戻る
「早戻しボタン」を押すと検索画面に戻ります。 [閉じる]

コーパス検索結果 (１語後でソート)

通し番号をクリックするとPubMedの該当ページを表示します
1 uantify regional-scale diversity through the Phanerozoic.
2 tent macroevolutionary forces throughout the Phanerozoic.
3 nated in successive substages throughout the Phanerozoic.
4 t major changes in Mg/Ca occurred during the Phanerozoic.
5 he radiation of higher life forms during the Phanerozoic.
6 seawater chemistry has fluctuated during the Phanerozoic.
7 evere terrestrial ecosystem collapses of the Phanerozoic.
8 sity and evolutionary novelty throughout the Phanerozoic.
9 cceeded by overall smaller variations in the Phanerozoic.
10 erozoic, and bacterial families prior to the Phanerozoic.
11 tary mixed and transition layers through the Phanerozoic.
12 n increase in alpha diversity throughout the Phanerozoic.
13  direct driver of extinctions throughout the Phanerozoic.
14 kedly nutrient-rich crust at the dawn of the Phanerozoic.
15 nsk event, the first major extinction of the Phanerozoic.
16 out carbonate ramps and platforms during the Phanerozoic.
17 trajectory of marine biodiversity during the Phanerozoic.
18 c-like marine redox conditions well into the Phanerozoic.
19  twelve marine evaporite basins spanning the Phanerozoic.
20  process never reached saturation during the Phanerozoic.
21 decrease in true polar wander rates into the Phanerozoic.
22 the thickest crust formed in the Archean and Phanerozoic.
23 e the most productive reef ecosystems of the Phanerozoic.
24  invertebrate diversity dynamics through the Phanerozoic.
25  and biological utilization of seawater P in Phanerozoic.
26 abolic and ecological innovations during the Phanerozoic.
27  helped prevent severe glaciation during the Phanerozoic.
28  SMT duplication event occurred later in the Phanerozoic.
29 ost pronounced climatic perturbations of the Phanerozoic.
30 towards the end of the Proterozoic and early Phanerozoic.
31 re varied between 10% and 35% throughout the Phanerozoic.
32 ntle may have operated throughout the entire Phanerozoic.
33 ty is the predominant pattern throughout the Phanerozoic.
34  98 metazoan clades radiating throughout the Phanerozoic.
35 ly confined to the water column in the early Phanerozoic.
36 ontinental-scale marine transgression of the Phanerozoic.
37 gical impact in the biosphere throughout the Phanerozoic [1].
38 of the five main extinction intervals of the Phanerozoic Aeon.
39  are recorded in marine sedimentary rocks of Phanerozoic age and were associated with major extinctio
40 60 or so known terrestrial impact craters of Phanerozoic age, equivalent ejecta deposits within dista
41 pulses, during warming events throughout the Phanerozoic and 2) that conifer extinction increased sig
42 ost known porphyry Cu deposits formed in the Phanerozoic and are exclusively associated with moderate
43 the relationship between climate through the Phanerozoic and evolutionary patterns and diversity.
44  the most severe ecological event during the Phanerozoic and has long been presumed contemporaneous a
45 higher than modern levels during much of the Phanerozoic and it has hence been proposed that surface
46 values and concentrations much like those of Phanerozoic and modern marine carbonate rocks.
47  origination rates both declined through the Phanerozoic and that several extinctions in addition to
48 the most severe mass extinction event of the Phanerozoic and was followed by a several million-year d
49 roductivity (~100-fold lower than during the Phanerozoic) and enhanced preservation under anoxic cond
50 ciation, increased atmospheric oxygen in the Phanerozoic, and enhanced continental weathering.
