mrs. Ples' (Sts 5 specimen of Australopithecus africanus) is interpreted as a skull of a small male rather than a large female individual by Tawane & Thackeray (2018).[369]
- A study on the variation in the structure of trabecular bone and joint loading in the humeral head of extant hominoids, spider monkeys and Australopithecus africanus is published by Kivell et al. (2018), who interpret their findings as indicating that A. africanus may have still used its forelimbs for arboreal locomotion.[370]
- Description of a nearly complete, 3.32-million-year-old foot of a juvenile Australopithecus afarensis from Dikika (Ethiopia) is published by DeSilva et al. (2018).[371]
- A study on the possible date of the first appearance of Australopithecus sediba as indicated by the average hominin species' temporal range is published by Robinson et al. (2018).[372]
- Studies on the anatomy of the skeleton of Australopithecus sediba are published by De Ruiter et al. (2018),[373] Williams et al. (2018),[374] Churchill et al. (2018),[375] Kivell et al. (2018),[376] Churchill et al. (2018),[377] DeSilva et al. (2018)[378] and Holliday et al. (2018).[379]
- A digital animation of the proposed walking mechanics of Australopithecus sediba is presented by Zhang & DeSilva (2018).[380]
- A study on the linear marks observed on the hominin fossil Stw53 from the Sterkfontein cave site (South Africa), evaluating whether these marks were cutmarks inflicted by stone tools or non-anthropic modifications, is published by Hanon, Péan & Prat (2018).[381]
- New artifacts are described from the Swartkrans cave (South Africa) by Kuman et al. (2018), who confirm the affinity of the Swartkrans artifacts with the Oldowan industrial complex.[382]
- Oldowan stone tools and associated hominin-modified fossil bones are reported from strata estimated to ≈2.4 and ≈1.9 Ma from two deposits at Ain Boucherit (Algeria) by Sahnouni et al. (2018).[383]
- Pelvic remains of Homo naledi from the Dinaledi Chamber in the Rising Star Cave system (Cradle of Humankind, South Africa) are described by VanSickle et al. (2018).[384]
- A study on the minimum number of individuals and on a demographic profile of the assemblage of Homo naledi individuals in the Dinaledi Chamber (Rising Star Cave system, South Africa) is published by Bolter et al. (2018).[385]
- A study on the diet of Homo naledi as indicated by teeth wear textures is published by Ungar & Berger (2018).[386]
- A study comparing tooth shape and size in Homo naledi and other South African Plio-Pleistocene hominins, as well as a study on the possible diet of Homo naledi, is published by Berthaume, Delezene & Kupczik (2018).[387]
- A study on the endocast morphology of Homo naledi, comparing it with other hominoids and fossil hominins, is published by Holloway et al. (2018).[388]
- A study on the phenetic affinities and taxonomic validity of Homo naledi as indicated by teeth morphology will be published by Irish et al. (2018).[389]
- Three incudes of Homo naledi recovered from the Dinaledi Chamber in the Rising Star cave system are described by Elliott et al. (2018).[390]
- Partial mandible of Homo naledi which was most likely affected by peripheral osteoma is reported by Odes et al. (2018).[391]
- A study on evaluating whether deliberate disposal of corpses is the only likely explanation for large assemblages of fossil human bones from the Middle Pleistocene sites of Sima de los Huesos (Spain) and the Dinaledi Chamber (South Africa) is published by Egeland et al. (2018).[392]
- A study on the phylogenetic relationships of the Pleistocene hominin specimen (a fragmented skullcap) from Kocabaş (Denizli Basin, Turkey) is published by Vialet et al. (2018).[393]
- A study on the morphology and affinities of the hominin calvaria KNM-ER 42700 from Ileret, Kenya is published by Neubauer et al. (2018).[394]
- A study on the frequency and location of hominin (likely Homo habilis) butchery marks and carnivore tooth marks on mammal bones from the HWK EE site (Olduvai Gorge, Tanzania), and on their implications for inferring carnivorous feeding behavior of the HWK EE hominins and the ecological interactions they had with carnivores, is published by Pante et al. (2018).[395]
- A study estimating possible adult stature and body mass of the Homo erectus specimen KNM-WT 15000 ("Turkana Boy") is published by Cunningham et al. (2018).[396]
- A study on the structure of the animal community known from the Okote Member of the Koobi Fora Formation at East Turkana (Kenya) as indicated by tracks and skeletal assemblages, and on the interactions of Homo erectus with environment and associated faunas from this site, is published by Roach et al. (2018).[397]
- A study on the large cutting tools from four Acheulean sites at Koobi Fora dated to ~1.4 million years ago, investigating the behavioural patterns underpinning recorded artefact variability, is published by Presnyakova et al. (2018).[398]
- A study on 1.07–0.99 million-year-old pelvic remains from Buia (Eritrea) is published by Hammond et al. (2018), who interpret their findings as indicating that the postcranial morphology of Homo erectus sensu lato was variable and, in some cases, nearly indistinguishable from modern human morphology, and that the shared last common ancestor of Late Pleistocene Homo species was unlikely to have an australopith-like pelvis.[399]
