Anomalies of bromine in the estuarine sediments as a signal of floods associated with typhoons

Ivan Kalugin; Anatolii Astakhov; Andrey Darin; Kirill Aksentov

doi:10.1007/s00343-015-4370-9

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Anomalies of bromine in the estuarine sediments as a signal of floods associated with typhoons

OriginalPaper | Updated：2023-05-16

- Anomalies of bromine in the estuarine sediments as a signal of floods associated with typhoons
- Anomalies of bromine in the estuarine sediments as a signal of floods associated with typhoons
- 海洋湖沼学报（英文） 2015年33卷第6期页码：1489-1495
- Affiliations：
  
  1. Sobolev Institute of Geology and Mineralogy Siberian Branch Russian Academy of Science
  2. . I. Il’ichev Pacific Oceanological Institute Far Eastern Branch Russian Academy of Science,V
- Author bio：
- Funds：
- DOI：10.1007/s00343-015-4370-9
  中图分类号：
- 网络首发：2015-11-06，
  
  纸质出版：2015
- Accepted：
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Anomalies of bromine in the estuarine sediments as a signal of floods associated with typhoons[J]. 海洋湖沼学报（英文）, 2015,33(6):1489-1495.

Kalugin, I., Astakhov, A., Darin, A. et al. Anomalies of bromine in the estuarine sediments as a signal of floods associated with typhoons., Chin. J. Ocean. Limnol. 33, 1489–1495 (2015). https://doi.org/10.1007/s00343-015-4370-9
Anomalies of bromine in the estuarine sediments as a signal of floods associated with typhoons[J]. 海洋湖沼学报（英文）, 2015,33(6):1489-1495. DOI： 10.1007/s00343-015-4370-9.

Kalugin, I., Astakhov, A., Darin, A. et al. Anomalies of bromine in the estuarine sediments as a signal of floods associated with typhoons., Chin. J. Ocean. Limnol. 33, 1489–1495 (2015). https://doi.org/10.1007/s00343-015-4370-9 DOI：

摘要

Abstract

X-ray fluorescence scanning with synchrotron radiation was performed to study sediment core records of floods in Amur Bay

Sea of Japan. Interlayers of 3–8 mm with abnormally low bromine content were formed by the Razdolnaya River discharge to the central part of the bay during extreme floods

accompanied by severe storms at sea. Such conditions in the region are typical for periods of deep tropical cyclones (typhoons)

to which the distinguished interlayers were compared on the timescale. This approach was made possible thanks to the high rate of sedimentation in the bay (3–5 mm/a) and low bioturbation of sediments under anoxic conditions.

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references

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