Late Pliocene Greenland glaciation controlled by a decline in atmospheric CO2 levels.
about
Molecular phylogeny and biogeography of Petaurista inferred from the cytochrome b gene, with implications for the taxonomic status of P. caniceps, P. marica and P. sybillaEvolution of a Planktonic Foraminifer during Environmental Changes in the Tropical OceansMolecular Phylogeny of Grassland Caterpillars (Lepidoptera: Lymantriinae: Gynaephora) Endemic to the Qinghai-Tibetan PlateauA new positive relationship between pCO2 and stomatal frequency in Quercus guyavifolia (Fagaceae): a potential proxy for palaeo-CO2 levelsPacific freshening drives Pliocene cooling and Asian monsoon intensificationWarm climates of the past--a lesson for the future?Antarctic and Southern Ocean influences on Late Pliocene global coolingPatterns and mechanisms of early Pliocene warmth.Exposure age and ice-sheet model constraints on Pliocene East Antarctic ice sheet dynamics.On the identification of a Pliocene time slice for data-model comparison.Reconstructing atmospheric CO2 during the Plio-Pleistocene transition by fossil Typha.Modelled ocean changes at the Plio-Pleistocene transition driven by Antarctic ice advanceAre there pre-Quaternary geological analogues for a future greenhouse warming?Only 5 southern Greenland shelf edge glaciations since the early PlioceneCoupling of CO2 and ice sheet stability over major climate transitions of the last 20 million years.Northern hemisphere glaciation during the globally warm early Late Pliocene.A persistent and dynamic East Greenland Ice Sheet over the past 7.5 million years.Plio-Pleistocene climate sensitivity evaluated using high-resolution CO2 records.Introduction. Pliocene climate, processes and problems.Late Miocene decoupling of oceanic warmth and atmospheric carbon dioxide forcing.A 40-million-year history of atmospheric CO2Greenhouse gases in the Earth system: a palaeoclimate perspective.Evidence for ephemeral middle Eocene to early Oligocene Greenland glacial ice and pan-Arctic sea ice.Paleoceanographic changes in the Eastern Equatorial Pacific over the last 10 MyrDeep-sea temperature and ice volume changes across the Pliocene-Pleistocene climate transitions.Climates of the Earth and Cryosphere EvolutionChallenges in quantifying Pliocene terrestrial warming revealed by data–model discordRegional and global climate for the mid-Pliocene using the University of Toronto version of CCSM4 and PlioMIP2 boundary conditionsThe role of vegetation feedbacks on Greenland glaciationThe last glacial cycle: transient simulations with an AOGCMEarth’s Climate SystemAtmospheric CO2decline during the Pliocene intensification of Northern Hemisphere glaciationsPhylogenetic analysis of the north-east Atlantic and Mediterranean species of the genus Stenosoma (Isopoda, Valvifera, Idoteidae)Dynamic Greenland ice sheet driven by pCO variations across the Pliocene Pleistocene transition
P2860
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P2860
Late Pliocene Greenland glaciation controlled by a decline in atmospheric CO2 levels.
description
2008 nî lūn-bûn
@nan
2008 թուականի Օգոստոսին հրատարակուած գիտական յօդուած
@hyw
2008 թվականի օգոստոսին հրատարակված գիտական հոդված
@hy
2008年の論文
@ja
2008年論文
@yue
2008年論文
@zh-hant
2008年論文
@zh-hk
2008年論文
@zh-mo
2008年論文
@zh-tw
2008年论文
@wuu
name
Late Pliocene Greenland glaciation controlled by a decline in atmospheric CO2 levels.
@ast
Late Pliocene Greenland glaciation controlled by a decline in atmospheric CO2 levels.
@en
Late Pliocene Greenland glaciation controlled by a decline in atmospheric CO2 levels.
@nl
type
label
Late Pliocene Greenland glaciation controlled by a decline in atmospheric CO2 levels.
@ast
Late Pliocene Greenland glaciation controlled by a decline in atmospheric CO2 levels.
@en
Late Pliocene Greenland glaciation controlled by a decline in atmospheric CO2 levels.
@nl
prefLabel
Late Pliocene Greenland glaciation controlled by a decline in atmospheric CO2 levels.
@ast
Late Pliocene Greenland glaciation controlled by a decline in atmospheric CO2 levels.
@en
Late Pliocene Greenland glaciation controlled by a decline in atmospheric CO2 levels.
@nl
P50
P356
P1433
P1476
Late Pliocene Greenland glaciation controlled by a decline in atmospheric CO2 levels.
@en
P2093
Emma J Stone
P2888
P304
P356
10.1038/NATURE07223
P407
P577
2008-08-01T00:00:00Z
P5875
P6179
1043098872