TY - JOUR
T1 - Abundance and distribution of fatty acids in hydrothermal vent sediments of the western Pacific Ocean
AU - Yamanaka, Toshiro
AU - Sakata, Susumu
N1 - Funding Information:
We thank all the crew members of RV Natsushima and the operating team of Shinkai 2000 . We are grateful to all scientists and scientific staff of JAMSTEC (Japan Marine Science and Technology Center) who participated in the cruises. Particularly, Prof. H. Chiba, Okayama University, and Dr. J. Ishibashi, Kyushu University, are thanked for helping us collect sediment samples. We are grateful to Dr. Chris Parrish and Dr. Cathy Allen for improvement of early version of our manuscript and editorial handling of Dr. John Volkman. Thanks are also due to Prof. T. Murae and Dr. F. Kitajima, Kyushu University, for insightful comments to the content of this paper. This research was partly funded by a grant-in-aid for Scientific Research (B-1) from JSPS (No. 15403014, organizer: Prof. T. Yamaguchi, Chiba University) and by a Ministry of Education, Culture, Sports, Science and Technology of Japan through Special Coordination Fund ‘Archaean Park’ project.
PY - 2004/5
Y1 - 2004/5
N2 - Sediments obtained from three active seafloor hydrothermal areas in the western Pacific Ocean were measured for the abundances and distributions of total fatty acids (TFAs). Approximately 50 fatty acids were identified, with the chain-length ranging from C9 to C29. The total concentrations of TFAs (∑TFA) show a wide range from 13.2 to 184 μg/g dry sediment. The values of ∑TFA, over 100 μg/g dry sediment, are significantly higher than those reported for non-hydrothermal seafloor sediments. Furthermore, the observed compositions of TFAs are rich in bacterial biomarkers especially monounsaturated fatty acids, which is common to sediments and symbiotic animal tissues from other sites associated with hydrothermal activities. High ratios of ∑TFA to total organic carbon content (TOC) relative to the non-hydrothermal seafloor sediment may also reflect a large contribution of organic matter produced at the vents. Due to the limited sample availability from these environments, the TFA compositions were not enough to evaluate relatedness between the vent sediment and vent animal community, while the wide diversity of TFAs suggests a large variation in source organisms in these hydrothermal environments. This study confirms the high contribution of bacteria and other vent organisms to organic matter in the sediments.
AB - Sediments obtained from three active seafloor hydrothermal areas in the western Pacific Ocean were measured for the abundances and distributions of total fatty acids (TFAs). Approximately 50 fatty acids were identified, with the chain-length ranging from C9 to C29. The total concentrations of TFAs (∑TFA) show a wide range from 13.2 to 184 μg/g dry sediment. The values of ∑TFA, over 100 μg/g dry sediment, are significantly higher than those reported for non-hydrothermal seafloor sediments. Furthermore, the observed compositions of TFAs are rich in bacterial biomarkers especially monounsaturated fatty acids, which is common to sediments and symbiotic animal tissues from other sites associated with hydrothermal activities. High ratios of ∑TFA to total organic carbon content (TOC) relative to the non-hydrothermal seafloor sediment may also reflect a large contribution of organic matter produced at the vents. Due to the limited sample availability from these environments, the TFA compositions were not enough to evaluate relatedness between the vent sediment and vent animal community, while the wide diversity of TFAs suggests a large variation in source organisms in these hydrothermal environments. This study confirms the high contribution of bacteria and other vent organisms to organic matter in the sediments.
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U2 - 10.1016/j.orggeochem.2004.01.002
DO - 10.1016/j.orggeochem.2004.01.002
M3 - Article
AN - SCOPUS:1842688712
SN - 0146-6380
VL - 35
SP - 573
EP - 582
JO - Organic Geochemistry
JF - Organic Geochemistry
IS - 5
ER -