The magnitude and duration of Late Ordovician-Early Silurian glaciation.
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Graptolite community responses to global climate change and the Late Ordovician mass extinctionThe Astrobiology Primer v2.0Phylogenetic Clustering of Origination and Extinction across the Late Ordovician Mass ExtinctionIsotopic evidence for long term warmth in the MesozoicClimate change and the selective signature of the Late Ordovician mass extinctionGraptoloid diversity and disparity became decoupled during the Ordovician mass extinctionCladal Turnover: the end-Ordovician as a large-scale analogue of species turnoverContinental arc volcanism as the principal driver of icehouse-greenhouse variability.Microbes and mass extinctions: paleoenvironmental distribution of microbialites during times of biotic crisis.Phanerozoic Earth system evolution and marine biodiversity.A Cenozoic-style scenario for the end-Ordovician glaciation.Response of beta diversity to pulses of Ordovician-Silurian mass extinction.Stable isotope analysis of Dacryoconarid carbonate microfossils: a new tool for Devonian oxygen and carbon isotope stratigraphy.87Sr/86Sr evidence from the epeiric Martin Ridge Basin for enhanced carbonate weathering during the Hirnantian.Clumped isotope analysis of carbonates: comparison of two different acid digestion techniques.Biogeographic and bathymetric determinants of brachiopod extinction and survival during the Late Ordovician mass extinction.An early Cambrian greenhouse climate.Abrupt global-ocean anoxia during the Late Ordovician-early Silurian detected using uranium isotopes of marine carbonates.Oxygen isotope composition of the Phanerozoic ocean and a possible solution to the dolomite problemThe Hirnantian (Late Ordovician) and end-Guadalupian (Middle Permian) mass-extinction events comparedWithin- and among-genus components of size evolution during mass extinction, recovery, and background intervals: a case study of Late Permian through Late Triassic foraminiferaGraptoloid evolutionary rates track Ordovician–Silurian global climate changeBackground effects on Faraday collectors in gas-source mass spectrometry and implications for clumped isotope measurementsTerminal Ordovician stratigraphy of the Siljan district, Sweden
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P2860
The magnitude and duration of Late Ordovician-Early Silurian glaciation.
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2011 nî lūn-bûn
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2011 թուականի Յունուարին հրատարակուած գիտական յօդուած
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2011 թվականի հունվարին հրատարակված գիտական հոդված
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2011年の論文
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2011年論文
@yue
2011年論文
@zh-hant
2011年論文
@zh-hk
2011年論文
@zh-mo
2011年論文
@zh-tw
2011年论文
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name
The magnitude and duration of Late Ordovician-Early Silurian glaciation.
@ast
The magnitude and duration of Late Ordovician-Early Silurian glaciation.
@en
The magnitude and duration of Late Ordovician-Early Silurian glaciation.
@nl
type
label
The magnitude and duration of Late Ordovician-Early Silurian glaciation.
@ast
The magnitude and duration of Late Ordovician-Early Silurian glaciation.
@en
The magnitude and duration of Late Ordovician-Early Silurian glaciation.
@nl
prefLabel
The magnitude and duration of Late Ordovician-Early Silurian glaciation.
@ast
The magnitude and duration of Late Ordovician-Early Silurian glaciation.
@en
The magnitude and duration of Late Ordovician-Early Silurian glaciation.
@nl
P2093
P2860
P50
P356
P1433
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The magnitude and duration of Late Ordovician-Early Silurian glaciation.
@en
P2093
David S Jones
Nigel C Hughes
Seth Finnegan
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P304
P356
10.1126/SCIENCE.1200803
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P50
P577
2011-01-27T00:00:00Z