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  Reconstruction of the Late Holocene climate and environmental history from North Bolgoda Lake, Sri Lanka, using lipid biomarkers and pollen records

Gayantha, K., Routh, J., Anupama, K., Lazar, J., Prasad, S., Chandrajith, R., Roberts, P., & Gleixner, G. (2020). Reconstruction of the Late Holocene climate and environmental history from North Bolgoda Lake, Sri Lanka, using lipid biomarkers and pollen records. Journal of Quaternary Science, 35(4):, pp. 514-525. doi:10.1002/jqs.3196.

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アイテムのパーマリンク: https://hdl.handle.net/21.11116/0000-0006-1084-2 版のパーマリンク: https://hdl.handle.net/21.11116/0000-0007-616C-3
資料種別: 学術論文

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shh2564.pdf (出版社版), 2MB
ファイルのパーマリンク:
https://hdl.handle.net/21.11116/0000-0006-1086-0
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shh2564.pdf
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application/pdf / [MD5]
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作成者

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 作成者:
Gayantha, Kasun, 著者
Routh, Joyanto, 著者
Anupama, Krishnamurthy, 著者
Lazar, Jean, 著者
Prasad, Srinivasan, 著者
Chandrajith, Rohana, 著者
Roberts, Patrick1, 著者           
Gleixner, Gerd, 著者
所属:
1Archaeology, Max Planck Institute for the Science of Human History, Max Planck Society, ou_2074312              

内容説明

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キーワード: biomarker, carbon isotopes, monsoon, palaeosalinity, pollen
 要旨: The catastrophic impact and unpredictability of the Indian Ocean Monsoon (IOM) over South Asia are evident from devastating floods, mudslides and droughts in one of the most densely populated regions of the globe. However, our understanding as to how the IOM has varied in the past, as well as its impact on local environments, remains limited. This is particularly the case for Sri Lanka, where erosional landscapes have limited the availability of well-stratified, high-resolution terrestrial archives. Here, we present novel data from an undisturbed sediment core retrieved from the coastal Bolgoda Lake. This includes the presentation of a revised Late Holocene age model as well as an innovative combination of pollen, source-specific biomarkers, and compound-specific stable carbon isotopes of n-alkanes to reconstruct the shifts in precipitation, salinity and vegetation cover. Our record documents variable climate between 3000 years and the present, with arid conditions c. 2334 and 2067 cal a bp. This extreme dry period was preceded and followed by more wet conditions. The high-resolution palaeoenvironmental reconstruction fills a major gap in our knowledge on the ramifications of IOM shifts across South Asia and provides insights during a time of major redistribution of dense human settlements across Sri Lanka.

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言語: eng - English
 日付: 2020-03-202020-05
 出版の状態: 出版
 ページ: 12
 出版情報: -
 目次: Introduction
Background, materials and methods
- Study area and site
- Sampling
- Age–depth model
- Biomarker analysis
- Compound‐specific carbon isotope analysis
- Pollen analysis
Results
- Chronology and climate zones
- Biomarker trends and ratios of n‐alkanes
- Triterpenols
- δ13C isotopes in n‐alkanes
- Pollen
Discussion
- Palaeoenvironmental implications
- Mangrove vegetation, palaeosalinity changes and droughts
- Palaeoclimate and palaeoenvironmental reconstruction
- Zone 1 (2960 to 2390 cal a bp; 385–252 cm)
- Zone 2 (2390 to 1800 cal a bp; 252–140 cm)
- Zone 3 (1800 to 1318 cal a bp; 140–60 cm)
- Zone 4 (1318 cal a bp to present; 60–0 cm)
- South Asian comparisons and potential human implications
Conclusions
 査読: 査読あり
 識別子(DOI, ISBNなど): DOI: 10.1002/jqs.3196
その他: shh2564
 学位: -

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出版物 1

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出版物名: Journal of Quaternary Science
種別: 学術雑誌
 著者・編者:
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出版社, 出版地: Chichester : John Wiley & Sons, Ltd.
ページ: - 巻号: 35 (4) 通巻号: jqs.3196 開始・終了ページ: 514 - 525 識別子(ISBN, ISSN, DOIなど): ISSN: 0267-8179
CoNE: https://pure.mpg.de/cone/journals/resource/954925500137