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DOI | 10.1016/j.quascirev.2020.106490 |
Multi-proxy approach to unravel methane emission history of an Arctic cold seep | |
Yao H.; Niemann H.; Panieri G. | |
发表日期 | 2020 |
ISSN | 0277-3791 |
卷号 | 244 |
英文摘要 | Arctic Ocean sediments contain large amounts of methane in the form of free gas and gas hydrate. This highly dynamic methane reservoir is susceptible to be modified by bottom water warming. The warming may lead to gas hydrate destabilization releasing elevated methane fluxes to the seafloor and seawater. Reconstructing past methane dynamics can be achieved by using specific proxies left in the geological record. In this study, we apply a multi-proxy approach for paleo seepage reconstruction from sediment records at gas hydrate mounds (GHMs) in Storfjordrenna (south of the Svalbard archipelago). These shallow water (∼380 m water depth) systems are potentially vulnerable to global warming related temperature changes. 14C dating of foraminifera shells indicated an onset of deglaciation in the Storfjordrenna region at ∼20 kyr BP and allowed us to establish a stratigraphic context based on sediment Zr/Rb and Fe/Ca ratios. Several major (between 15 and 17 kyr BP) and minor methane venting phases were identified and interpreted to be related to gas hydrate instability triggered by isostatic adjustment right after the onset of the deglaciation. The detection of all major methane releases was only possible by combining data sets of stable carbon isotope compositions of foraminifera, mineralogy and δ13C values of authigenic carbonates, and abundance and stable carbon isotope signatures of lipid biomarkers. The most robust single proxy in this study was provided by the δ13C values of archaeal biomarkers. In contrast, the sediment Ba/Ti ratios recorded only the major events. Our results highlight the complexity and heterogeneity of methane dynamics in a small area of some hundred meters across. © 2020 The Author(s) |
英文关键词 | Authigenic carbonates; Carbon isotopes; Foraminifera; Lipid biomarkers; Methane seepage reconstruction; Proxies |
语种 | 英语 |
scopus关键词 | Biomarkers; Carbon; Gases; Global warming; Hydration; Hydrocarbon seepage; Isotopes; Methane; Minerals; Sediments; Stratigraphy; Authigenic carbonates; Bottom-water warming; Foraminifera shells; Methane emissions; Methane reservoirs; Stable carbon isotope compositions; Stable carbon isotopes; Temperature changes; Gas hydrates; abundance; bottom water; carbon isotope; cold seep; deglaciation; foraminifera; gas hydrate; global warming; methane; seepage; shallow water; Arctic; Arctic Ocean; Svalbard; Svalbard and Jan Mayen; Archaea; Foraminifera |
来源期刊 | Quaternary Science Reviews
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/151350 |
作者单位 | CAGE - Centre for Arctic Gas Hydrate, Environment and Climate, Department of Geosciences, UiT the Arctic University of Norway in Tromsø, Norway; NIOZ Royal Institute for Sea Research, Department of Marine Microbiology and Biogeochemistry, And Utrecht University, P.O. Box 59, AB Den Burg, Texel, 1790, Netherlands; Department of Environmental Sciences, University of Basel, Bernoullistrasse 30, Basel, CH-4056, Switzerland |
推荐引用方式 GB/T 7714 | Yao H.,Niemann H.,Panieri G.. Multi-proxy approach to unravel methane emission history of an Arctic cold seep[J],2020,244. |
APA | Yao H.,Niemann H.,&Panieri G..(2020).Multi-proxy approach to unravel methane emission history of an Arctic cold seep.Quaternary Science Reviews,244. |
MLA | Yao H.,et al."Multi-proxy approach to unravel methane emission history of an Arctic cold seep".Quaternary Science Reviews 244(2020). |
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