Erratum to “Holocene climate optimum and last glacial maximum in the Mediterranean: the marine oxygen isotope record” [Marine Geology 153 (1999) 57–75]

1999 ◽  
Vol 161 (2-4) ◽  
pp. 385-387 ◽  
Author(s):  
Eelco J Rohling ◽  
S De Rijk
Keyword(s):  
Oxygen Isotope ◽  
Last Glacial Maximum ◽  
Glacial Maximum ◽  
Marine Geology ◽  
Holocene Climate ◽  
Last Glacial ◽  
Oxygen Isotope Record ◽  
Isotope Record ◽  
The Mediterranean

Controlling factors on a paleo-lake oxygen isotope record (Yammoûneh, Lebanon) since the Last Glacial Maximum

2010 ◽  
Vol 29 (7-8) ◽  
pp. 865-886 ◽  
Author(s):  
Anne-Lise Develle ◽  
Julien Herreros ◽  
Laurence Vidal ◽  
Alexandre Sursock ◽  
Françoise Gasse
Keyword(s):  
Oxygen Isotope ◽  
Last Glacial Maximum ◽  
Controlling Factors ◽  
Glacial Maximum ◽  
Last Glacial ◽  
Oxygen Isotope Record ◽  
Isotope Record ◽  
The Last Glacial Maximum ◽  
The Last Glacial

scholarly journals 14C Ages of a Varved Last Glacial Maximum Section Off Pakistan

Radiocarbon ◽  
2003 ◽  
Vol 45 (3) ◽  
pp. 467-477 ◽  
Author(s):  
Ulrich von Rad ◽  
Michael Sarnthein ◽  
Pieter M Grootes ◽  
Heidi Doose-Rolinski ◽  
Jochen Erbacher
Keyword(s):  
Mass Spectrometry ◽  
Oxygen Isotope ◽  
Last Glacial Maximum ◽  
Accelerator Mass Spectrometry ◽  
Ice Core ◽  
Glacial Maximum ◽  
Last Glacial ◽  
Oxygen Isotope Record ◽  
Isotope Record

In a core off Pakistan, we obtained 38 14C analyses by accelerator mass spectrometry (AMS) from a 4.4-m-thick, expanded, annually-laminated Last Glacial Maximum (LGM) section, bracketed by bioturbated intervals ascribed to the Heinrich-1 (H1) and Heinrich-2 (H2) equivalent events (52 14C analyses between 24–15 kyr BP). A floating varve age scale, anchored to the oxygen isotope record of the layer-counted GISP2 ice core at the H2/LGM boundary, results in an annually dated record for the LGM from 23,450–17,900 cal BP. The floating varve scale of the LGM provides us with a tentative calibration of local marine AMS 14C age dates to calendar years.

A 5000-year lacustrine sediment oxygen isotope record of late Holocene climate change in Newfoundland, Canada

2022 ◽  
Vol 278 ◽  
pp. 107376
Author(s):  
Matthew S. Finkenbinder ◽  
Byron A. Steinman ◽  
Broxton W. Bird ◽  
Ellen C. Heilman ◽  
Alexandria R. Aspey ◽  
...  
Keyword(s):  
Climate Change ◽  
Oxygen Isotope ◽  
Late Holocene ◽  
Lacustrine Sediment ◽  
Holocene Climate ◽  
Holocene Climate Change ◽  
Oxygen Isotope Record ◽  
Isotope Record

scholarly journals Global Speleothem Oxygen Isotope Measurements Since the Last Glacial Maximum

2013 ◽  
Vol 2013 ◽  
pp. 1-9 ◽  
Author(s):  
A. M. Shah ◽  
C. Morrill ◽  
E. P. Gille ◽  
W. S. Gross ◽  
D. M. Anderson ◽  
...  
Keyword(s):  
Oxygen Isotope ◽  
Last Glacial Maximum ◽  
Large Scale ◽  
Asian Summer Monsoon ◽  
Glacial Maximum ◽  
Last Glacial ◽  
Hydrologic Variability ◽  
The World ◽  
The Last Glacial Maximum ◽  
The Last Glacial

This synthesis of thirty-six sites (sixty cores with over 27 000 measurements) located around the world facilitates scientific research on the climate of the last 21 000 years ago obtained from oxygen isotope ( or delta-O-18) measurements. Oxygen isotopes in speleothem calcite record the influence of ambient temperature and the isotopic composition of the source water, the latter providing evidence of hydrologic variability and change. Compared to paleoclimate proxies from sedimentary archives, the age uncertainty is unusually small, around +/−100 years for the last 21 000-year interval. Using data contributed to the World Data Center (WDC) for Paleoclimatology, we have created consistently formatted data files for individual sites as well as composite dataset of annual to millennial resolution. These individual files also contain the chronology information about the sites. The data are useful in understanding hydrologic variability at local and regional scales, such as the Asian summer monsoon and the Intertropical Convergence Zone (as discussed in the underlying source publications), and should also be useful in understanding large-scale aspects of hydrologic change since the Last Glacial Maximum (LGM).

Oxygen isotope stage 3 fluvial and eolian successions in Europe compared with climate model results

2003 ◽  
Vol 59 (2) ◽  
pp. 223-233 ◽  
Author(s):  
K.o van Huissteden ◽  
David Pollard
Keyword(s):  
Oxygen Isotope ◽  
Last Glacial Maximum ◽  
Climate Model ◽  
Regional Climate ◽  
Glacial Maximum ◽  
Oxygen Isotope Stage ◽  
Last Glacial ◽  
Wind Speeds ◽  
Fluvial Response ◽  
Eolian Deposits

AbstractFluvial and eolian successions of oxygen isotope stage 3 are compared with global (GCM) and regional climate (RCM) modeling experiments of the stage 3 and last glacial maximum climate in Europe. Differences in precipitation between stage-3 stades and interstades were minor, which is confirmed by the fluvial successions. The fluvial response to climate variation is non-uniform, and in southern Europe more pronounced than in northern Europe. The model simulations indicate a strong western winter circulation over Europe during stage 3, which is supported by the eolian deposits data. Wind speeds in the last glacial maximum simulation appear modest compared with those of stage 3, which contrasts with the abundance of eolian deposits. This suggests that during glacial climates the stabilizing effect of vegetation determines eolian sedimentation rates, rather than wind speed. Stage 3 can be divided into an older part (>45,000 cal yr B.P.) with a relatively stable landscape and moist climate and a younger part with more frequent climate change and decreasing landscape stability.

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