Nannoplankton extinction and origination across the Paleocene-Eocene Thermal Maximum.
about
Increasing costs due to ocean acidification drives phytoplankton to be more heavily calcified: optimal growth strategy of coccolithophoresA long-term association between global temperature and biodiversity, origination and extinction in the fossil recordThe geological record of ocean acidificationPhytoplankton calcification in a high-CO₂ worldConsequences of elevated temperature and pCO2 on insect folivory at the ecosystem level: perspectives from the fossil recordSurviving rapid climate change in the deep sea during the Paleogene hyperthermalsPhylogenetic analysis of Thecosomata Blainville, 1824 (holoplanktonic opisthobranchia) using morphological and molecular dataBiodiversity tracks temperature over timeMarine planktonic microbes survived climatic instabilities in the pastThe future of the oceans pastThe rise and fall of species: implications for macroevolutionary and macroecological studiesRapid emergence of climate change in environmental drivers of marine ecosystems.Ocean fertilization: a potential means of geoengineering?Time-calibrated molecular phylogeny of pteropodsSensitivity of coccolithophores to carbonate chemistry and ocean acidification.Predominance of heavily calcified coccolithophores at low CaCO3 saturation during winter in the Bay of Biscay.A probabilistic assessment of the rapidity of PETM onset.Long-term legacy of massive carbon input to the Earth system: Anthropocene versus Eocene.Anthropogenic modification of the oceans.Gas hydrates: past and future geohazard?Calcareous nannoplankton response to surface-water acidification around Oceanic Anoxic Event 1a.Mass extinction in tetraodontiform fishes linked to the Palaeocene-Eocene thermal maximum.On the duration of the Paleocene-Eocene thermal maximum (PETM)Warm plankton soup and red herrings: calcareous nannoplankton cellular communities and the Palaeocene-Eocene Thermal MaximumAssessing the Past and Future Stability of Global Gas Hydrate ReservoirsAnalyzing abrupt and nonlinear climate changes and their impactsMajor shifts in calcareous phytoplankton assemblages through the Eocene-Oligocene transition of Tanzania and their implications for low-latitude primary productionRapid and sustained surface ocean acidification during the Paleocene-Eocene Thermal MaximumIntegrated stratigraphy of the Paleocene-Eocene thermal maximum in the New Jersey Coastal Plain: Toward understanding the effects of global warming in a shelf environment
P2860
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P2860
Nannoplankton extinction and origination across the Paleocene-Eocene Thermal Maximum.
description
2006 nî lūn-bûn
@nan
2006 թուականի Դեկտեմբերին հրատարակուած գիտական յօդուած
@hyw
2006 թվականի դեկտեմբերին հրատարակված գիտական հոդված
@hy
2006年の論文
@ja
2006年論文
@yue
2006年論文
@zh-hant
2006年論文
@zh-hk
2006年論文
@zh-mo
2006年論文
@zh-tw
2006年论文
@wuu
name
Nannoplankton extinction and origination across the Paleocene-Eocene Thermal Maximum.
@ast
Nannoplankton extinction and origination across the Paleocene-Eocene Thermal Maximum.
@en
type
label
Nannoplankton extinction and origination across the Paleocene-Eocene Thermal Maximum.
@ast
Nannoplankton extinction and origination across the Paleocene-Eocene Thermal Maximum.
@en
prefLabel
Nannoplankton extinction and origination across the Paleocene-Eocene Thermal Maximum.
@ast
Nannoplankton extinction and origination across the Paleocene-Eocene Thermal Maximum.
@en
P2093
P356
P1433
P1476
Nannoplankton extinction and origination across the Paleocene-Eocene Thermal Maximum.
@en
P2093
Jocelyn A Sessa
Paul A Wilson
Samantha J Gibbs
Timothy J Bralower
P304
P356
10.1126/SCIENCE.1133902
P407
P50
P577
2006-12-01T00:00:00Z