Journal ArticleDOI
Deglacial warming of the northeastern Atlantic ocean: correlation with the paleoclimatic evolution of the european continent
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TLDR
Isotopic, micropaleontologic and pollen analyses of deep-sea cores from the Bay of Biscay and the northeastern Atlantic Ocean show that the deglacial warming of this oceanic area was closely correlated with the paleoclimatic evolution of the adjacent European continent.About:
This article is published in Palaeogeography, Palaeoclimatology, Palaeoecology.The article was published on 1981-01-01. It has received 380 citations till now. The article focuses on the topics: Younger Dryas & Allerød oscillation.read more
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A 17,000-year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation
TL;DR: In this paper, a global oxygen isotope record for ocean water has been calculated from the Barbados sea level curve, allowing separation of the ice volume component common to all isotope records measured in deep-sea cores.
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Sea-land oxygen isotopic relationships from planktonic foraminifera and speleothems in the Eastern Mediterranean region and their implication for paleorainfall during interglacial intervals
Miryam Bar-Matthews,Avner Ayalon,Mabs Gilmour,Alan Matthews,Chris J. Hawkesworth,Chris J. Hawkesworth +5 more
TL;DR: In this article, a new, accurately dated 250-kyr δ18O and δ13C record determined from speleothems of the Peqiin Cave, Northern Israel is presented.
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The North Atlantic Ocean during the last deglaciation
TL;DR: The last deglacial warming of the high-latitude North Atlantic Ocean (40°65°) occurred in three discrete steps: in the southeast and central regions at 13 000 B.P., in the central and northern sectors at 10 000 B., and in the western (Labrador Sea) sector between 9000 and 6500 B., with a major influx of products of glacial wastage (meltwater and icebergs) as mentioned in this paper.
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Seasonal temperatures in Britain during the past 22,000 years, reconstructed using beetle remains
TL;DR: In this article, seasonal and mean annual temperatures were reconstructed from radiocarbon-dated beetle remains to yield a synthesis of the palaeoclimatic history of Britain over the last 22,000 years.
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Late Quaternary Paleoclimate in the Eastern Mediterranean Region from Stable Isotope Analysis of Speleothems at Soreq Cave, Israel
TL;DR: In this article, the eastern Mediterranean continental paleoclimate during the past 25,000 years was determined by a high-resolution petrographic, stable isotopic, and age study of speleothems from Soreq Cave, Israel.
References
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Journal ArticleDOI
Oxygen isotope and palaeomagnetic stratigraphy of Equatorial Pacific core V28-238: Oxygen isotope temperatures and ice volumes on a 105 year and 106 year scale☆
TL;DR: The core Vema 28-238 as discussed by the authors preserves an excellent oxygen isotope and magnetic stratigraphy and is shown to contain undisturbed sediments deposited continuously through the past 870,000 yr.
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Quaternary stratigraphy of Norden, a proposal for terminology and classification
TL;DR: In this paper, a proposal for a common chronostratigraphical classification of the Quaternary in Norden (and partly continental NW Europe) is made, based on the sequence of glacials/interglacials.
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Modeling the Climatic Response to Orbital Variations
John Imbrie,John Z. Imbrie +1 more
TL;DR: This article summarizes how the theory has evolved since the pioneer studies of James Croll and Milutin Milankovitch, reviews recent evidence that supports the theory, and argues that a major opportunity is at hand to investigate the physical mechanisms by which the climate system responds to orbital forcing.
Attainment of isotopic equilibrium between ocean water and the benthonic foraminifera genus Uvigerina: isotopic changes in the ocean during the last glacial
TL;DR: In this article, it was shown that even when the oxygen isotopic composition of foraminiferal tests is examined using non-standard analytical methods, the measurements may be expressed in terms of the PDB standard and that Uvigerina deposits its test at or near isotopic equilibrium in the temperature range 0.8 °G to 7 °C.
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Insolation changes, ice volumes, and the O18 record in deep‐sea cores
Wallace S. Broecker,Jan van Donk +1 more
TL;DR: In this article, a detailed curve of ice volume versus time is needed in order to test the validity of the hypothesis that changes in the earth's orbital parameters are the cause of oscillations in Pleistocene climate.