- A study on the humeral rigidity and strength in members of the species Homo erectus known from Zhoukoudian (China), comparing it with the humeral rigidity and strength in the African members of the species, is published by Xing et al. (2018).[400]
- A study on the morphology of teeth of Homo erectus from Zhoukoudian is published by Xing, Martinón-Torres & Bermúdez de Castro (2018).[401]
- A study on the age of the archaeological layers from the Zhoukoudian Upper Cave, and on its implications for understanding Late Quaternary human evolution in eastern Asia, is published by Li et al. (2018).[402]
- New magnetostratigraphic dating results for the Bailong Cave (China) sedimentary sequence containing hominin teeth assigned to the species Homo erectus are presented by Kong et al. (2018).[403]
- An Early Pleistocene artefact sequence, containing 17 artefact layers that extend from approximately 1.26 million years ago to about 2.12 million years ago, is described from the Shangchen locality (Loess Plateau, China) by Zhu et al. (2018), indicating that hominins left Africa earlier than indicated by the evidence from Dmanisi.[404]
- A study investigating how the hominin groups living in the Qinling Mountains range (China) responded to glacial–interglacial shifts from ~1.20 million years ago to ~0.05 million years ago is published by Sun et al. (2018).[405]
- A study on the morphology and affinities of the Middle Pleistocene hominin mandible recovered from La Niche cave site of the Montmaurin karst system (France) is published by Vialet et al. (2018).[406]
- Taphonomic signatures of the Aroeira 3 cranium, with a specific focus on cranial breakage, are described by Sanz et al. (2018), who attempt to approximate the cause of death of this individual.[407]
- A study on strategies for thermoregulation in the absence of fire in conditions experienced by hominins in north-west Europe before 400,000 years ago is published by MacDonald (2018).[408]
- Evidence for progressive aridification in East Africa since about 575,000 years before present, based on data from sediments from Lake Magadi (Kenya), is presented by Owen et al. (2018), who also evaluate the influence of the increasing Middle- to Late-Pleistocene aridification and environmental variability on the physical and cultural evolution of Homo sapiens in East Africa.[409]
- A series of excavated Middle Stone Age sites from the Olorgesailie Basin (Kenya), dated as ≈320,000 years old, is presented by Brooks et al. (2018), who report evidence of hominins preparing cores and points, exploiting iron-rich rocks to obtain red pigment, and procuring stone tool materials from ≥25–50 km distance.[410]
- A study on the environmental dynamics before and after the onset of the early Middle Stone Age in the Olorgesailie Basin (Kenya) is published by Potts et al. (2018).[411]
- A study on the chronology of the Acheulean and early Middle Stone Age sedimentary deposits in the Olorgesailie Basin (Kenya) is published by Deino et al. (2018).[412]
- A study on bone artefacts from Middle Stone Age layers at Sibudu Cave (South Africa), evaluating what kinds of animals were used to make bone tools, is published by Bradfield (2018).[413]
- A study on the stone tools from the Acheulean site of Saffaqah near Dawadmi (Saudi Arabia), and their implications for inferring how hominins adapted to this region, is published by Shipton et al. (2018).[414]
- A study on the stratigraphy, archaeology and chronology of the Saffaqah site, providing the first secure dates for this site, is published by Scerri et al. (2018).[415]
- A study on the age of stone tools from the Attirampakkam site in India is published by Akhilesh et al. (2018), indicating the emergence of a Middle Paleolithic culture in India at 385 ± 64 thousand years ago.[416]
- Stone tools associated with a skeleton of Rhinoceros philippinensis showing clear signs of butchery are described from a bone bed at Kalinga in the Cagayan Valley of northern Luzon (the Philippines), dated to between 777 and 631 thousand years ago, by Ingicco et al. (2018).[417]
- The study on the Cerutti Mastodon site published by Holen et al. (2017), reporting possible evidence of an unidentified species of the genus Homo living in California 130,000 years ago,[418] is criticized by Ferraro et al. (2018).[419][420]
- Bone retouchers dated as approximately 125–105,000 years old are described from the Lingjing site in Henan, China by Doyon et al. (2018), representing the first evidence from Eastern Asia for the use of bone as raw material to modify stone tools.[421]
- A 90,000-years-old specialized bone tool discovered in association with the Aterian techno-complex is described from the cave site of Dar es-Soltan 1 (Morocco) by Bouzouggar et al. (2018).[422]
- A study on the antiquity of the remains of Homo antecessor, based on the first direct Electron Spin Resonance dating of a tooth from the TD6 unit of Atapuerca Gran Dolina site (Spain), is published by Duval et al. (2018).[423]
- A study aiming to test the hypothesis if Homo antecessor molars approximated the Neanderthal rather than the Homo sapiens condition for tissue proportions and enamel thickness is published by Martín-Francés et al. (2018).[424]
- An assemblage of hominin tracks produced by adults and children potentially as young as 12 months, probably members of the species Homo heidelbergensis living 700,000 years ago, is described from the Upper Awash Valley (Ethiopia) by Altamura et al. (2018).[425]
