ライフサイエンスコーパス: Paleogene

1 ddle Ordovician-Carboniferous; Late Jurassic-Paleogene).

2 community in the latest Cretaceous and early Paleogene.

3 ns of the Eurasian landmass during the Early Paleogene.

4 fast sensitivity reach far beyond the early Paleogene.

5 f the angiosperms (flowering plants), then a Paleogene advance to ecological dominance in concert wit

6 Comparisons with other Paleogene Afro-Arabian forms are generally inconclusive.

7 cently, during the Late Cretaceous and early Paleogene, although the exact timing and cause of their

8 There appears to be a strong break between Paleogene and Neogene Asian anthropoid assemblages.

9 rations relevant for simulation of the early Paleogene, and (iii) fast or "Charney" climate sensitivi

10 f these groups are known to survive into the Paleogene, and their persistence into the latest Maastri

11 ost complete and best-preserved cranium of a Paleogene anthropoid ever found, that of a small female

12 deal of emphasis on the dental evidence for Paleogene anthropoid interrelationships, but cladistic a

13 propliopithecines than they are to any other Paleogene anthropoid taxon, and that Proteopithecus exhi

14 Paleogene arthropod biotas have proved important for tra

15 ation of anthracothere affinities with other Paleogene artiodactyls.

16 t establish synchrony between the Cretaceous-Paleogene boundary and associated mass extinctions with

17 itiated ~250,000 years before the Cretaceous-Paleogene boundary and that >1.1 million cubic kilometer

18 of mammalian groups crossing the Cretaceous-Paleogene boundary are lacking.

19 drop in delta(7)Li(SW) across the Cretaceous-Paleogene boundary cannot be produced by an impactor or

20 sil plant specimens, spanning the Cretaceous/Paleogene boundary in southwestern North Dakota.

21 The mass extinction at the Cretaceous-Paleogene boundary, approximately 66 Ma, is thought to b

22 nt estimated to be present at the Cretaceous-Paleogene boundary, produce what might have been one of

23 igate goethite spherules from the Cretaceous-Paleogene boundary, revealing the internal elemental dis

24 ion of non-avian dinosaurs at the Cretaceous-Paleogene boundary, triggered ecological diversification

25 extinction of pachycormids at the Cretaceous-Paleogene boundary, which is consistent with an opportun

26 inosaurs and continued across the Cretaceous-Paleogene boundary.

27 es, but did not change across the Cretaceous-Paleogene boundary.

28 vely cool temperatures across the Cretaceous-Paleogene boundary; there is no indication of a major wa

29 ure of atmospheric carbon dioxide (pCO2) and Paleogene climate is poorly resolved.

30 of model simulations using modern and early Paleogene configurations.

31 ith more generalized taxa from the Laurasian Paleogene (e.g., geolabidids, nyctitheriids, leptictids)

32 ose eruption played a role in the Cretaceous-Paleogene extinction event.

33 ional anatomy in mineralized arthropods from Paleogene fissure fillings and demonstrate the value of

34 Despite the large number of Paleogene fossil arthropods in Europe and North America

35 dition, a rich new harvest of Cretaceous and Paleogene fossils has helped to date the major evolution

36 agnitude of warming reconstructed from early Paleogene greenhouse climates and demands a close examin

37 diversity on land during the Mesozoic-early Paleogene interval, applying sample-standardization to a

38 The effect of the Cretaceous-Paleogene (K-Pg) (formerly Cretaceous-Tertiary, K-T) mas

39 The Cretaceous-Paleogene (K-Pg) boundary is marked by a major mass exti

40 origin of Schizophora within the Cretaceous-Paleogene (K-Pg) boundary, about 68.3 Ma.

41 in core Lamiales (CL) around the Cretaceous-Paleogene (K-Pg) boundary, and seven more in EDL relativ

42 gin of placentals relative to the Cretaceous-Paleogene (K-Pg) boundary, we scored 4541 phenomic chara

43 le placental ancestor crossed the Cretaceous-Paleogene (K-Pg) boundary.

44 fast radiations subsequent to the Cretaceous-Paleogene (K-Pg) event.

45 he 35 million years following the Cretaceous-Paleogene (K-Pg) extinction event.

46 their final disappearance at the Cretaceous-Paleogene (K-Pg) mass extinction event 66 Mya has been d

47 continues about the nature of the Cretaceous-Paleogene (K-Pg) mass extinction event.

48 The southernmost Cretaceous - Paleogene (K-Pg) outcrop exposure is the well-studied ex

49 ion of species richness after the Cretaceous/Paleogene (K/Pg) boundary deserves further examination i

50 he extinction of dinosaurs at the Cretaceous/Paleogene (K/Pg) boundary was the seminal event that ope

51 We find that the Cretaceous-Paleogene (K/Pg) extinction event marked a profound chan

52 nsequences of the end-Cretaceous [Cretaceous/Paleogene (K/Pg)] mass extinction persist in present-day

53 aceous Terrestrial Revolution and Cretaceous-Paleogene (KPg) mass extinction in opening up ecospace t

54 nd were a rare and endemic faunal element of Paleogene mammal assemblages of central Asia.

55 has produced Afro-Arabia's primary record of Paleogene mammalian evolution, including the world's mos

56 The Cretaceous-Paleogene mass extinction approximately 66 million years

57 n bird orders diverged before the Cretaceous-Paleogene mass extinction event 66 million years ago ins

58 uring a rapid radiation after the Cretaceous-Paleogene mass extinction event about 66 million years a

59 gies, and survivorship across the Cretaceous-Paleogene mass extinction event.

60 suggests a possible impact of the Cretaceous-Paleogene mass extinction on their radiation and that Br

61 portunities persisted through the Cretaceous-Paleogene mass extinction.

62 were relatively unaffected by the Cretaceous-Paleogene mass extinction.

63 were relatively unaffected by the Cretaceous-Paleogene mass extinction.

64 centals remain conspicuously absent from the Paleogene of Afro-Arabia.

65 he genus by at least 10 million years in the Paleogene of Asia, which closes the gap between Mimolagu

66 tion of tarsiers relative to anthropoids and Paleogene omomyids remains a subject of lively debate th

67 e reported from two of the best exemplars of Paleogene penguins yet recovered.

68 and postcranium of certain poorly understood Paleogene primates are clearly needed to help test wheth

69 estimates of the Late Eocene and Cretaceous/Paleogene projectiles are within 50% of independent esti

70 f the chronological evidence shared by later Paleogene strata exposed in Egypt and Oman (Taqah and Th

71 molluscs) from a highly expanded Cretaceous-Paleogene succession: the Lopez de Bertodano Formation o

72 important role in maintaining elevated early Paleogene temperatures, (ii) radiative forcing by carbon

73 play a substantial role in maintaining early Paleogene warmth.

74 thin a single biogeographic realm during the Paleogene, with a few long-distance dispersal events.