Bacteriohopanepolyol distribution in Yenisei River and Kara Sea suspended particulate matter and sediments traces terrigenous organic matter input

被引:11
作者
De Jonge, Cindy [1 ]
Talbot, Helen M. [2 ]
Bischoff, Juliane [2 ]
Stadnitskaia, Alina [1 ]
Cherkashov, Georgy [3 ]
Damste, Jaap S. Sinninghe [1 ]
机构
[1] NIOZ Royal Netherlands Inst Sea Res, Dept Marine Organ Biogeochem, POB 59, NL-1790 AB Den Burg, Texel, Netherlands
[2] Newcastle Univ, Sch Civil Engn & Geosci, Drummond Bldg, Newcastle Upon Tyne NE1 7RU, Tyne & Wear, England
[3] Russian Acad Sci, All Russian Res Inst Geol & Mineral Resources Wor, Minist Nat Resources, St Petersburg 196140, Russia
基金
欧洲研究理事会; 英国自然环境研究理事会;
关键词
METHANOTROPHIC BACTERIA; TETRAETHER LIPIDS; CARBON TRANSPORT; CLIMATE-CHANGE; ARCTIC-OCEAN; HOPANOIDS; BIOMARKERS; PERMAFROST; METHANE; POPULATIONS;
D O I
10.1016/j.gca.2015.11.008
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Bacteriohopanepolyols (BHPs) are ubiquitous bacterial membrane lipids, encountered in soils, river and marine suspended particulate matter (SPM) and sediments. Their abundance and distribution provides a direct means to identify bacterial inputs and can be used to trace soil-derived bacterial organic matter (OM) and in some cases the presence of bacterial groups and their activities in aquatic systems. We have studied the BHP distribution in the SPM of a major Siberian River (Yenisei River) that crosses a large latitudinal gradient, draining a large part of Mongolia and Siberian Russia. The Yenisei River is the main river to flow into the Kara Sea, a shelf sea of the Arctic Ocean. We show that the BHP distribution and concentration of SPM and surface sediments of the Yenisei Outflow in the Kara Sea allow to trace soil-marker BHPs and evaluate the performance of the R-soil' index, a proxy developed to trace bacterial soil-derived OM. Soil-marker BHPs are present in the Yenisei River, and their concentration decreases from the Yenisei River Outflow into the offshore marine sediments. The R-soil' correlates well with an independent proxy for bacterial OM, the BIT-index (r(2) = 0.82) and has a moderate correlation with the delta C-13(org) values, a bulk OM proxy for terrigenous input (r(2) = 0.44). Consequently, the R-soil' index performs well in the Kara Sea, strengthening its application for tracing bacterial OM in the Arctic Ocean, both in modern and downcore sediments. Furthermore, a suite of BHPs that are characteristic for methanotrophic bacteria, i.e. 35-aminobacteriohopane-30,31,32,33,34-pentol (aminopentol) and 35-aminobacteriohopane-31,32,33,34-tetrol (aminotetrol), is encountered in the Yenisei Outflow sediments. These components are partly sourced from terrigenous sources, but are likely also produced in-situ in the marine sediments. The distribution of the pentafunctionalized cyclitol ether BHP in the marine systems is noteworthy, and indicates that it can possibly be applied as a marker for cyanobacterial biomass in marine sediments. (c) 2015 Elsevier Ltd. All rights reserved.
引用
收藏
页码:85 / 101
页数:17
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