کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
6303487 1618252 2014 10 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Evidence of Holocene millennial-scale climatic change from Gonghe Basin peat deposit, northeastern Qinghai-Tibet Plateau
ترجمه فارسی عنوان
شواهد تغییرات اقلیمی هولوسن در هزاره ی دهه ی هفتاد و هشتم از ذخایر قلیایی حوضه ی گونگه، قطب شمال چینگ های تبت
کلمات کلیدی
تغییرات آب و هوایی، رویدادهای سرد، ساز و کار اجباری، حوضه گونگ، هولوسن،
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات فرآیندهای سطح زمین
چکیده انگلیسی
The northeastern Qinghai-Tibetan Plateau (QTP) lies at the convergence of the Asian winter and summer monsoons and westerlies, making it an ideal place for studying the effects of climatic change, owing to its fragile ecological environment and unique geographical location. This paper reports on a multi-proxy analysis consisting of magnetic susceptibility, total organic carbon content (TOC), pollen, grain size, and geochemical parameters from the peat deposit in the Gonghe Basin to reconstruct the Holocene millennial-scale climatic variation. The results indicate that the climate tended to be warm and humid since 10.0 cal ka BP, but it deteriorated obviously (cold and dry) in 8.6-7.1 cal ka BP. The regional optimal warm and humid period was from 7.1-3.8 cal ka BP, although there were frequent climatic fluctuations during that time. Thereafter, the climate became cold and dry. 10 millennial-time-scale cold events were recorded, which were coincident with climatic records from deep sediments in the North Atlantic Ocean, ice cores, lakes, peat, and aeolian deposits in the QTP. In addition, we discovered that the southwestern monsoons forced by solar insolation in the Holocene have crucial effects on regional climatic change, and the millennial-scale cold fluctuations are possibly related to the thermohaline circulation (THC).
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Journal of Arid Environments - Volume 106, July 2014, Pages 1-10
نویسندگان
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