Late Miocene decoupling of oceanic warmth and atmospheric carbon dioxide forcing. - Wikidata - wikimedia - TriplyDB

Late Miocene decoupling of oceanic warmth and atmospheric carbon dioxide forcing.

Late Miocene decoupling of oceanic warmth and atmospheric carbon dioxide forcing.

http://www.wikidata.org/entity/Q46126235

about

Cenozoic planktonic marine diatom diversity and correlation to climate change Evidence for ice-free summers in the late Miocene central Arctic Ocean.Pliocene reversal of late Neogene aridification Evolution of a Planktonic Foraminifer during Environmental Changes in the Tropical Oceans Light intensity modulation by coccoliths of Emiliania huxleyi as a micro-photo-regulator Pliocene cooling enhanced by flow of low-salinity Bering Sea water to the Arctic Ocean Patterns and mechanisms of early Pliocene warmth.Model systems for a no-analog future: species associations and climates during the last deglaciation.Elevation-induced climate change as a dominant factor causing the late Miocene C(4) plant expansion in the Himalayan foreland.Quaternary coral reef refugia preserved fish diversity.Late Miocene episodic lakes in the arid Tarim Basin, western China Dominant 100,000-year precipitation cyclicity in a late Miocene lake from northeast Tibet.A 12-million-year temperature history of the tropical Pacific Ocean.Active Pacific meridional overturning circulation (PMOC) during the warm Pliocene.End-member modeling of the grain-size record of Sikouzi fine sediments in Ningxia (China) and implications for temperature control of Neogene evolution of East Asian winter monsoon.Late Miocene threshold response of marine algae to carbon dioxide limitation.Roles of dental development and adaptation in rodent evolution.Wetter subtropics in a warmer world: Contrasting past and future hydrological cycles.A 40-million-year history of atmospheric CO2 Biogeochemistry: Ancient algae crossed a threshold.Late Miocene climate cooling and intensification of southeast Asian winter monsoon.Effect of Vegetation on the Late Miocene Ocean Circulation Coccolithophore carbonate during the last 450 ka in the NW Pacific Ocean (ODP site 1209B, Shatsky Rise)

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Late Miocene decoupling of oceanic warmth and atmospheric carbon dioxide forcing.

http://www.wikidata.org/entity/Q46126235

description

2012 nî lūn-bûn

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2012年の論文

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2012年学术文章

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2012年学术文章

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2012年学术文章

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2012年学术文章

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2012年学术文章

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2012年学术文章

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2012年學術文章

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2012年學術文章

@zh-hant

name

Late Miocene decoupling of oceanic warmth and atmospheric carbon dioxide forcing.

@en

Late Miocene decoupling of oceanic warmth and atmospheric carbon dioxide forcing.

@nl

type

label

Late Miocene decoupling of oceanic warmth and atmospheric carbon dioxide forcing.

@en

Late Miocene decoupling of oceanic warmth and atmospheric carbon dioxide forcing.

@nl

prefLabel

Late Miocene decoupling of oceanic warmth and atmospheric carbon dioxide forcing.

@en

Late Miocene decoupling of oceanic warmth and atmospheric carbon dioxide forcing.

@nl

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Late Miocene decoupling of oceanic warmth and atmospheric carbon dioxide forcing.

@en

P2093

A Christina Ravelo

http://www.w3.org/2001/XMLSchema#string

Heather L Ford

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Jonathan P LaRiviere

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Michael W Wara

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Mitch Lyle

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Petra S Dekens

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P2860

Target Atmospheric CO2: Where Should Humanity Aim?

High Earth-system climate sensitivity determined from Pliocene carbon dioxide concentrations

Stable carbon cycle-climate relationship during the Late Pleistocene

Calibration of the alkenone paleotemperature index U37K′ based on core-tops from the eastern South Atlantic and the global ocean (60°N-60°S)

Trends, Rhythms, and Aberrations in Global Climate 65 Ma to Present

Climate. A paleoclimatic enigma?

Tropical ocean temperatures over the past 3.5 million years.

Tropical cyclones and permanent El Niño in the early Pliocene epoch.

Permanent El Niño-like conditions during the Pliocene warm period.

The Pliocene paradox (mechanisms for a permanent El Niño).

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97-100

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scholarly article

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10.1038/NATURE11200

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7401

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486

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Allison Crimmins

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2012-06-06T00:00:00Z

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1045147672

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22678287

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