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名   称 A rapid hydroclimate change and its influence on the Songliao Basin during the Santonian-Campanian transition as recorded by compound-specific isotopes
科技资源标识 CSTR:11738.14.NCDC.XDA14.PP4409.2024
DOI 10.1016/j.palaeo.2020.109674
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摘   要 paleoclimate and paleoenvironment of the Songliao Basin has important theoretical and
practical significance to reveal the regional continental climate characteristics and continental organic matter
accumulation under the Cretaceous greenhouse climate conditions. Here, we report the composition of bio_x0002_markers and the stable carbon and hydrogen isotope compositions of n-alkanes from Nenjiang Formation sediments in the Songliao Basin, which provide information on the source of organisms, paleoenvironmental
conditions, and paleoclimate changes during the Late Cretaceous. Our hydrogen isotope records of n-alkanes
displayed a significantly negative shift, indicating that a dramatically wet climate occurred during the
Santonian-Campanian transition. A wet climate, such as that during a prolonged rainfall event, had a significant
impact on the lake and resulted in the lake level increasing and the salinity decreasing in the surface water
during this period. However, the freshwater input increased the salinity difference between the upper and lower
water layers, which caused stable water stratification to occur in the lake. In addition, the high total organic
carbon (TOC) content indicates high primary productivity because of increased precipitation carrying more
terrigenous nutrients into the lake, which resulted in eutrophication during this period. Notably, the increased
aryl isoprenoid ratios and the occurrence of isorenieratane indicates that photic zone euxinia (PZE) was enhanced during the Santonian-Campanian transition, which was possibly due to the dramatic change in the
hydroclimate. We speculate that the large freshwater input promoted the formation of PZE in the lake. Then, PZE
restricted the habitat available for aerobic organisms, which had fatal effects on the lake ecosystem.
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作者 Li Wang
数据量 3.1 MiB
论文类型: journal
论文网址: https://doi.org/10.1016/j.palaeo.2020.109674
期刊名称: Palaeogeography, Palaeoclimatology, Palaeoecology
出版时间: 2020-05-15
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数据引用
Li Wang. A rapid hydroclimate change and its influence on the Songliao Basin during the Santonian-Campanian transition as recorded by compound-specific isotopes. 国家冰川冻土沙漠科学数据中心(http://www.ncdc.ac.cn), 2024. https://cstr.cn/CSTR:11738.14.NCDC.XDA14.PP4409.2024.
Li Wang. A rapid hydroclimate change and its influence on the Songliao Basin during the Santonian-Campanian transition as recorded by compound-specific isotopes. 国家冰川冻土沙漠科学数据中心(http://www.ncdc.ac.cn), 2024. https://www.doi.org/10.1016/j.palaeo.2020.109674.
许可协议
知识共享许可协议   本作品采用 知识共享署名 4.0 国际许可协议进行许可。

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