51 Neoproterozoic, roughly doubled by the Early Phanerozoic, and remained comparatively high until the C
52 e, the paleogeographic position of all major Phanerozoic arc-continent collisions was reconstructed a
53             The microbialite declines in the Phanerozoic are attributed to disruption of the mats by
54 cterized by pervasive anoxia relative to the Phanerozoic (at least approximately 30-40% of modern sea
55 its diversification with the Proterozoic and Phanerozoic atmospheric oxygenation.
56 ical big five mass extinctions) early in the Phanerozoic being a direct consequence of limited early
57  sea level play an important role in driving Phanerozoic biodiversity at timescales >50 Myr, and duri
58  megafloral ecosystems surviving the largest Phanerozoic biodiversity crisis.
59 to what degree they impact broader trends in Phanerozoic biodiversity.
60 ydrogen sulfide toxicity was a key driver of Phanerozoic biodiversity.
61 ntinental fragmentation have impacted global Phanerozoic biodiversity.
62  most rapid and sustained increase in marine Phanerozoic biodiversity.
63 l shifts related to the establishment of the Phanerozoic biosphere.
64 cambrian' life, and on the other the modern 'Phanerozoic' biosphere with its extraordinary diversity
65 r global marine fossil genera throughout the Phanerozoic, both before and after corrections for the i
66 l P concentrations across the Neoproterozoic-Phanerozoic boundary (600 to 400 million years), showing
67 ce of living agnathans, near the Proterozoic/Phanerozoic boundary (approximately 550Mya).
68 e third largest mass extinction event in the Phanerozoic, characterized by a rise in CO(2) -concentra
69                                          The Phanerozoic climate has been interrupted by two long "ic
70 d, which may help to explain large shifts in Phanerozoic climate.
71 of widespread ocean oxygen deficiency in the Phanerozoic, coinciding with rapid atmospheric pCO2 incr
72  Early Paleozoic than during the rest of the Phanerozoic, consistent with extinction rates derived fr
73 ndrite break-up, the only resolvable peak in Phanerozoic cratering rates indicative of an asteroid sh
74 ass extinction (LOME) was the second largest Phanerozoic crisis, but its cause remains elusive.
75 mparted by the balanced feedbacks modulating Phanerozoic deglaciation.
76             Our comprehensive compilation of Phanerozoic delta(18)O data for carbonate and phosphate
77 genian have never been replicated during the Phanerozoic despite similar, and sometimes more dramatic
78 se clades, extant diversity reflects largely Phanerozoic diversification.
79              The analysis of Madin et al. of Phanerozoic diversity failed to support expected correla
80  fossil record transforms interpretations of Phanerozoic diversity patterns and their macroevolutiona
81 bined to produce the long-term trajectory of Phanerozoic diversity.
82 tion is one of the five most catastrophic in Phanerozoic Earth history.
83 helped to prevent snowball glaciation on the Phanerozoic Earth.
84 an important driver of the assembly of later Phanerozoic ecologies.
85 bundance of algal food sources comparable to Phanerozoic ecosystems.
86 ites and hardgrounds--the substrates for pre-Phanerozoic endoliths--provide a hitherto poorly explore
87 harp contrast to organic-rich rocks from the Phanerozoic Eon (10 to 100 m/Ma).
88 educing ocean-atmosphere system, whereas the Phanerozoic eon (less than 542 million years ago) is kno
89 road picture of CO2 variation throughout the Phanerozoic eon (the past 544 Myr), inconsistencies and
90 New calculations of carbon fluxes during the Phanerozoic eon (the past 550 million years) illustrate
91 nts how continental rearrangement during the Phanerozoic Eon drives profound variations in ocean oxyg
92               Cold subduction typical of the Phanerozoic eon favours the preservation of oxidized car
93 vironmental and biological properties of the Phanerozoic Eon from various published data sets and con
94      They have a rich fossil record from the Phanerozoic eon lending insight into the early history o
95 plant fossils, and biological soil crusts of Phanerozoic eon sandy palaeosols.
96 versification model that reproduces the main Phanerozoic eon trends in the global diversity of marine
97 e invertebrate biodiversity patterns for the Phanerozoic Eon while controlling for sampling effort.
