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Continental erosion and the Cenozoic rise of marine diatoms

Continental erosion and the Cenozoic rise of marine diatoms

http://www.wikidata.org/entity/Q28649816

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A bottom-up perspective on ecosystem change in Mesozoic oceans Ice sheets as a missing source of silica to the polar oceans.The evolution of diatoms and their biogeochemical functions.Approaches to Macroevolution: 2. Sorting of Variation, Some Overarching Issues, and General Conclusions.Detecting environment-dependent diversi_cation from phylogenies: a simulation study and some empirical illustrations.Accelerated diversification is related to life history and locomotion in a hyperdiverse lineage of microbial eukaryotes (Diatoms, Bacillariophyta).Silica cycling over geologic time The silicon cycle impacted by past ice sheets

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P2860

Continental erosion and the Cenozoic rise of marine diatoms

http://www.wikidata.org/entity/Q28649816

description

2015 nî lūn-bûn

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2015 թուականի Ապրիլին հրատարակուած գիտական յօդուած

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2015 թվականի ապրիլին հրատարակված գիտական հոդված

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2015年の論文

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2015年論文

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2015年論文

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2015年論文

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2015年論文

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2015年論文

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2015年论文

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Continental erosion and the Cenozoic rise of marine diatoms

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Continental erosion and the Cenozoic rise of marine diatoms

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Continental erosion and the Cenozoic rise of marine diatoms

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Continental erosion and the Cenozoic rise of marine diatoms

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Continental erosion and the Cenozoic rise of marine diatoms

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Continental erosion and the Cenozoic rise of marine diatoms

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Continental erosion and the Cenozoic rise of marine diatoms

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PNAS.1412883112

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Proceedings of the National Academy of Sciences of the United States of America

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Continental erosion and the Cenozoic rise of marine diatoms

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P2093

Morgan F Schaller

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Oscar E Romero

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Paul G Falkowski

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Sergio M Vallina

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P2860

Cenozoic planktonic marine diatom diversity and correlation to climate change

Radiolarians decreased silicification as an evolutionary response to reduced Cenozoic ocean silica availability

Equatorial convergence of India and early Cenozoic climate trends

The evolution of modern eukaryotic phytoplankton

High-latitude controls of thermocline nutrients and low latitude biological productivity.

Diversity dynamics of marine planktonic diatoms across the Cenozoic.

Lithium isotope history of Cenozoic seawater: changes in silicate weathering and reverse weathering.

Impact of Antarctic Circumpolar Current development on late Paleogene ocean structure.

The long-term carbon cycle, fossil fuels and atmospheric composition.

Mix and match: how climate selects phytoplankton.

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4239-4244

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scholarly article

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3200677

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10.1073/PNAS.1412883112

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112

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