- A study on the morphology and function of the browridge of the Kabwe 1 archaic hominin specimen is published by Godinho, Spikins & O'Higgins (2018).[426]
- A study intending to detect introgressed Denisovan genetic material in present-day human genomes is published by Browning et al. (2018), who report evidence of Denisovan ancestry in populations from East and South Asia and Papuans, and interpret their findings as indicating that at least two distinct instances of Denisovan admixture into modern humans occurred.[427]
- Genome recovered from a bone fragment from the Denisova Cave (Russia) is presented by Slon et al. (2018), who interpret the studied individual as the offspring of a Neanderthal mother and a Denisovan father.[428]
- A study on the absolute bone volume in five human long bones from the Sima de los Huesos site is published by Carretero et al. (2018), who interpret their findings as indicating that Sima de los Huesos hominins had on average heavier long bones than extant humans of the same size.[429]
- A study on the stone tools from the site of la Noira (France) and their implications for reconstructing early Acheulean hominin behavior is published by Hardy et al. (2018), who argue that the hominins from this site used a broad range of resources including wood, plants, mammals, and possibly birds and fish, and that Middle Pleistocene hominins had detailed local environmental knowledge and were able to adapt to a wide range of environments.[430]
- A study aiming to estimate total lung capacity of Neanderthals, as well as Early Pleistocene hominins from the Gran Dolina site ATD6 (Spain), is published by García-Martínez et al. (2018).[431]
- A series of partially charred wooden tools is described from the late Middle Pleistocene site of Poggetti Vecchi (central Italy) by Aranguren et al. (2018), who interpret their findings as indicating that Neanderthals were able to choose the appropriate timber and to process it with fire to produce tools.[432]
- A wooden tool (possibly a digging stick), likely produced by Neanderthals, is described from the early Late Pleistocene Aranbaltza III site (Basque Country, Spain) by Rios-Garaizar et al. (2018), representing the oldest wooden tool from southern Europe reported so far.[433]
- Cave art in Cave of La Pasiega, Maltravieso cave and Ardales cave (Spain) is dated as older than 64,000 years (thus predating the arrival of modern humans in Europe) by Hoffmann et al. (2018), who interpret their findings as indicative of Neandertal authorship of the art;[434] the study is subsequently criticized by Pearce & Bonneau (2018),[435][436] Aubert, Brumm & Huntley (2018),[437][438] Slimak et al. (2018)[439][440] and White et al. (2020).[441][442]
- A study on the age of the flowstone capping the Cueva de los Aviones deposit in southeast Spain is published by Hoffmann et al. (2018), who report that Neanderthal-associated evidence of symbolic behavior found at the site is 115,000 to 120,000 years old and predates the earliest known comparable evidence associated with modern humans by 20,000 to 40,000 years.[443]
- Genomes of five Neanderthals from Belgium (Spy Cave and Goyet Caves), France (Les Cottés cave), Croatia (Vindija Cave) and Russia (Mezmaiskaya cave), who lived around 39,000 to 47,000 years ago, are sequenced by Hajdinjak et al. (2018).[444]
- A study on Neanderthal skeletal remains and animal fossils from the Vindija Cave, and on their implications for inferring Neanderthal behaviour, is published by Patou-Mathis, Karavanić & Smith (2018).[445]
- A study evaluating three hypotheses forwarded to explain the distinctive Neanderthal face is published by Wroe et al. (2018).[446]
- A study evaluating ecological niche similarity between the datasets of morphologically diagnostic Neanderthal remains and of archaeological sites with Middle Paleolithic artifacts (but no diagnostic hominin remains), as well as assessing its implications for inferring whether those archaeological sites represent Neanderthal occurrences, is published by Bible & Peterson (2018).[447]
- Gaudzinski-Windheuser et al. (2018) report perforations observed on two fallow deer skeletons from the 120,000-year-old lake shore deposits from Neumark-Nord (Germany), interpreted as evidence of close-range use of thrusting spears by Neanderthals.[448]
- A study on the timing and duration of periods of climate deterioration in the interior of the Iberian Peninsula in the late Pleistocene, evaluating the impact of climate on the abandonment of inner Iberian territories by Neanderthals 42,000 years ago, is published by Wolf et al. (2018).[449]
- A study on pollen recovered from hyaena coprolites from Vanguard Cave (Gibraltar), and on its implications for reconstructing the vegetation landscapes in the environment inhabited by southern Iberian Neanderthals during the MIS 3, is published by Carrión et al. (2018).[450]
- Evidence of bird and carnivore exploitation by Neanderthals (cut-marks in golden eagle, raven, wolf and lynx remains) is reported from the Axlor site (Spain) by Gómez-Olivencia et al. (2018).[451]
- The first direct artefactual evidence for regular, systematic fire production by Neanderthals is reported from archaeological layers attributed to late Mousterian industries at multiple sites throughout France by Sorensen, Claud & Soressi (2018).[452]