98 tions have been relatively constant over the Phanerozoic eon, the past 542 million years (Myr) of Ear
99 s ago) was one of the warmest periods of the Phanerozoic eon, with tropical sea surface temperatures
100 , nor fully oxic as supposed for most of the Phanerozoic eon.
101 est and most severe glaciation of the entire Phanerozoic Eon.
102  directly quantitatively compared across the Phanerozoic eon.
103 r deep-mantle source compositions during the Phanerozoic Eon.
104 weathering and carbon sequestration over the Phanerozoic Eon.
105 story of tidal energy dissipation during the Phanerozoic Eon.
106  long before evolution of land plants in the Phanerozoic Eon.
107 a minor player in sulfur cycling through the Phanerozoic Eon.
108 ough homogenous waters during periods of the Phanerozoic eon.
109 isted or returned in the oceans of the early Phanerozoic eon.
110 g composition of the marine biota during the Phanerozoic eon.
111   The transition between the Proterozoic and Phanerozoic eons, beginning 542 million years (Myr) ago,
112 ospheric thinning during the Proterozoic and Phanerozoic eons, the lithosphere beneath many cratons s
113                             In addition, the Phanerozoic eustasy record indicates that the claimed ef
114 ve deep-ocean anoxia developing in the early Phanerozoic even under modern pO(2).
115 's growth environment were driven by various Phanerozoic events: specifically, the middle to late Pal
116 f the Cambrian explosion, after which normal Phanerozoic evolutionary rates were established.
117 cs are identical to those of well-understood Phanerozoic examples that lithified in coastal pore flui
118 y interpreted in the same way as is done for Phanerozoic examples.
119                                     The sole Phanerozoic exception to this pattern of global sea leve
120 obal flooded continental area throughout the Phanerozoic exhibits diversity levels approaching ecolog
121                                        Other Phanerozoic extinctions have also been related to the ex
122 ge igneous provinces (LIPs) and intervals of Phanerozoic faunal turnover that has been much discussed
123 ediments representing 15 time-windows in the Phanerozoic for content of micrometeoritic relict chrome
124 me previous analyses of the 540-million-year Phanerozoic fossil record found a contrary relationship,
125 ntroduce a new database of this kind for the Phanerozoic fossil record of marine invertebrates.
126 of marine metazoans correlate throughout the Phanerozoic fossil record regardless of corrections and
127  the temporal co-occurrence structure of the Phanerozoic fossil record, covering 1,273,254 occurrence
128 n established but unexplained feature of the Phanerozoic fossil record.
129  A data set containing global occurrences of Phanerozoic fossils of benthic marine invertebrates show
130 ns derived from phylogenetically unambiguous Phanerozoic fossils of multicellular plants and animals.
131 iversity of benthic marine invertebrates for Phanerozoic geological formations.
132 (2) as the dominant control on variations in Phanerozoic global climate and suggesting an apparent Ea
133 variables on global plant biomass across the Phanerozoic has not yet been established.
134 nction (PTME), the most severe crisis of the Phanerozoic, has been attributed to intense global warmi
135 ction, the most devastating biocrisis of the Phanerozoic, has been widely attributed to eruptions of
136 os from the late Neoproterozoic and earliest Phanerozoic have caused much excitement because they pre
137 mposition of Earth's marine biota during the Phanerozoic have historically been explained in two diff
138 tion (EPE), the largest biotic crisis of the Phanerozoic, have not resolved the timing of events in s
139                          Unlike the familiar Phanerozoic history of life, evolution during the earlie
140                                          The Phanerozoic history of microbial endoliths has been eluc
141 tion (PTME), the most catastrophic crisis in Phanerozoic history.
