کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
8868467 | 1622102 | 2018 | 55 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
Sedimentary evolution of the Yangtze River mouth (East China Sea) over the past 19,000Â years, with emphasis on the Holocene variations in coastal currents
ترجمه فارسی عنوان
تکامل رسوب دهانه رودخانه یانگ تسه (دریای چین شرقی) در طول 19،000 سال گذشته، با تأکید بر تغییرات هولسن در جریان ساحلی
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کلمات کلیدی
دلتا یانگ تسه، آخرین انفجار، هولوسن، محیط زیست، جریان ساحلی، میکروفوسل،
موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
فرآیندهای سطح زمین
چکیده انگلیسی
Water mass variations in the early Yangtze estuary during the postglacial transgression have not been thoroughly studied. This research gap has hampered the understanding of riverine sediment 'source to sink' processes in this region. This study presents the results of integrated analyses of grain size, pollen-spore-dinocyst assemblages, benthic foraminifera and ostracods from a borehole, H5, located at the northern Yangtze mouth, to investigate the complete sedimentary history and associated variations in coastal currents since 19Â ka. At the core site, a fluvial floodplain developed from ca. 19-11.3Â ka, whereas an estuary to shelf to subaqueous delta prevailed during most of the Holocene. Based on changes in the dominant microfauna species, which mainly consist of Chinese coastal water species, two main current patterns were distinguished: one dominated by the Yellow Sea coastal current (YSCC) before ca. 7.9Â ka and one dominated by the Yangtze dilute water (YDW). Marked increases in open-sea saline species, including Bolivina robusta, and stratified water dinocyst species Spiniferites ramous and Spiniferites spp. were interpreted as the encroachment of the Taiwan warm current (TWWC) and the intensification of the YDW, respectively. The YDW and TWWC penetrated the area dominated by the YSCC before 7.9Â ka, which was likely related to intensity variations in the Kuroshio Current (KC) and Asian summer monsoon (ASM). Under maximal ASM and KC conditions, upwelling resulted from the intensified intrusion of the TWWC, as indicated by the blooming of Bolivina robusta from 7.9-6.3Â ka. After ca. 6Â ka, the YDW clearly weakened due to the decline of the ASM, yet the Yangtze plume prevailed due to the rapid seaward migration of the Yangtze mouth. Considering the dominance of the YSCC in the early Holocene, Yellow River-derived sediment likely represented a large proportion of the material delivered to the early Yangtze estuary.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Palaeogeography, Palaeoclimatology, Palaeoecology - Volume 490, 15 January 2018, Pages 431-449
Journal: Palaeogeography, Palaeoclimatology, Palaeoecology - Volume 490, 15 January 2018, Pages 431-449
نویسندگان
Baocheng Zhao, Xuexin Yan, Zhanghua Wang, Yujin Shi, Zhongyuan Chen, Jianlei Xie, Jing Chen, Zhongfa He, Qing Zhan, Xiao Li,