- A study on Neanderthal manual activities is published by Karakostis et al. (2018), who report evidence of habitual performance of precision grasping by Neanderthals.[453]
- 3D virtual reconstruction of the thorax of the Kebara 2 Neanderthal individual is presented by Gómez-Olivencia et al. (2018).[454]
- A study aiming to determine whether metabolic differences between competing populations of Neanderthals and anatomically modern humans alone could have accounted for Neanderthal extinction, as well as investigating Neanderthal fire use, is published by Goldfield, Booton & Marston (2018).[455]
- A study on the climate changes in Europe during the Middle–Upper Paleolithic transition (based on speleothem records from the Ascunsă Cave and from the Tăușoare Cave, Romania), and on their implications for the replacement of Neanderthals by modern humans in Europe, is published by Fernández et al. (2018).[456]
- A study on the cultural attribution and stratigraphic integrity of the Neanderthal skeletal material from La Roche-à-Pierrot, Saint-Césaire (France), evaluating whether there is reliable evidence for a Neanderthal-Châtelperronian association at this site, is published by Gravina et al. (2018).[457]
- A study aiming to reconstruct 3D brain shape of Neanderthals and early Homo sapiens is published by Kochiyama et al. (2018).[458]
- A study on patterns of seasonal variation in the environment inhabited by Neanderthals, on Neanderthal life history and on their exposure to potential environmental hazards, as indicated by data from oxygen isotopes, trace element distributions and tooth development in two Neanderthals and one modern human from Payre (an archeological site in the Rhone Valley, France), is published by Smith et al. (2018).[459]
- A study on the human teeth from the Middle Pleistocene sites of Fontana Ranuccio and Visogliano (Italy), aiming to identify the presence, if any, of a Neanderthal-like signature in the inner structure of these teeth, is published by Zanolli et al. (2018).[460]
- Evidence indicating that interbreeding between Neanderthals and modern humans led to the exposure of each species to novel viruses and to the exchange of adaptive alleles that provided resistance against these viruses is presented by Enard & Petrov (2018).[461]
- A study on Neanderthals and early Upper Paleolithic anatomically modern humans, reassessing the hypothesis of higher skull trauma prevalence among Neanderthals than among anatomically modern humans, is published by Beier et al. (2018).[462]
- A study on the age of the Buran-Kaya III site in Crimea is published by Prat et al. (2018), who interpret their findings as casting doubt on the survival of Neanderthal refuge zones in Crimea 28,000 years before present, and indicating that the human remains from this site represent some of the oldest evidence of anatomically modern humans in Europe.[463]
- A study on the use of plants by early modern humans during the Middle Stone Age as indicated by analyses of phytoliths from the Pinnacle Point locality (South Africa) is published by Esteban et al. (2018).[464]
- A study on the climatic changes in the Lake Tana area in the last 150,000 years and their implications for early modern human dispersal out of Africa is published by Lamb et al. (2018).[465]
- A review of fossil, archaeological, genetic, and paleoenvironmental data on the origin of Homo sapiens is published by Scerri et al. (2018), who argue that Homo sapiens evolved within a set of interlinked groups living across Africa, whose connectivity changed through time, rather than from a single region/population in Africa.[466]
- A review of the archaeological and palaeoenvironmental datasets relating to the Middle–Late Pleistocene dispersal of Homo sapiens within and beyond Africa is published by Roberts & Stewart (2018), who argue that H. sapiens developed a new ecological niche.[467]
- A study on the evolution of modern human brain shape based on endocasts of Homo sapiens fossils from different geologic time periods is published by Neubauer, Hublin & Gunz (2018).[468]
- Late Pleistocene hominin tracks, probably produced by Homo sapiens, are described from the Waenhuiskrans Formation (South Africa) by Helm et al. (2018).[469]
- A study on the proxy evidence for environmental changes during past 116,000 years in lake sediment cores from the Chew Bahir basin, south Ethiopia (close to the key hominin site of Omo Kibish), and on its implications for inferring the environmental context for dispersal of anatomically modern humans from northeastern Africa, is published by Viehberg et al. (2018).[470]
- A study on the age of a modern human mandible with teeth from the Misliya cave (Mount Carmel, Israel) is published by Hershkovitz et al. (2018), who date the fossil as at least 177,000 years old, representing the oldest reported fossil of a member of the Homo sapiens clade found outside Africa.[471][472][473]
- A phalanx of a member of the species Homo sapiens is described from the ≈95–86,000 years old Al Wusta site (An Nafud, Saudi Arabia) by Groucutt et al. (2018), representing the oldest directly dated fossil of Homo sapiens found outside Africa and the Levant.[474]