142  fossil assemblages of marine organisms from Phanerozoic (i.e., Cambrian to Recent) assemblages indic
143  continental LIPs and faunal turnover in the Phanerozoic is unlikely to occur by chance, suggesting a
144       We present compiled data that indicate Phanerozoic island arc igneous rocks are more oxidized (
145                       Average V/Sc ratios of Phanerozoic island arc rocks are elevated (by +1.1) comp
146 c magmatism dominates crust formation in the Phanerozoic, its role in earlier Earth history remains u
147 northwestern China, one of the largest known Phanerozoic lakes, during Early Permian climate warming.
148 ated large-scale spatial patterns during the Phanerozoic (last 541 million years).
149                                              Phanerozoic levels of atmospheric oxygen relate to the b
150                                     Numerous Phanerozoic limestones are comprised of diagenetic calci
151    These data show that the vast majority of Phanerozoic limestones characterized by rhombic microcry
152  demonstrate that the second-most-voluminous Phanerozoic LIP, the Kerguelen LIP, may have contributed
153               However, although Archaean and Phanerozoic lithosphere differ in their thickness and co
154                  For comparison, we compiled Phanerozoic (<500 Ma) data from comparable depositional
155 tures previously calculated for steady-state Phanerozoic mantle plumes.
156 order control on the long-term trajectory of Phanerozoic marine animal diversity.
157 to rates of origination and extinction among Phanerozoic marine animal genera.
158                We examine how the history of Phanerozoic marine biodiversity relates to environmental
159 of continuing uncertainties over patterns of Phanerozoic marine diversity and the variety of factors
160 ttern of sponge abundance during collapse of Phanerozoic marine ecosystems.
161 tion and origination rates across the entire Phanerozoic marine fossil record.
162 f-supporting regions in the fossil record of Phanerozoic marine invertebrates.
163              A leading hypothesis explaining Phanerozoic mass extinctions and associated carbon isoto
164                        Because the record of Phanerozoic mass extinctions and postextinction recoveri
165  Province eruptions coincide with many major Phanerozoic mass extinctions, suggesting a cause-effect
166 the Nama interval, comparable to loss during Phanerozoic mass extinctions.
167 k, reveals saw-toothed fluctuations around a Phanerozoic mean of 18.6 million years.
168           The model allows us to calculate a Phanerozoic O(2) history that agrees with independent mo
169  seafloor anoxic area for other CO(2)-driven Phanerozoic OAEs, suggest a common response of ocean ano
170 ater Precambrian, and were even a feature of Phanerozoic ocean anoxic events.
171 ong Java Plateau, reveal preservation to the Phanerozoic of tungsten isotopic heterogeneities in the
172 ful pattern of enrichment in 13C relative to Phanerozoic or earlier Proterozoic samples.
173 tio of seawater remained constant during the Phanerozoic or underwent substantial secular change.
174 deeper portions (45 to 100 kilometers) yield Phanerozoic Os model ages and show evidence for extensiv
175 ra, whose diversification happened after the Phanerozoic Oxidation Event (0.45-0.4 Ga), in which oxyg
176            Independent models predicting the Phanerozoic (past 600 million years) history of atmosphe
177 n the ALDH 3/10/7/8 gene cluster occurred in Phanerozoic period (about 300 million years ago).
178 urther, these trace fossils persist into the Phanerozoic, providing a critical link between Ediacaran
179 ratons are stronger than surrounding younger Phanerozoic provinces.
180          Frequency analyses of the deep-time Phanerozoic record of DZ U-Pb and ZHe ages demonstrate a
181                      The published Tonian to Phanerozoic record of interpreted non-spiculate sponges
182 ent of accretion of the fertile SCLM in many Phanerozoic regions are poorly constrained.
183 ntinental lithospheric mantle (SCLM) beneath Phanerozoic regions is mostly constituted by fertile lhe
184   The canonical five mass extinctions of the Phanerozoic reveals the loss of different, albeit someti
185 Neoproterozoic land surface, followed by the Phanerozoic rise of vascular plants.
186  change and paleoenvironmental conditions in Phanerozoic rocks.
