Evidence for obliquity forcing of glacial Termination II.

scientific article

Evidence for obliquity forcing of glacial Termination II. is …
instance of (P31):
scholarly articleQ13442814

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P356DOI10.1126/SCIENCE.1170371
P698PubMed publication ID19679773

P50authorJohn HellstromQ37614190
Russell DrysdaleQ43144962
Maria Fernanda Sanchez GoñiQ50229970
Anthony FallickQ56419470
Gerrit LohmannQ56447989
Giovanni ZanchettaQ56546108
Ilaria IsolaQ57880572
Isabelle CouchoudQ98611461
P2093author name stringR Maas
J McDonald
P2860cites workCollapse of the California Current during glacial maxima linked to climate change on landQ30655672
Southern Ocean origin for the resumption of Atlantic thermohaline circulation during deglaciationQ30815410
Orbital and millennial-scale features of atmospheric CH4 over the past 800,000 yearsQ31155450
Penultimate deglacial sea-level timing from uranium/thorium dating of Tahitian coralsQ33434279
Evidence from U-Th dating against Northern Hemisphere forcing of the penultimate deglaciationQ33893250
Obliquity pacing of the late Pleistocene glacial terminationsQ34406442
Orbital and millennial Antarctic climate variability over the past 800,000 years.Q34646794
Unlocking the mysteries of the ice agesQ34737473
Direct determination of the timing of sea level change during termination II.Q45354467
Rapid fluctuations in sea level recorded at huon peninsula during the penultimate deglaciationQ46915070
Open-system coral ages reveal persistent suborbital sea-level cyclesQ47280490
Early Pleistocene glacial cycles and the integrated summer insolation forcingQ47295519
Sea-level fluctuations during the last glacial cycleQ47313108
Continuous 500,000-year climate record from vein calcite in devils hole, nevadaQ47342271
Stalagmite evidence for the precise timing of North Atlantic cold events during the early last glacialQ57556511
Palaeoclimatic implications of the growth history and stable isotope (δ18O and δ13C) geochemistry of a Middle to Late Pleistocene stalagmite from central-western ItalyQ57556529
Increasing vegetation and climate gradient in Western Europe over the Last Glacial Inception (122–110 ka): data-model comparisonQ57564728
High resolution palynological record off the Iberian margin: direct land-sea correlation for the Last Interglacial complexQ57564763
Abrupt Temperature Changes in the Western Mediterranean over the Past 250,000 YearsQ57865988
Dansgaard-Oeschger and Heinrich event imprints in Alboran Sea paleotemperaturesQ57866063
Sea-level reversal during Termination IIQ58394113
P433issue5947
P407language of work or nameEnglishQ1860
P304page(s)1527-1531
P577publication date2009-08-13
P1433published inScienceQ192864
P1476titleEvidence for obliquity forcing of glacial Termination II
P478volume325

Reverse relations

cites work (P2860)
Q64081966800-kyr land temperature variations modulated by vegetation changes on Chinese Loess Plateau
Q57556396A continuous stable isotope record from the penultimate glacial maximum to the Last Interglacial (159–121 ka) from Tana Che Urla Cave (Apuan Alps, central Italy)
Q21093487An optimized multi-proxy, multi-site Antarctic ice and gas orbital chronology (AICC2012): 120–800 ka
Q21128943An optimized multi-proxy, multi-site Antarctic ice and gas orbital chronology (AICC2012): 120–800 ka
Q38432102Anthropology. Absolute dating of cave art.
Q58080595Atmospheric bridge on orbital time scales
Q40848897Bipolar seesaw control on last interglacial sea level.
Q57318100Enhanced climate instability in the North Atlantic and southern Europe during the Last Interglacial
Q49923497Evidence of thermophilisation and elevation-dependent warming during the Last Interglacial in the Italian Alps.
Q57556392Hydrological variability over the Apennines during the Early Last Glacial precession minimum, as revealed by a stable isotope record from Sulmona basin, Central Italy
Q55919190Interglacials of the last 800,000 years
Q57556406Lateglacial to Holocene trace element record (Ba, Mg, Sr) from Corchia Cave (Apuan Alps, central Italy): paleoenvironmental implications
Q39543400Luminescence dating of glaciofluvial deposits linked to the penultimate glaciation in the Eastern Alps
Q100464078Magnesium in subaqueous speleothems as a potential palaeotemperature proxy
Q64168145Milankovitch-paced Termination II in a Nevada speleothem?
Q99350148Millennial climate oscillations controlled the structure and evolution of Termination II
Q35153396North Atlantic storm track changes during the Last Glacial Maximum recorded by Alpine speleothems
Q58479290Pulses of carbon dioxide emissions from intracrustal faults following climatic warming
Q31035898Reconciliation of the Devils Hole climate record with orbital forcing
Q58080567Simulating climate and stable water isotopes during the Last Interglacial using a coupled climate-isotope model
Q97424148Speleothem record attests to stable environmental conditions during Neanderthal-modern human turnover in southern Italy
Q105875655Stable isotopes in caves over altitudinal gradients: fractionation behaviour and inferences for speleothem sensitivity to climate change
Q29027410Tidal obliquity evolution of potentially habitable planets

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