- A study on the effects of the Toba supereruption in East Africa is published by Yost et al. (2018), who find no evidence of the eruption causing a volcanic winter in East Africa or a population bottleneck among African populations of anatomically modern humans.[475]
- Microscopic glass shards characteristic of the Youngest Toba Tuff (ashfall from the Toba eruption), dated as approximately 74,000 years old, are described from two archaeological sites on the south coast of South Africa by Smith et al. (2018), who interpret their findings as indicating that humans in this region thrived through the Toba event and the ensuing full glacial conditions.[476]
- Evidence of human activity dating back to 78,000 years ago is reported from the Panga ya Saidi cave (Kenya) by Shipton et al. (2018), who describe a rich technological sequence that includes lithic forms elsewhere associated with the Middle Stone Age and the Later Stone Age.[477]
- A cross-hatched pattern drawn with an ochre crayon is reported from approximately 73,000-year-old Middle Stone Age levels at Blombos Cave (South Africa) by Henshilwood et al. (2018), pre-dating previously known abstract and figurative drawings by at least 30,000 years.[478]
- A study on the age of the cave art from the Kapova Cave (Russia) is published by Dublyansky et al. (2018).[479]
- New rock art site, linkable chronoculturally to the Early Upper Paleolithic, is identified in Las Ventanas Cave (Spain) by Cortés-Sánchez et al. (2018).[480]
- Rock art, including a figurative painting of an animal dating to at least 40,000 years ago, is described from the Lubang Jeriji Saléh cave (East Kalimantan, Indonesia) by Aubert et al. (2018).[481]
- A study on changes in ochre use throughout an entire Upper Paleolithic sequence at Hohle Fels cave (Germany) is published by Velliky, Porr & Conard (2018).[482]
- A study on the timing and mechanisms of the initial colonization of the Nwya Devu Paleolithic site (Tibetan Plateau) by humans is published by Zhang et al. (2018).[483]
- A study on the human use of rainforest plant resources of prehistoric Sri Lanka, as indicated by data from phytoliths from the Fahien Rock Shelter sediments, is published by Premathilake & Hunt (2018).[484]
- A reassessment of the Late Pleistocene human occupation site at Leang Burung 2 (Sulawesi, Indonesia), presenting new stratigraphic information and dating evidence from the site, is published by Brumm et al. (2018).[485]
- A study on the timing of arrival of anatomically modern humans to Southeast Asia and Sahul is published by O'Connell et al. (2018), who consider it unlikely that the artifacts from Madjedbebe (northern Australia) reported by Clarkson et al. (2017)[486] are more than 50,000 years old.[487]
- A study investigating the most likely route used by early modern humans to colonize Sahul is published by Kealy, Louys & O'Connor (2018).[488]
- A study on the results of re-excavation of Karnatukul (Serpent's Glen rockshelter in the Australian Little Sandy Desert), as well as on the chronology of this site, is published by McDonald et al. (2018).[489]
- Genomic data from seven 15,000-year-old modern humans from Morocco, attributed to the Iberomaurusian culture, is presented by van de Loosdrecht et al. (2018), who report evidence of a genetic affinity of the studied individuals with early Holocene Near Easterners.[490]
- A study on charred food remains from Shubayqa 1, a Natufian hunter-gatherer site located in northeastern Jordan and dated to 14.6–11.6 ka cal BP, is published by Arranz-Otaegui et al. (2018), who interpret their findings as providing the earliest empirical evidence for the preparation of bread-like products by Natufian hunter-gatherers, predating the emergence of agriculture by at least 4,000 years.[491]
- A study on the timing of first human arrival in Madagascar, as indicated by evidence of prehistoric human modification of multiple elephant bird postcranial elements, is published by Hansford et al. (2018).[492]
- A study on the timing of human colonization of Madagascar, as indicated by data from butchery marks on megafaunal bones, radiocarbon chronology of bone deposits and an analysis of the sedimentary record, is published by Anderson et al. (2018).[493]
- Description of the morphology of three partial human mandibles from the Niah Caves (Sarawak, Malaysia) and a study on the age of these bones is published by Curnoe et al. (2018).[494]
- A study investigating whether the human population occupying Beringia during the Last Glacial Maximum represented an example of human adaptation to an extreme environment, focusing on gene variations which might have conferred advantage in transmitting nutrients from mother to infant through breast milk under conditions of extremely low UV, is published by Hlusko et al. (2018).[495]
- A review of the genetic, archeological and paleoecological data on the course of the settlement of the Americas is published by Potter et al. (2018), who argue that available evidence is consistent with an inland migration through an ice-free corridor or with a migration through Pacific coastal routes (or both), but neither can be rejected.[496]
- A study on the timing of the latest Pleistocene glaciation in southeastern Alaska and its implication for inferring the route and timing of early human migration to the Americas is published by Lesnek et al. (2018).[497]
