TY - JOUR
T1 - Concentrations and distributions of amino acids in black and white smoker fluids at temperatures over 200°C
AU - Fuchida, Shigeshi
AU - Mizuno, Yuki
AU - Masuda, Harue
AU - Toki, Tomohiro
AU - Makita, Hiroko
N1 - Funding Information:
We thank Nakamura K. (chief scientist) and the other members of the NT12-24 cruise. We would also like to thank Takahashi, Y. and Kikuchi, S. for providing the hydrothermal fluid chemistry data. This study was financially supported by the Ministry of Education, Culture, Sports, Science and Technology (MEXT) of Japan through a special coordination fund (Project TAIGA: Trans-crustal Advection and in situ reaction of Global subseafloor Aquifer). We thank Philip A. Meyers, University of Michigan and the reviewers for their thoughtful comments that helped us to improve this contribution.
PY - 2014/1
Y1 - 2014/1
N2 - The distribution of amino acids in seafloor hydrothermal systems was investigated through the determination of the concentrations of total hydrolysable amino acids (THAAs), dissolved free amino acids (DFAAs) and cell density in>200°C black and white smoker fluids sampled from the Mariana Trough. THAA concentrations of>10μM were detected in the black and white smoker fluids, which are higher than those of low temperature (< 53°C) fluids and ambient seawater (< 1μM). 1.4×104-8.6×105cell/ml of microbe was detected from low temperature hydrothermal fluids (< 100°C) and ambient seawater. The concentration of THAAs increased with increasing temperature, although the cell density decreased in high temperature fluid (> 150°C). The bioactivity would be restricted under the high temperature condition.Levels of DFAAs (< 0.7. μM) were very low, suggesting that the amino acids existed mainly as polymers in these hydrothermal fluids. The amino acid polymers plausibly derive from biological protein and dissolve during the reaction of hydrothermal fluids along flow paths around the hydrothermal vents.Amino acids are considered to be unstable under hydrothermal condition (> 200. °C). However, labile amino acids (e.g., Asp and Ser) were abundant in high temperature fluids. These amino acids would be protected by reaction with inorganic compounds. The behavior of the amino acids derived from organisms around hydrothermal vents would be constrained more by abiotic physico-chemical reactions than biological activities in hydrothermal systems.
AB - The distribution of amino acids in seafloor hydrothermal systems was investigated through the determination of the concentrations of total hydrolysable amino acids (THAAs), dissolved free amino acids (DFAAs) and cell density in>200°C black and white smoker fluids sampled from the Mariana Trough. THAA concentrations of>10μM were detected in the black and white smoker fluids, which are higher than those of low temperature (< 53°C) fluids and ambient seawater (< 1μM). 1.4×104-8.6×105cell/ml of microbe was detected from low temperature hydrothermal fluids (< 100°C) and ambient seawater. The concentration of THAAs increased with increasing temperature, although the cell density decreased in high temperature fluid (> 150°C). The bioactivity would be restricted under the high temperature condition.Levels of DFAAs (< 0.7. μM) were very low, suggesting that the amino acids existed mainly as polymers in these hydrothermal fluids. The amino acid polymers plausibly derive from biological protein and dissolve during the reaction of hydrothermal fluids along flow paths around the hydrothermal vents.Amino acids are considered to be unstable under hydrothermal condition (> 200. °C). However, labile amino acids (e.g., Asp and Ser) were abundant in high temperature fluids. These amino acids would be protected by reaction with inorganic compounds. The behavior of the amino acids derived from organisms around hydrothermal vents would be constrained more by abiotic physico-chemical reactions than biological activities in hydrothermal systems.
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U2 - 10.1016/j.orggeochem.2013.11.008
DO - 10.1016/j.orggeochem.2013.11.008
M3 - Article
AN - SCOPUS:84890134001
SN - 0146-6380
VL - 66
SP - 98
EP - 106
JO - Organic Geochemistry
JF - Organic Geochemistry
ER -