Open-system coral ages reveal persistent suborbital sea-level cycles.
about
Climate change and trace gasesSea-level oscillations during the last interglacial highstand recorded by Bahamas coralsRapid coupling between ice volume and polar temperature over the past 150,000 years.Evidence for obliquity forcing of glacial Termination II.Sr-Nd-Pb isotope evidence for ice-sheet presence on southern Greenland during the Last Interglacial.Deep-sea corals feel the flow.Mid-Pliocene sea level and continental ice volume based on coupled benthic Mg/Ca palaeotemperatures and oxygen isotopes.Interglacials of the last 800,000 yearsClimate sensitivity in the AnthropoceneA global picture of the first abrupt climatic event occurring during the last glacial inceptionCentennial-scale evolution of Dansgaard-Oeschger events in the northeast Atlantic Ocean between 39.5 and 56.5 ka B.PPromotion of glacial ice sheet buildup 60-115 kyr B.P. by precessionally paced Northern Hemispheric meltwater pulsesPhasing and amplitude of sea-level and climate change during the penultimate interglacialSea-level records challenged
P2860
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P2860
Open-system coral ages reveal persistent suborbital sea-level cycles.
description
2005 nî lūn-bûn
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2005年の論文
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2005年学术文章
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2005年学术文章
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2005年学术文章
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2005年学术文章
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2005年学术文章
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2005年学术文章
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2005年學術文章
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name
Open-system coral ages reveal persistent suborbital sea-level cycles.
@en
Open-system coral ages reveal persistent suborbital sea-level cycles.
@nl
type
label
Open-system coral ages reveal persistent suborbital sea-level cycles.
@en
Open-system coral ages reveal persistent suborbital sea-level cycles.
@nl
prefLabel
Open-system coral ages reveal persistent suborbital sea-level cycles.
@en
Open-system coral ages reveal persistent suborbital sea-level cycles.
@nl
P356
P1433
P1476
Open-system coral ages reveal persistent suborbital sea-level cycles.
@en
P2093
Steven L Goldstein
William G Thompson
P304
P356
10.1126/SCIENCE.1104035
P407
P577
2005-04-01T00:00:00Z