ライフサイエンスコーパス: Phanerozoic

1 helped prevent severe glaciation during the Phanerozoic.

2 seawater chemistry has fluctuated during the Phanerozoic.

3 SMT duplication event occurred later in the Phanerozoic.

4 invertebrate diversity dynamics through the Phanerozoic.

5 ost pronounced climatic perturbations of the Phanerozoic.

6 towards the end of the Proterozoic and early Phanerozoic.

7 re varied between 10% and 35% throughout the Phanerozoic.

8 ntle may have operated throughout the entire Phanerozoic.

9 ty is the predominant pattern throughout the Phanerozoic.

10 98 metazoan clades radiating throughout the Phanerozoic.

11 ly confined to the water column in the early Phanerozoic.

12 ontinental-scale marine transgression of the Phanerozoic.

13 tent macroevolutionary forces throughout the Phanerozoic.

14 nated in successive substages throughout the Phanerozoic.

15 abolic and ecological innovations during the Phanerozoic.

16 t major changes in Mg/Ca occurred during the Phanerozoic.

17 he radiation of higher life forms during the Phanerozoic.

18 are recorded in marine sedimentary rocks of Phanerozoic age and were associated with major extinctio

19 60 or so known terrestrial impact craters of Phanerozoic age, equivalent ejecta deposits within dista

20 the relationship between climate through the Phanerozoic and evolutionary patterns and diversity.

21 higher than modern levels during much of the Phanerozoic and it has hence been proposed that surface

22 values and concentrations much like those of Phanerozoic and modern marine carbonate rocks.

23 origination rates both declined through the Phanerozoic and that several extinctions in addition to

24 Neoproterozoic, roughly doubled by the Early Phanerozoic, and remained comparatively high until the C

25 The microbialite declines in the Phanerozoic are attributed to disruption of the mats by

26 cterized by pervasive anoxia relative to the Phanerozoic (at least approximately 30-40% of modern sea

27 most rapid and sustained increase in marine Phanerozoic biodiversity.

28 ntinental fragmentation have impacted global Phanerozoic biodiversity.

29 cambrian' life, and on the other the modern 'Phanerozoic' biosphere with its extraordinary diversity

30 r global marine fossil genera throughout the Phanerozoic, both before and after corrections for the i

31 ce of living agnathans, near the Proterozoic/Phanerozoic boundary (approximately 550Mya).

32 of widespread ocean oxygen deficiency in the Phanerozoic, coinciding with rapid atmospheric pCO2 incr

33 mparted by the balanced feedbacks modulating Phanerozoic deglaciation.

34 genian have never been replicated during the Phanerozoic despite similar, and sometimes more dramatic

35 se clades, extant diversity reflects largely Phanerozoic diversification.

36 The analysis of Madin et al. of Phanerozoic diversity failed to support expected correla

37 bined to produce the long-term trajectory of Phanerozoic diversity.

38 tion is one of the five most catastrophic in Phanerozoic Earth history.

39 helped to prevent snowball glaciation on the Phanerozoic Earth.

40 ites and hardgrounds--the substrates for pre-Phanerozoic endoliths--provide a hitherto poorly explore

41 educing ocean-atmosphere system, whereas the Phanerozoic eon (less than 542 million years ago) is kno

42 road picture of CO2 variation throughout the Phanerozoic eon (the past 544 Myr), inconsistencies and

43 New calculations of carbon fluxes during the Phanerozoic eon (the past 550 million years) illustrate

44 Cold subduction typical of the Phanerozoic eon favours the preservation of oxidized car

45 plant fossils, and biological soil crusts of Phanerozoic eon sandy palaeosols.

46 e invertebrate biodiversity patterns for the Phanerozoic Eon while controlling for sampling effort.

47 tions have been relatively constant over the Phanerozoic eon, the past 542 million years (Myr) of Ear

48 s ago) was one of the warmest periods of the Phanerozoic eon, with tropical sea surface temperatures

49 a minor player in sulfur cycling through the Phanerozoic Eon.

50 ough homogenous waters during periods of the Phanerozoic eon.

51 isted or returned in the oceans of the early Phanerozoic eon.

52 g composition of the marine biota during the Phanerozoic eon.

53 , nor fully oxic as supposed for most of the Phanerozoic eon.

54 est and most severe glaciation of the entire Phanerozoic Eon.

55 The transition between the Proterozoic and Phanerozoic eons, beginning 542 million years (Myr) ago,

56 In addition, the Phanerozoic eustasy record indicates that the claimed ef

57 cs are identical to those of well-understood Phanerozoic examples that lithified in coastal pore flui

58 y interpreted in the same way as is done for Phanerozoic examples.

