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Palaeoclimatic changes in the Qinghai Lake area during the last 18,000 years

TLDR
In this article, multi-proxy analysis of a sediment core from Qinghai Lake, including pollen, carbonate, TOC, TN and δ 13 C of organic matter, was used to document regional climatic changes during the last 18,000 years.
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This article is published in Quaternary International.The article was published on 2005-07-01. It has received 640 citations till now. The article focuses on the topics: Younger Dryas & Glacial period.

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Citations
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East Asian summer monsoon precipitation variability since the last deglaciation

TL;DR: A well-dated, pollen-based, ~20-yr-resolution quantitative precipitation reconstruction from an alpine lake in North China, which provides for the first time a direct record of EASM evolution since 14.7 ka, points to strong internal feedback processes driving the EASm, and may aid the understanding of future monsoon behaviour under ongoing anthropogenic climate change.
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Asian monsoon oscillations in the northeastern Qinghai–Tibet Plateau since the late glacial as interpreted from visible reflectance of Qinghai Lake sediments

TL;DR: This article used reflectance spectroscopy to characterize the sediments in a 795-cm long core taken from the southeastern part of the lake and found that redness increases at times of increased precipitation, that is, as monsoon strength increases.
References
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Journal ArticleDOI

A Pervasive Millennial-Scale Cycle in North Atlantic Holocene and Glacial Climates

TL;DR: In this paper, the North Atlantic deep sea cores reveal that abrupt shifts punctuated what is conventionally thought to have been a relatively stable Holocene climate, and they make up a series of climate shifts with a cyclicity close to 1470 ± 500 years, which is the most recent manifestation of a pervasive millennial-scale climate cycle operating independently of the glacial-interglacial climate state.
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Comparison of oxygen isotope records from the GISP2 and GRIP Greenland ice cores

TL;DR: In this article, the authors present the complete oxygen isotope record for the Greenland Ice Sheet Project 2 (GISP2) core, drilled 28 km west of the GRIP core, and observe large, rapid climate fluctuations throughout the last glacial period.
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Holocene climatic instability: A prominent, widespread event 8200 yr ago

TL;DR: The most prominent Holocene climatic event in Greenland ice-core proxies, with approximately half the amplitude of the Younger Dryas, occurred ∼8000 to 8400 yr ago.
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Evidence for massive discharges of icebergs into the North Atlantic ocean during the last glacial period

TL;DR: In this article, the authors present evidence that the most recent six Heinrich layers, deposited between 14,000 and 70,000 years ago, record marked decreases in sea surface temperature and salinity, decreases in the flux of planktonic foraminifera to the sediments, and short-lived, massive discharges of icebergs originating in eastern Canada.
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Applications of organic geochemistry to paleolimnological reconstructions: a summary of examples from the Laurentian Great Lakes

TL;DR: The organic matter content of lake sediments contains information that helps to reconstruct past environmental conditions, evaluate histories of climate change, and assess impacts of humans on local ecosystems as discussed by the authors, and serve as proxies of organic matter delivery and accumulation.
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