Hydrogen and carbon isotope responses to salinity in greenhouse-cultivated mangroves
Paired hydrogen and carbon isotope ratios (2 H/1 H and 13 C/12 C) of mangrove lipids can
be used to quantitatively reconstruct past salinity and 2 H/1 H ratios of environmental water,
and in some cases precipitation rate. This approach is based on the observation that net 2 H-
and 13 C-fractionation increases and decreases, respectively, with the salinity of
environmental water. In order to better understand the mechanisms underlying these
empirical observations and ultimately improve estimates of paleoprecipitation from the …
be used to quantitatively reconstruct past salinity and 2 H/1 H ratios of environmental water,
and in some cases precipitation rate. This approach is based on the observation that net 2 H-
and 13 C-fractionation increases and decreases, respectively, with the salinity of
environmental water. In order to better understand the mechanisms underlying these
empirical observations and ultimately improve estimates of paleoprecipitation from the …
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