Extreme                          13                         C depletions in seawater-derived brines and their implications for the past geochemical carbon cycle

B. Lazar; J. Erez

doi:10.1130/0091-7613(1990)018<1191:ECDISD>2.3.CO;2

Extreme ¹³ C depletions in seawater-derived brines and their implications for the past geochemical carbon cycle

B. Lazar, J. Erez

Fredy & Nadine Herrmann Institute of Earth Sciences

Research output: Contribution to journal › Article › peer-review

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Abstract

Extreme depletions in the ¹³ C content of the total dissolved inorganic carbon (C _T ) were found in brines overlying microbial mat communities. Total alkalinity (A _T ) and C _T in the brines suggest that intense photosynthetic activity of the microbial mat communities depletes the C _T from the brine. -from Authors

Original language	English
Pages (from-to)	1191-1194
Number of pages	4
Journal	Geology
Volume	18
Issue number	12
DOIs	https://doi.org/10.1130/0091-7613(1990)018<1191:ECDISD>2.3.CO;2
State	Published - 1990

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10.1130/0091-7613(1990)018<1191:ECDISD>2.3.CO;2

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title = " Extreme 13 C depletions in seawater-derived brines and their implications for the past geochemical carbon cycle ",

abstract = " Extreme depletions in the 13 C content of the total dissolved inorganic carbon (C T ) were found in brines overlying microbial mat communities. Total alkalinity (A T ) and C T in the brines suggest that intense photosynthetic activity of the microbial mat communities depletes the C T from the brine. -from Authors ",

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AB - Extreme depletions in the 13 C content of the total dissolved inorganic carbon (C T ) were found in brines overlying microbial mat communities. Total alkalinity (A T ) and C T in the brines suggest that intense photosynthetic activity of the microbial mat communities depletes the C T from the brine. -from Authors

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Extreme ¹³ C depletions in seawater-derived brines and their implications for the past geochemical carbon cycle

Abstract

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