Geochemistry of Middle Holocene sediments from south Yellow Sea: Implications to provenance and climate change

Xiaoxia Lü; Gerard J. M. Versteegh; Jinming Song; Xuegang Li; Huamao Yuan; Ning Li

doi:10.1007/s12583-015-0577-0

Volume 27 Issue 5

Sep 2016

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Journal of Earth Science > 2016 > 27(5): 751-762.

Xiaoxia Lü, Gerard J. M. Versteegh, Jinming Song, Xuegang Li, Huamao Yuan, Ning Li. Geochemistry of Middle Holocene sediments from south Yellow Sea: Implications to provenance and climate change. Journal of Earth Science, 2016, 27(5): 751-762. doi: 10.1007/s12583-015-0577-0

Citation:

Xiaoxia Lü, Gerard J. M. Versteegh, Jinming Song, Xuegang Li, Huamao Yuan, Ning Li. Geochemistry of Middle Holocene sediments from south Yellow Sea: Implications to provenance and climate change. Journal of Earth Science, 2016, 27(5): 751-762. doi: 10.1007/s12583-015-0577-0

Citation:

Xiaoxia Lü, Gerard J. M. Versteegh, Jinming Song, Xuegang Li, Huamao Yuan, Ning Li. Geochemistry of Middle Holocene sediments from south Yellow Sea: Implications to provenance and climate change. Journal of Earth Science, 2016, 27(5): 751-762. doi: 10.1007/s12583-015-0577-0

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Geochemistry of Middle Holocene sediments from south Yellow Sea: Implications to provenance and climate change

doi: 10.1007/s12583-015-0577-0

1.
Faculty of Marine Sciences, China University of Geosciences, Wuhan, 430074, China
2.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430074, China
3.
Heisenberg Group on Marine Kerogen, Center for Marine Environmental Sciences (MARUM), Bremen University, Bremen, D-28359, Germany
4.
Institute of Oceanology, Chinese Academy of Sciences, Qingdao, 266072, China

More Information

Corresponding author: Xiaoxia Lü, luxiaox@163.com
Received Date: 24 Jul 2014
Accepted Date: 07 Nov 2014
Publish Date: 01 Oct 2016

Abstract

Abstract

From a large number of case studies on terrestrial deposits we know that Late Holocene climate fluctuations have an important impact on the terrestrial environments. However, it is hitherto not clear how the marine sediments can be used to shed light on the environment and climate change of the catchment. To provide such insight, we used the major element, trace element and rare earth element (REE) compositions in the southern Yellow Sea (SYS) sediments to reconstruct the changes in weathering and erosion of their source regions. The sediments originate predominantly from the upper crust of East China and are transported into the basin especially by the Yellow River (Huanghe) and to a lesser extent by the Yangtze River (Changjiang). The chemical index of alteration (CIA; 53.7-59.7) suggests low chemical weathering of the source rocks since the Middle Holocene. This is consistent with the relatively cool and arid climate in North China after the Holocene Megathermal. Comparison of element ratios, including Al/Ca, K/Ca, Al/Na, K/Na, Rb/Sr, Li/Ba and the CIA shows that we can use the latter as a robust proxy for climate change. The CIA-based mean annual precipitation and mean annual temperature show a series of climate fluctuations in the catchment. A relatively warm and humid Period Ⅰ (5.3-2.9 cal. ka BP), a relatively cool and dry Period Ⅱ (2.9-0.9 cal. ka BP) and an increasingly cool and dry Period Ⅲ (0.9-0.3 cal. ka BP). These periods can be linked to climate intervals recognized elsewhere.
- geochemical composition,
- elemental ratio,
- climate change,
- provenance,
- South Yellow Sea sediment

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Geochemistry of Middle Holocene sediments from south Yellow Sea: Implications to provenance and climate change

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Geochemistry of Middle Holocene sediments from south Yellow Sea: Implications to provenance and climate change

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