The paleoclimatic events and cause in the Okinawa Trough during 50 kaBP
Planktonic foraminiferal delta O-18 record for core DGKS9603 from the Okinawa Trough shows a series of climatic fluctuations and sudden cooling events in short time scale during 50 kaBP, which appear to correlate closely to the Younger Dryas and Heinrich events H1-5 recorded in Chinese loess, the So...
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ftchinacasciocas:oai:ir.qdio.ac.cn:337002/3816 2024-09-15T18:09:10+00:00 The paleoclimatic events and cause in the Okinawa Trough during 50 kaBP Liu, ZX Li, TG Li, PY Huang, QY Berne, S Saito, Y Cheng, ZB Wei, GJ Liu, LJ Li, Z 2001 http://ir.qdio.ac.cn/handle/337002/3817 英语 eng CHINESE SCIENCE BULLETIN Liu, ZX; Li, TG; Li, PY; Huang, QY; Berne, S; Saito, Y; Cheng, ZB; Wei, GJ; Liu, LJ; Li, Z.The paleoclimatic events and cause in the Okinawa Trough during 50 kaBP,CHINESE SCIENCE BULLETIN,2001,46(2):153-157 http://ir.qdio.ac.cn/handle/337002/3817 Okinawa Trough Sudden Paleoclimatic Change Events Polarity Reversal Events Late Quaternary Multidisciplinary Sciences Article 期刊论文 2001 ftchinacasciocas 2024-08-09T03:18:11Z Planktonic foraminiferal delta O-18 record for core DGKS9603 from the Okinawa Trough shows a series of climatic fluctuations and sudden cooling events in short time scale during 50 kaBP, which appear to correlate closely to the Younger Dryas and Heinrich events H1-5 recorded in Chinese loess, the South China Sea, the North Atlantic cores and the Greenland ice cores. Three polarity reversal events, correlating to Gothenburg, Mungo and Laschamp events, approximately correspond to Heinrich events H1, H3 and H5 respectively, which could be a cause of global climate changes. The delta O-18 curve of the Okinawa Trough is well associated with the grain size record of the Lijiayuan loess profile in northwestern China and is somewhat different from the climate fluctuations documented in the Greenland ice cores. These correlation results indicate that regional factors play an important role in controlling the climate changes in the East Asia, and the East Asian Monsoon could be the prominent regional controlling factor. Planktonic foraminiferal delta O-18 record for core DGKS9603 from the Okinawa Trough shows a series of climatic fluctuations and sudden cooling events in short time scale during 50 kaBP, which appear to correlate closely to the Younger Dryas and Heinrich events H1-5 recorded in Chinese loess, the South China Sea, the North Atlantic cores and the Greenland ice cores. Three polarity reversal events, correlating to Gothenburg, Mungo and Laschamp events, approximately correspond to Heinrich events H1, H3 and H5 respectively, which could be a cause of global climate changes. The delta O-18 curve of the Okinawa Trough is well associated with the grain size record of the Lijiayuan loess profile in northwestern China and is somewhat different from the climate fluctuations documented in the Greenland ice cores. These correlation results indicate that regional factors play an important role in controlling the climate changes in the East Asia, and the East Asian Monsoon could be the prominent regional controlling ... Article in Journal/Newspaper Greenland Greenland ice cores North Atlantic Institute of Oceanology, Chinese Academy of Sciences: IOCAS-IR |
institution |
Open Polar |
collection |
Institute of Oceanology, Chinese Academy of Sciences: IOCAS-IR |
op_collection_id |
ftchinacasciocas |
language |
English |
topic |
Okinawa Trough Sudden Paleoclimatic Change Events Polarity Reversal Events Late Quaternary Multidisciplinary Sciences |
spellingShingle |
Okinawa Trough Sudden Paleoclimatic Change Events Polarity Reversal Events Late Quaternary Multidisciplinary Sciences Liu, ZX Li, TG Li, PY Huang, QY Berne, S Saito, Y Cheng, ZB Wei, GJ Liu, LJ Li, Z The paleoclimatic events and cause in the Okinawa Trough during 50 kaBP |
topic_facet |
Okinawa Trough Sudden Paleoclimatic Change Events Polarity Reversal Events Late Quaternary Multidisciplinary Sciences |
description |
Planktonic foraminiferal delta O-18 record for core DGKS9603 from the Okinawa Trough shows a series of climatic fluctuations and sudden cooling events in short time scale during 50 kaBP, which appear to correlate closely to the Younger Dryas and Heinrich events H1-5 recorded in Chinese loess, the South China Sea, the North Atlantic cores and the Greenland ice cores. Three polarity reversal events, correlating to Gothenburg, Mungo and Laschamp events, approximately correspond to Heinrich events H1, H3 and H5 respectively, which could be a cause of global climate changes. The delta O-18 curve of the Okinawa Trough is well associated with the grain size record of the Lijiayuan loess profile in northwestern China and is somewhat different from the climate fluctuations documented in the Greenland ice cores. These correlation results indicate that regional factors play an important role in controlling the climate changes in the East Asia, and the East Asian Monsoon could be the prominent regional controlling factor. Planktonic foraminiferal delta O-18 record for core DGKS9603 from the Okinawa Trough shows a series of climatic fluctuations and sudden cooling events in short time scale during 50 kaBP, which appear to correlate closely to the Younger Dryas and Heinrich events H1-5 recorded in Chinese loess, the South China Sea, the North Atlantic cores and the Greenland ice cores. Three polarity reversal events, correlating to Gothenburg, Mungo and Laschamp events, approximately correspond to Heinrich events H1, H3 and H5 respectively, which could be a cause of global climate changes. The delta O-18 curve of the Okinawa Trough is well associated with the grain size record of the Lijiayuan loess profile in northwestern China and is somewhat different from the climate fluctuations documented in the Greenland ice cores. These correlation results indicate that regional factors play an important role in controlling the climate changes in the East Asia, and the East Asian Monsoon could be the prominent regional controlling ... |
format |
Article in Journal/Newspaper |
author |
Liu, ZX Li, TG Li, PY Huang, QY Berne, S Saito, Y Cheng, ZB Wei, GJ Liu, LJ Li, Z |
author_facet |
Liu, ZX Li, TG Li, PY Huang, QY Berne, S Saito, Y Cheng, ZB Wei, GJ Liu, LJ Li, Z |
author_sort |
Liu, ZX |
title |
The paleoclimatic events and cause in the Okinawa Trough during 50 kaBP |
title_short |
The paleoclimatic events and cause in the Okinawa Trough during 50 kaBP |
title_full |
The paleoclimatic events and cause in the Okinawa Trough during 50 kaBP |
title_fullStr |
The paleoclimatic events and cause in the Okinawa Trough during 50 kaBP |
title_full_unstemmed |
The paleoclimatic events and cause in the Okinawa Trough during 50 kaBP |
title_sort |
paleoclimatic events and cause in the okinawa trough during 50 kabp |
publishDate |
2001 |
url |
http://ir.qdio.ac.cn/handle/337002/3817 |
genre |
Greenland Greenland ice cores North Atlantic |
genre_facet |
Greenland Greenland ice cores North Atlantic |
op_relation |
CHINESE SCIENCE BULLETIN Liu, ZX; Li, TG; Li, PY; Huang, QY; Berne, S; Saito, Y; Cheng, ZB; Wei, GJ; Liu, LJ; Li, Z.The paleoclimatic events and cause in the Okinawa Trough during 50 kaBP,CHINESE SCIENCE BULLETIN,2001,46(2):153-157 http://ir.qdio.ac.cn/handle/337002/3817 |
_version_ |
1810446589033971712 |