59 me previous analyses of the 540-million-year Phanerozoic fossil record found a contrary relationship,

60 ntroduce a new database of this kind for the Phanerozoic fossil record of marine invertebrates.

61 of marine metazoans correlate throughout the Phanerozoic fossil record regardless of corrections and

62 A data set containing global occurrences of Phanerozoic fossils of benthic marine invertebrates show

63 ns derived from phylogenetically unambiguous Phanerozoic fossils of multicellular plants and animals.

64 os from the late Neoproterozoic and earliest Phanerozoic have caused much excitement because they pre

65 mposition of Earth's marine biota during the Phanerozoic have historically been explained in two diff

66 Unlike the familiar Phanerozoic history of life, evolution during the earlie

67 The Phanerozoic history of microbial endoliths has been eluc

68 tion (PTME), the most catastrophic crisis in Phanerozoic history.

69 fossil assemblages of marine organisms from Phanerozoic (i.e., Cambrian to Recent) assemblages indic

70 Phanerozoic levels of atmospheric oxygen relate to the b

71 However, although Archaean and Phanerozoic lithosphere differ in their thickness and co

72 tures previously calculated for steady-state Phanerozoic mantle plumes.

73 order control on the long-term trajectory of Phanerozoic marine animal diversity.

74 to rates of origination and extinction among Phanerozoic marine animal genera.

75 of continuing uncertainties over patterns of Phanerozoic marine diversity and the variety of factors

76 ttern of sponge abundance during collapse of Phanerozoic marine ecosystems.

77 tion and origination rates across the entire Phanerozoic marine fossil record.

78 A leading hypothesis explaining Phanerozoic mass extinctions and associated carbon isoto

79 Because the record of Phanerozoic mass extinctions and postextinction recoveri

80 The model allows us to calculate a Phanerozoic O(2) history that agrees with independent mo

81 ater Precambrian, and were even a feature of Phanerozoic ocean anoxic events.

82 ong Java Plateau, reveal preservation to the Phanerozoic of tungsten isotopic heterogeneities in the

83 ful pattern of enrichment in 13C relative to Phanerozoic or earlier Proterozoic samples.

84 tio of seawater remained constant during the Phanerozoic or underwent substantial secular change.

85 deeper portions (45 to 100 kilometers) yield Phanerozoic Os model ages and show evidence for extensiv

86 Independent models predicting the Phanerozoic (past 600 million years) history of atmosphe

87 n the ALDH 3/10/7/8 gene cluster occurred in Phanerozoic period (about 300 million years ago).

88 ratons are stronger than surrounding younger Phanerozoic provinces.

89 The canonical five mass extinctions of the Phanerozoic reveals the loss of different, albeit someti

90 Neoproterozoic land surface, followed by the Phanerozoic rise of vascular plants.

91 change and paleoenvironmental conditions in Phanerozoic rocks.

92 We review Phanerozoic sea-level changes [543 million years ago (Ma

93 dation Event (GOE), and is traceable through Phanerozoic shales to modern marine settings, where mari

94 ry success of planktic calcifiers during the Phanerozoic stabilized the climate system by introducing

95 of Proterozoic-style microbial matgrounds by Phanerozoic-style bioturbated mixgrounds.

96 ppears to fluctuate during the course of the Phanerozoic, the eon during which hard shells and skelet

97 geological systems or periods into which the Phanerozoic, the fossiliferous last 540 million years, o

98 four of the Big Five mass extinctions of the Phanerozoic, the marine genera that survived the extinct

99 Throughout most of the Phanerozoic, the random-walk null hypothesis is not reje

100 partial pressure of atmospheric oxygen over Phanerozoic time are constrained by the mass balances re

101 estimates of paleoseawater composition over Phanerozoic time as inputs and (87)Sr/(86)Sr of ophiolit

102 from similar depositional environments from Phanerozoic time, we find evidence for inhibited oxidati

103 with survivorship for the great majority of Phanerozoic time.

104 roductivity would double or triple with each Phanerozoic transition from low to high CO(2), productiv

105 ntary rocks deposited across the Proterozoic-Phanerozoic transition record extreme climate fluctuatio

106 y Archean pH values between 6.5 and 7.0 and Phanerozoic values between 7.5 and 9.0, which was cause

107 nction, the most severe biotic crisis in the Phanerozoic, was accompanied by climate change and expan

108 hroughout the bilaterian tree and across the Phanerozoic), we estimate that the last common ancestor

109 Unlike in the late Neoproterozoic and Phanerozoic, when negative delta(82/78)Se values are obs

110 greater extent than typical for most of the Phanerozoic, which can be attributed both directly and i

111 es by a factor of approximately 1.6 over the Phanerozoic, with minima when seawater Mg and SO4 are lo

112 ites are among the best-known fossils of the Phanerozoic, yet their habitat is poorly understood.