Coherent High- and Low-Latitude Climate Variability During the Holocene Warm Period-Reference-Cited by-同舟云学术

Coherent High- and Low-Latitude Climate Variability During the Holocene Warm Period

Published:2000-06-23 Issue:5474 Volume:288 Page:2198-2202
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

deMenocal Peter¹,Ortiz Joseph¹,Guilderson Tom²,Sarnthein Michael³

Affiliation:

1. Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964, USA.

2. Center for Accelerator Mass Spectrometry, Lawrence-Livermore National Laboratory, Livermore, CA 94551, USA.

3. Institut für Geowissenschaften, Universität Kiel, Kiel, Germany.

Abstract

A faunal record of sea-surface temperature (SST) variations off West Africa documents a series of abrupt, millennial-scale cooling events, which punctuated the Holocene warm period. These events evidently resulted from increased southward advection of cooler temperate or subpolar waters to this subtropical location or from enhanced regional upwelling. The most recent of these events was the Little Ice Age, which occurred between 1300 to 1850 A.D., when subtropical SSTs were reduced by 3° to 4°C. These events were synchronous with Holocene changes in subpolar North Atlantic SSTs, documenting a strong, in-phase link between millennial-scale variations in high- and low-latitude climate during the Holocene.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference39 articles.

1. Evidence for general instability of past climate from a 250-kyr ice-core record

2. Correlations between climate records from North Atlantic sediments and Greenland ice

3. Massive iceberg discharges as triggers for global climate change

4. Holocene climatic instability: A prominent, widespread event 8200 yr ago

5. Holocene Climatic Variations—Their Pattern and Possible Cause

Cited by 577 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Evolution of ocean circulation and water masses in the Guaymas Basin (Gulf of California) during the last 31,000 years revealed by radiolarians and silicoflagellates in IODP expedition 385 sediment cores;Frontiers in Earth Science;2024-01-18

2. Monsoon-driven changes in aeolian and fluvial sediment input to the central Red Sea recorded throughout the last 200 000 years;Climate of the Past;2024-01-03

3. Synthesis and perspectives: drivers, rhythms, and spatial patterns of Holocene climate change;European Glacial Landscapes;2024

4. Introduction to the Holocene climate;European Glacial Landscapes;2024

5. A multicentennial mode of North Atlantic climate variability throughout the Last Glacial Maximum;Science Advances;2023-11-03