Biomarkers, chemistry and microbiology show chemoautotrophy in a multilayer chemocline in the Cariaco Basin

被引:69
|
作者
Wakeham, Stuart G. [1 ]
Turich, Courtney [1 ]
Schubotz, Florence [2 ,3 ]
Podlaska, Agnieszka [4 ]
Li, Xiaona N. [4 ]
Varela, Ramon [7 ]
Astor, Yrene [7 ]
Saenz, James P. [5 ]
Rush, Darci [6 ]
Damste, Jaap S. Sinninghe [6 ]
Summons, Roger E. [5 ]
Scranton, Mary I. [4 ]
Taylor, Gordon T. [4 ]
Hinrichs, Kai-Uwe [2 ,3 ]
机构
[1] Skidaway Inst Oceanog, Savannah, GA USA
[2] Univ Bremen, MARUM Ctr Marine Environm Sci, D-28359 Bremen, Germany
[3] Univ Bremen, Dept Geosci, D-28359 Bremen, Germany
[4] SUNY Stony Brook, Sch Marine & Atmospher Sci, Stony Brook, NY 11794 USA
[5] MIT, Dept Earth Atmospher & Planetary Sci, Cambridge, MA USA
[6] Royal Netherlands Inst Sea Res, Texel, Netherlands
[7] Fdn Salle Ciencias Nat, Estn Invest Marinas Margarita, Edo Nueva Esparta, Venezuela
基金
美国国家科学基金会;
关键词
Cariaco Basin; Particulate matter; Lipid biomarkers; Bacteria; Archaea; Ammonium oxidation; Sulfur oxidation; Chemoautotrophy; ANAEROBIC AMMONIUM OXIDATION; TRANSPARENT EXOPOLYMER PARTICLES; CARBON-ISOTOPIC COMPOSITIONS; LADDERANE LIPID DISTRIBUTION; GLYCEROL TETRAETHER LIPIDS; OXYGEN-MINIMUM-ZONE; INTACT POLAR LIPIDS; MEMBRANE-LIPIDS; BLACK-SEA; WATER-COLUMN;
D O I
10.1016/j.dsr.2012.01.005
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
The Cariaco Basin is the world's largest truly marine anoxic basin. We have conducted a comprehensive multidisciplinary investigation of the water column (42-750 m) bracketing the redox boundary (a 250-m thick "chemocline") of the Cariaco Basin to evaluate linkages between lipid biomarkers, distributions of major dissolved chemical species, and the microbial community and associated redox processes. Our multidimensional data set includes: hydrography, water column chemistry, microbial distributions and rates, and lipid biomarkers. Multivariant statistical analysis of this data set partitions the investigated water column into 5 distinct zones, each characterized by different chemistries, microbiologies and biomarker compositions. The core of this chemocline is a 25-m thick suboxic zone where both dissolved oxygen and sulfide were below detection limits, bacterial and archaeal cell numbers and the rate of chemoautotrophic (dark) carbon fixation are elevated, and dissolved chemical species and bacterial and archaeal lipid biomarkers are indicative of tightly coupled cycles of carbon, nitrogen, and sulfur through chemoautotrophy. (C) 2012 Elsevier Ltd. All rights reserved.
引用
收藏
页码:133 / 156
页数:24
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