- A study on the technological traits of fluted projectile points from northern Alaska and Yukon, in combination with artifacts from further south in Canada, the Great Plains, and eastern United States, evaluating the plausibility of historical relatedness and evolutionary patterns in the spread of fluted-point technology in North America in the latest Pleistocene and earliest Holocene, is published by Smith & Goebel (2018).[498]
- Late Pleistocene human footprints left by a minimum of three people are described from the Calvert Island (British Columbia, Canada) by McLaren et al. (2018).[499]
- Associated human and ground sloth tracks are described from the Rancholabrean deposits in the White Sands National Park (New Mexico, United States) by Bustos et al. (2018), who interpret their finding as evidence of humans actively stalking, harassing and likely hunting ground sloths in the late Pleistocene.[500]
- A study on the age of a series of sedimentary samples from the earliest cultural assemblage at the Gault Site (Texas, United States), including a previously unknown, early projectile point technology unrelated to Clovis, is published by Williams et al. (2018).[501]
- A robust lithic projectile point assemblage is reported from the layers dated between ≈13.5 and 15.5 ka ago at the Debra L. Friedkin site (Texas, United States) by Waters et al. (2018).[502]
- A study on the age of the Anzick burial site (Montana, United States) is published by Becerra-Valdivia et al. (2018).[503]
- The genome of two infants from the Upward Sun River site dated 11,500 years ago is sequenced, leading to the discovery of the Ancient Beringian ethnic group.[504][505]
- Scheib et al. (2018) sequence 91 ancient human genomes from California and southwestern Ontario, demonstrating the existence of two distinct ancestries in North America, and finding contribution from both of these ancestral populations in all modern Central and South Americans.[506]
- Posth et al. (2018) report genome-wide ancient DNA from 49 individuals from Central and South America, all dating to at least ~9,000 years ago, and interpret their finding as indicative of two previously undocumented genetic exchanges between North and South America.[507]
- A study on the history of dispersal and diversification of people within the Americas, based on data from ancient human genomes spanning Alaska to Patagonia, is published by Moreno-Mayar et al. (2018).[508]
- A study on the site context, geoarchaeology and material assemblages of the Valiente lithic workshop site (Chile) is published by Méndez et al. (2018).[509]
- Evidence of plant domestication and food production from the early and middle Holocene site of Teotonio (southwestern Amazonia, Brazil) is presented by Watling et al. (2018).[510]
- A study on the morphological affinity of the late Paleolithic human skull from the Zlatý kůň site in the Bohemian Karst (Czech Republic) is published by Rmoutilová et al. (2018), who also evaluate whether it is possible to determine the sex of the Zlatý kůň individual based on its skull morphology.[511]
- A study on the Mesolithic site of Star Carr, indicating that there was intensive human activity at the site for several hundred years when the community was subject to multiple, severe, abrupt climate events that impacted air temperatures, the landscape and the ecosystem of the region, is published by Blockley et al. (2018).[512]
- A study on the tools preserved with Ötzi, evaluating their implications for inferring Ötzi's individual history, the reconstruction of his last days and his cultural and social background, is published by Wierer et al. (2018).[513]
- A study on the contents of Ötzi's stomach is published by Maixner et al. (2018).[514]
- A study on the compositions of the faunal and stone artifact assemblages at Liang Bua (Flores, Indonesia), aiming to determine the last appearance dates of Stegodon, giant marabou stork, Old World vulture belonging to the genus Trigonoceps, and Komodo dragon at the Liang Bua site, and to determine what raw materials were preferred by hominins from this site ~50,000–13,000 years ago and whether these preferences were similar to those seen in the stone artifact assemblages attributed to Homo floresiensis or to those attributed to modern humans, is published by Sutikna et al. (2018).[515]
- A study on genetic variation among a population of Rampasasa pygmies living close to the cave where remains of Homo floresiensis were discovered is published by Tucci et al. (2018), who find evidence of admixture with Denisovans and Neanderthals but no evidence for gene flow with other archaic hominins, and interpret their findings as indicating that at least two independent instances of hominin insular dwarfism occurred on Flores.[516]
- A synthesis of patterns and incidences of developmental abnormalities and anomalies in the Pleistocene Homo fossil record is published by Trinkaus (2018).[517]
New taxa
| Name | Novelty | Status | Authors | Age | Unit | Location | Notes | Images |
|---|---|---|---|---|---|---|---|---|
| Sp. nov | Valid | Rose et al. | Cambay Shale Formation | |||||
| Gen. et sp. nov | Valid | Atwater & Kirk | A member of the family Omomyidae. Genus includes new species B. cerutti. | |||||
| Gen. et sp. nov | Valid | Atwater & Kirk | A member of the family Omomyidae. Genus includes new species E. walshi. | |||||
| Sp. nov | Valid | Godinot in Godinot et al. | ||||||
| Gen. et sp. nov | Valid | Atwater & Kirk | A member of the family Omomyidae. Genus includes new species G. randalli. | |||||
