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Open AccessJournal ArticleDOI

On the glacial-interglacial variability of the Asian monsoon in speleothem δ18O records.

TLDR
It is found that the records close to the monsoon moisture source show large glacial-interglacial variability, which then decreases landward, the moisture transport pathway effect, which counteracts the forcing of glacial boundary conditions.
Abstract
While Asian monsoon (AM) changes have been clearly captured in Chinese speleothem oxygen isotope (δ18O) records, the lack of glacial-interglacial variability in the records remains puzzling. Here, we report speleothem δ18O records from three locations along the trajectory of the Indian summer monsoon (ISM), a major branch of the AM, and characterize AM rainfall over the past 180,000 years. We have found that the records close to the monsoon moisture source show large glacial-interglacial variability, which then decreases landward. These changes likely reflect a stronger oxygen isotope fractionation associated with progressive rainout of AM moisture during glacial periods, possibly due to a larger temperature gradient and suppressed plant transpiration. We term this effect, which counteracts the forcing of glacial boundary conditions, the moisture transport pathway effect.

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Low oxygen isotope values of fossil cellulose indicate an intense monsoon in East Asia during the late Oligocene

TL;DR: In this article, the authors quantify monsoon strength based on new oxygen isotope measurements on cellulose (δ18Ocell) extracted from modern and fossil wood from southern China.
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Late Pleistocene human paleoecology in the highland savanna ecosystem of mainland Southeast Asia.

TL;DR: In this paper, stable carbon and oxygen isotope results suggest long-term opportunistic behavior among hunter-gatherers in foraging on a variety of food items in a mosaic environment and/or inhabiting an open forest edge during the terminal Pleistocene.
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Spatio-temporal expressions of precessional-scale stalagmite δ18O variations from the Asian monsoon area

TL;DR: In this article , changes in orbital-scale stalagmite δ18O (δ18Os) recorded from two caves in southern China reveal a clear precessional cycle during Marine Isotope Stage (MIS) 5 and from MIS 9.3 to MIS 8.3, respectively.
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Determining key upstream convection and rainout zones affecting δ18O in water vapor and precipitation based on 10-year continuous observations in the East Asian Monsoon region

TL;DR: Using a 10-year continuous high-resolution stalagmite δ18Ov and precipitation data at Nanjing (southeast China), the longest record of this kind, this article developed an improved time-lagged correlation method for key upstream convection Zones Identification (KUCZI).
Journal ArticleDOI

Orbital-scale hydroclimate variations in the southern Tibetan Plateau over the past 414,000 years

TL;DR: In this article , the Tianmen δ18O records from Tianmen cave, in the south-central Tibetan Plateau (TP), together with previous records from the same cave, were used to reconstruct a composite Tianmen record spanning over the past 414,000 years.
References
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Journal ArticleDOI

The NCEP/NCAR 40-Year Reanalysis Project

TL;DR: The NCEP/NCAR 40-yr reanalysis uses a frozen state-of-the-art global data assimilation system and a database as complete as possible, except that the horizontal resolution is T62 (about 210 km) as discussed by the authors.
Journal ArticleDOI

A Pliocene-Pleistocene stack of 57 globally distributed benthic δ18O records

TL;DR: In this paper, a 53-Myr stack (LR04) of benthic δ18O records from 57 globally distributed sites aligned by an automated graphic correlation algorithm is presented.

Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica

TL;DR: The recent completion of drilling at Vostok station in East Antarctica has allowed the extension of the ice record of atmospheric composition and climate to the past four glacial-interglacial cycles.
Journal ArticleDOI

Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica

TL;DR: The recent completion of drilling at Vostok station in East Antarctica has allowed the extension of the ice record of atmospheric composition and climate to the past four glacial-interglacial cycles as discussed by the authors.
Journal ArticleDOI

A High-Resolution Absolute-Dated Late Pleistocene Monsoon Record from Hulu Cave, China

TL;DR: The record links North Atlantic climate with the meridional transport of heat and moisture from the warmest part of the ocean where the summer East Asian Monsoon originates and generally agrees with the timing of temperature changes from the Greenland Ice Sheet Project Two (GISP2).
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