Isotopic Fractionation during Cellulose Synthesis in Two Mangrove Species: Salinity Effects

نویسندگان

  • NAOMI ISH-SHALOM-GORDON
  • GUANGHUI LIN
چکیده

Carbon, non-exchangeable hydrogen, and oxygen isotope ratios of cellulose of Avicennia germinans and Rkizophora mangle plants hydroponically grown under different salinities (0, 18, 45% sea water, but with irrigation waters having the same isotopic ratios) were measured to determine the possibility of using isotopic ratios of plant tissues as biological recorders of sea level rise. There was a large variability in the 6D values of leaf nitrated cellulose between different treatments and even within a single treatment for both A. germinans and R. mangle. Thus, 6D values of non-exchangeable hydrogens of cellulose cannot be used as a historical tracer for utilization of ocean water or freshwater by mangroves. In contrast, 6 ‘*O values of cellulose were not significantly different between different salinity treatments for both mangroves, indicating that 6l*O of cellulose can be used as a sea water tracer. 613C values of cellulose did not vary directly with salinity as has been observed with other plants. 6’ 3C values of cellulose from A. germinans were the lowest for plants growing at 18% sea water, with cellulose from plants growing in 0 and 45% sea water having significantly higher 6 13C values. 613C values of cellulose from R. mangle were the highest for plants grown in 45% sea water, with plants grown in 0 and 18% sea water having equally lower 613C values.

برای دانلود متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

ثبت نام

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

منابع مشابه

Variation in oxygen isotope fractionation during cellulose synthesis: intramolecular and biosynthetic effects.

The oxygen isotopic composition of plant cellulose is commonly used for the interpretations of climate, ecophysiology and dendrochronology in both modern and palaeoenvironments. Further applications of this analytical tool depends on our in-depth knowledge of the isotopic fractionations associated with the biochemical pathways leading to cellulose. Here, we test two important assumptions regard...

متن کامل

Hydrogen and Oxygen Isotopic Fractionation During Heterotrophic Cellulose Synthesis

Hydrogen and oxygen isotopic fractionation relative to medium water for two different carbohydrate metabolic pathways leading to cellulose synthesis were measured. This was accomplished by analysing stable hydrogen and oxygen isotope ratios of water and cellulose for seedlings. The seedlings had been germinated and heterotrophically grown in closed vessels from species having starch (Triticum a...

متن کامل

Inverse relationship between salinity and n-alkane dD values in the mangrove Avicennia marina

Hydrogen isotope ratios in lipids derived frommangroves have the potential to be used for paleohydrologic reconstructions and could serve as a much needed tool for establishing past climate variability in the tropics. We assessed the effect of salinity on the apparent fractionation factor, aa, between mangrove derived n-alkanes and their source water for Avicennia marina (gray mangrove) specime...

متن کامل

Utiliza Tion of Surface Water by Red Mangrove (rhizophora Mangle L.): an Isotopic Study

Physiological responses of mangroves to salinity changes in the field are difficult to quantify, partly because it is still not clear whether mangroves utilize mostly surface water, as believed by many researchers based on the shallow distribution of mangrove roots in anaerobic soils. To test this axiom, we analyzed oxygen isotope ratios of possible water sources in different soil layers and st...

متن کامل

NOTE Biogeochemical implications of the isotopic equilibrium fractionation factor between the oxygen atoms of acetone and water

Carbonyl oxygens of organic molecules undergo isotopic exchange with water during reversible hydration reactions. The equilibrium isotopic fractionation factors between the carbonyl oxygen of acetone and water at 15”, 25”, and 35°C are 1.028, I .028, and 1.026 respectively. The differences between the 6’aO values of the carbonyl oxygen of acetone and of the water with which it is in equilibrium...

متن کامل

ذخیره در منابع من


  با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید

برای دانلود متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

ثبت نام

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

عنوان ژورنال:

دوره   شماره 

صفحات  -

تاریخ انتشار 2001