| Gen. et sp. nov | Valid | Turvey et al. | A gibbon. Genus includes new species J. imperialis. | |||||
| Gen. et sp. nov | Valid | Godinot, Senut & Pickford | Middle Eocene | A member of the family Adapidae belonging to the subfamily Caenopithecinae. The type species is N. interdictus. | ||||
| Gen. et sp. nov | Valid | Godinot in Godinot et al. | A member of the family Notharctidae. Genus includes new species R. pulcher. | |||||
| Sp. nov | Valid | Rossie & Hill | Middle Miocene | |||||
| Gen. et sp. et comb. nov | Valid | López-Torres, Silcox & Holroyd | Eocene (Uintan and Duchesnean) | A member of the family Omomyidae. The type species is W. esmaraldensis; genus also includes W. mcgrewi (Robinson, 1968) and W. shifrae (Krishtalka, 1978). |
Other eutherians
- Putative Cretaceous metatherian Sinodelphys szalayi is reinterpreted as an early member of Eutheria by Bi et al. (2018).[525]
- A study on the anatomy of the Early Cretaceous eutherian Endotherium niinomii is published by Wang et al. (2018), who consider this species to be a valid taxon.[526]
- Napoli et al. (2018) digitally visualize and describe the endocast of a taeniodont Onychodectes tisonensis.[527]
- A study evaluating when solenodons split from other eulipotyphlans, based on updated fossil calibrations, is published by Springer, Murphy & Roca (2018), who place the split between solenodons and other eulipotyphlans in the Late Cretaceous.[528]
- Fragment of the mandible of the mole Mongoloscapter zhegalloi is described from the Late Oligocene Tsakhir-Ula locality (Mongolia) by Lopatin (2018), representing the second record of Mongoloscapter reported so far.[529]
- A study comparing the size and morphology of the common shrew (Sorex araneus), Sorex runtonensis, the tundra shrew (S. tundrensis) and the Caucasian shrew (S. satununi) with the type material of the fossil shrew Sorex subaraneus (in order to either support or falsify the validity of S. subaraneus and the putative ancestry of the extant common shrew) is published by Rzebik-Kowalska & Pereswiet-Soltan (2018).[530]
- A study on the phylogenetic relationships of the gymnure Deinogalerix within the tribe Galericini is published by Borrani et al. (2018).[531][532]
- A study on the systematic usefulness of the humerus in proterotheriid litopterns is published by Corona, Perea & Ubilla (2018), who consider the species Proterotherium berroi Kraglievich (1930) to be a probable synonym of Neolicaphrium recens.[533]
- A study on the diversity of shapes of snout in notoungulates and on the evolution of the wide range of shapes of snout in this group of mammals is published by Gomes Rodrigues et al. (2018).[534]
- A study on the variation of teeth shape and on the factors affecting changes in the shape of teeth of notopithecid notoungulates is published by Scarano & Vera (2018).[535]
- A study on the variation of teeth shape in late Miocene members of the hegetotheriid notoungulate genus Paedotherium, as well as its implications for the systematics and phylogenetic relationships of the late Miocene species of Paedotherium, is published by Ercoli et al. (2018).[536]
- A study on the variability of the diagnostic characters in the fossils of members of the hegetotheriid notoungulate genus Tremacyllus is published by Sostillo, Cerdeño & Montalvo (2018), who consider the species T. incipiens to be a junior synonym of the species T. impressus.[537]
- New fossil remains of pachyrukhine hegetotheriid notoungulates are described from the Huayquerías del Este (Mendoza, Argentina) by Vera & Ercoli (2018), who consider the species Tremacyllus subdiminutus to be a synonym of T. impressus.[538]
- Fernández-Monescill et al. (2018) provide muscular reconstruction and infer functional properties of the forelimb of the mesotheriid notoungulate Plesiotypotherium achirense.[539]
- A study on the tooth wear, tooth replacement and enamel microstructure in a perissodactyl-like ungulate Cambaytherium is published by von Koenigswald et al. (2018).[540]
- Anatomical redescription of the periptychid species Periptychus carinidens is published by Shelley, Williamson & Brusatte (2018).[541]
- Description of new fossil material of the hyaenodont species Prionogale breviceps from the Miocene of Kenya and Uganda, and a study on the anatomy of teeth of Namasector soriae, is published by Morales & Pickford (2018).[542]
- Partial skull of Hyaenodon leptorhynchus is described from the Chattian deposits in Séon Saint-André (Marseille, France) by Solé et al. (2018).[543]
- A study on the early Pleistocene leporid fossils from the Roland Springs Ranch Locality 1 (Texas, United States), considered against the backdrop of Neogene-Quaternary faunal turnover that included the radiation within the subfamily Leporinae, is published by Moretti (2018).[544]
| Name | Novelty | Status | Authors | Age | Unit | Location | Notes | Images |
|---|---|---|---|---|---|---|---|---|
| Gen. et sp. nov | Valid | Bi et al. | An early eutherian. Genus includes new species A. zhoui. | |||||
| Sp. nov | Valid | López-Torres & Silcox | Early Eocene | Blackheath Beds | A member of Plesiadapiformes belonging to the family Paromomyidae. | |||
| Sp. nov | Valid | López-Torres & Silcox | Early Eocene | A member of Plesiadapiformes belonging to the family Paromomyidae. | ||||
