Did cooling oceans trigger Ordovician biodiversification? Evidence from conodont thermometry
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Graptolite community responses to global climate change and the Late Ordovician mass extinctionOnset of main Phanerozoic marine radiation sparked by emerging Mid Ordovician icehouseDiversity partitioning during the Cambrian radiationClimate change and the selective signature of the Late Ordovician mass extinctionPolar front shift and atmospheric CO2 during the glacial maximum of the Early Paleozoic Icehouse.The magnitude and duration of Late Ordovician-Early Silurian glaciation.Pulse of atmospheric oxygen during the late Cambrian.The nature of Ordovician limestone-marl alternations in the Oslo-Asker District (Norway): witnesses of primary glacio-eustasy or diagenetic rhythms?Comment on "Lethally hot temperatures during the Early Triassic greenhouse".Seaweed morphology and ecology during the great animal diversification events of the early Paleozoic: A tale of two floras.First plants cooled the OrdovicianTrilobites from the Middle Ordovician Stairway Sandstone, Amadeus Basin, central AustraliaAn early Cambrian greenhouse climate.Quantifying ecological impacts of mass extinctions with network analysis of fossil communities.Early Palaeozoic ocean anoxia and global warming driven by the evolution of shallow burrowing.Evidence of nearby supernovae affecting life on EarthClimates of the Earth and Cryosphere EvolutionPacing of Paleozoic macroevolutionary rates by Milankovitch grand cyclesThe Hirnantian (Late Ordovician) and end-Guadalupian (Middle Permian) mass-extinction events comparedOxygenation as a driver of the Great Ordovician Biodiversification EventEcological revolution of Oklahoma's rhynchonelliform brachiopod fauna during the Great Ordovician Biodiversification EventHow is biodiversity produced? Examining speciation processes during the GOBEProlonged Late Permian-Early Triassic hyperthermal: failure of climate regulation?Theoretical diversity of the marine biosphereBiodiversification of Early to Middle Ordovician conodonts: a case study from the Zitai Formation of Anhui Province, eastern ChinaLate Ordovician conodont biozonation of Australia—current status and regional biostratigraphic correlationsGraptoloid evolutionary rates track Ordovician–Silurian global climate change
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P2860
Did cooling oceans trigger Ordovician biodiversification? Evidence from conodont thermometry
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2008 nî lūn-bûn
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2008 թուականի Յուլիսին հրատարակուած գիտական յօդուած
@hyw
2008 թվականի հուլիսին հրատարակված գիտական հոդված
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2008年の論文
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2008年論文
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2008年論文
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2008年論文
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2008年論文
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2008年論文
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2008年论文
@wuu
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Did cooling oceans trigger Ord ...... ence from conodont thermometry
@ast
Did cooling oceans trigger Ord ...... ence from conodont thermometry
@en
Did cooling oceans trigger Ord ...... ence from conodont thermometry
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type
label
Did cooling oceans trigger Ord ...... ence from conodont thermometry
@ast
Did cooling oceans trigger Ord ...... ence from conodont thermometry
@en
Did cooling oceans trigger Ord ...... ence from conodont thermometry
@nl
prefLabel
Did cooling oceans trigger Ord ...... ence from conodont thermometry
@ast
Did cooling oceans trigger Ord ...... ence from conodont thermometry
@en
Did cooling oceans trigger Ord ...... ence from conodont thermometry
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Did cooling oceans trigger Ord ...... ence from conodont thermometry
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Christopher R Barnes
Robert S Nicoll
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10.1126/SCIENCE.1155814
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2008-07-25T00:00:00Z