187  for about two billion years until the early Phanerozoic, roughly 0.5 billion years ago.
188 e thus conclude that the fertile sections of Phanerozoic SCLM can be accreted during "recent" events
189  of melting associated with the formation of Phanerozoic SCLM or from the refertilization of ancient
190  America is an exaggerated global M-curve of Phanerozoic sea level.
191                                    We review Phanerozoic sea-level changes [543 million years ago (Ma
192 record, separating Precambrian basement from Phanerozoic sedimentary rocks.
193 mpact record, and the first-order pattern of Phanerozoic sedimentation can together be explained by s
194 dation Event (GOE), and is traceable through Phanerozoic shales to modern marine settings, where mari
195 mixed and transition layers evolved over the Phanerozoic since animals first began to extensively col
196         The Chengjiang Biota is the earliest Phanerozoic soft-bodied fossil assemblage offering the m
197 ry success of planktic calcifiers during the Phanerozoic stabilized the climate system by introducing
198 of Proterozoic-style microbial matgrounds by Phanerozoic-style bioturbated mixgrounds.
199 ose a previously overlooked coupling between Phanerozoic tectonic cycles, the major-element compositi
200 e passive margin record, benchmarked against Phanerozoic tectonic velocities.
201 re we document patterns of local richness in Phanerozoic terrestrial tetrapods using a global data se
202 ppears to fluctuate during the course of the Phanerozoic, the eon during which hard shells and skelet
203 geological systems or periods into which the Phanerozoic, the fossiliferous last 540 million years, o
204 four of the Big Five mass extinctions of the Phanerozoic, the marine genera that survived the extinct
205                       Throughout most of the Phanerozoic, the random-walk null hypothesis is not reje
206  partial pressure of atmospheric oxygen over Phanerozoic time are constrained by the mass balances re
207  estimates of paleoseawater composition over Phanerozoic time as inputs and (87)Sr/(86)Sr of ophiolit
208             We calculated C:N:P(org) through Phanerozoic time by including nutrient- and temperature-
209                            Unexpectedly, our Phanerozoic time windows show a stable flux dominated by
210                                         Over Phanerozoic time, ecosystems have become more productive
211  from similar depositional environments from Phanerozoic time, we find evidence for inhibited oxidati
212  with survivorship for the great majority of Phanerozoic time.
213 ssil record across the last ~538.8 Ma of the Phanerozoic to investigate the presence and strength of
214                                              Phanerozoic transgressions relative to long-term changes
215 roductivity would double or triple with each Phanerozoic transition from low to high CO(2), productiv
216 ntary rocks deposited across the Proterozoic-Phanerozoic transition record extreme climate fluctuatio
217 rder control on extinction rates through the Phanerozoic using a combined Earth system and ecophysiol
218 ly Archean pH values between 6.5 and 7.0 and Phanerozoic values between 7.5 and 9.0, which was caused
219 orcing shaped the evolutionary trajectory of Phanerozoic vegetated icehouses.
220  of the three major marine faunas during the Phanerozoic was intimately coupled to the evolution of t
221 nction, the most severe biotic crisis in the Phanerozoic, was accompanied by climate change and expan
222 hroughout the bilaterian tree and across the Phanerozoic), we estimate that the last common ancestor
223 er has not evolved substantially through the Phanerozoic, we interpret this record as primarily refle
224        Unlike in the late Neoproterozoic and Phanerozoic, when negative delta(82/78)Se values are obs
225  greater extent than typical for most of the Phanerozoic, which can be attributed both directly and i
226 zircon have been shown to faithfully reflect Phanerozoic whole-rock-based plate-tectonic discriminato
227 es by a factor of approximately 1.6 over the Phanerozoic, with minima when seawater Mg and SO4 are lo
228 ites are among the best-known fossils of the Phanerozoic, yet their habitat is poorly understood.

 
Page Top