| Sp. nov | Valid | De Bast, Gagnaison & Smith | Late Paleocene | A member of Plesiadapiformes belonging to the family Plesiadapidae. | ||||
| Sp. nov | Valid | Hooker | A member of the family Nyctitheriidae. | |||||
| Sp. nov | Valid | Solé et al. | A member of the family Mesonychidae. | |||||
| Sp. nov | Valid | Solé et al. | A member of the family Mesonychidae. | |||||
| Sp. nov | Valid | Wyss, Flynn & Croft | Early Oligocene | |||||
| Sp. nov | Valid | Wyss, Flynn & Croft | Early Oligocene | |||||
| Gen. et sp. nov | Valid | Carrillo et al. | Early Pliocene–late Pliocene or early Pleistocene | A member of Toxodontidae. Genus includes new species F. aguilerai. | ||||
| Gen. et sp. nov | Valid | Scott | A relative of Horolodectes. Genus includes new species F. sweeti. | |||||
| Sp. nov | Valid | Carrillo et al. | Middle Miocene | A member of Astrapotheriidae. | ||||
| Gen. et sp. nov | Valid | Lopatin & Averianov | Höovör locality | |||||
| Gen. et sp. nov | Valid | McGrath, Anaya & Croft | A member of Litopterna belonging the family Macraucheniidae. Genus includes new species L. shockeyi. | |||||
| Sp. nov | Valid | De Bast, Gagnaison & Smith | Late Paleocene | A member of Plesiadapiformes belonging to the family Plesiadapidae. | ||||
| Sp. nov | Valid | Jehle et al. | Late Paleocene | A member of Plesiadapiformes. | ||||
| Sp. nov | Valid | De Bast, Gagnaison & Smith | Late Paleocene | A member of Plesiadapiformes belonging to the family Plesiadapidae. | ||||
| Sp. nov | Valid | De Bonis et al. | Middle Eocene | Pondaung Formation | A member of the family Hyaenodontidae. | |||
| Gen. et comb. nov | Valid | Wyss, Flynn & Croft | Early Oligocene | A notohippid notoungulate; a new genus for "Eomorphippus" pascuali Simpson (1967). | ||||
| Gen. et comb. nov | Valid | Cerdeño, Vera & Combina | Early Miocene | A mesotheriid notoungulate; a new genus for "Trachytherus" mendocensis Simpson & Minoprio (1949). | ||||
| Gen. et sp. nov | Valid | Angelone et al. | Early Pleistocene | A member of the family Leporidae. Genus includes new species S. obscurus. | ||||
| Gen. et sp. nov | Valid | Zazhigin & Voyta | Middle Miocene | Oshin Suite | A shrew belonging to the subfamily Crocidosoricinae. The type species is S. angustirostris. | |||
| Gen. et sp. nov | Valid | Wyss, Flynn & Croft | Early Oligocene | A leontiniid notoungulate. Genus includes new species T. flacoensis. | ||||
| 'Theosodon' arozquetai[553] | Sp. nov | Valid | McGrath, Anaya & Croft | A member of Litopterna belonging the family Macraucheniidae, tentatively referred to the genus Theosodon. | ||||
| Wyonycteris kingi[559] | Sp. nov | Valid | Hooker | Paleogene | Woolwich |  United Kingdom | A member of the family Nyctitheriidae. Announced in 2018; the final version of the article naming it was published in 2020. | |
| Sp. nov | Valid | Armella, García-López & Dominguez | ||||||
| Gen. et sp. nov | Valid | López-Torres & Fostowicz-Frelik | Late Eocene | A relative of Anagale. The type species is Z. ergilinensis. |
Other mammals
- A diverse footprint assemblage dominated by small mammal tracks is described from the Lower Cretaceous Patuxent Formation (Maryland, United States) by Stanford et al. (2018), who name a new mammal ichnotaxon Sederipes goddardensis.[562]
- A description of the middle ear ossicles of Arboroharamiya is published by Meng et al. (2018).[563]
- Asymmetric bicrural stapes is reported in the Jurassic multituberculate Pseudobolodon oreas by Schultz, Ruf & Martin (2018).[564]
- New specimens of the cladotherian species Palaeoxonodon ooliticus (two partial dentaries) are described from the Middle Jurassic Kilmaluag Formation (Isle of Skye, Scotland, United Kingdom) by Panciroli, Benson & Butler (2018).[565]
- A fossil trackway produced by a mouse-sized primitive mammal, assigned to the ichnotaxon Ameghinichnus patagonicus, and deviating from the usual bilateral symmetry of posture and motion, is described from the Middle Jurassic of Patagonia, Argentina by Kuznetsov & Panyutina (2018), who interpret the tracks as most likely produced by a mammal carrying a heavy load on the left side of its body, plausibly a milk-producing mother carrying her babies.[566]
| Name | Novelty | Status | Authors | Age | Unit | Location | Notes | Images |
|---|---|---|---|---|---|---|---|---|
| Gen. et sp. nov | Castro et al. | An early member of Tribosphenida. The type species is B. stardusti. | ||||||
| Sp. nov | Valid | Scott, Weil & Theodor | Early Paleocene | A multituberculate belonging to the group Taeniolabidoidea. | ||||
| Gen. et sp. nov | Valid | Huttenlocker et al. | A member of Haramiyida belonging to the family Hahnodontidae. The type species is C. wahkarmoosuch. | |||||
| Gen. et sp. nov | Valid | Lofgren et al. | A multituberculate. Genus includes new species G. mylesi. | |||||
| Gen. et sp. nov | Valid | Averianov et al. | A member of Docodonta belonging to the family Tegotheriidae. The type species is K. yakutensis. | |||||
| Gen. et sp. nov | Disputed | Csiki-Sava et al. | A multituberculate belonging to the family Kogaionidae. The type species is L. tholocephalos. Smith et al. (2021) considered it to be a junior synonym of Barbatodon transylvanicus.[573] | |||||
| Gen. et sp. nov | Valid | Averianov et al. | A member of Eutriconodonta of uncertain phylogenetic placement. The type species is S. aquilonium. |
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