Taphonomic and early diagenetic effects on the C and N stable isotope composition of cladoceran remains: implications for paleoecological studies |
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Authors: | Marie-Elodie Perga |
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Institution: | (1) National Institute for Agronomical Research (INRA), Alpine Centre for Research on Lake Ecosystems and Food Webs (CARRTEL), 75 Avenue de Corzent, BP 511, 74203 Thonon les Bains Cedex, France |
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Abstract: | I addressed the effects of taphonomic and early diagenetic processes on the isotope composition of cladoceran remains, using
both experimental and field approaches. An experiment was designed to mimic the conditions encountered by cladoceran remains
when they settle through the water column and are buried in the sediment. Cladoceran exoskeletons were incubated for 4 months
in oxic or anoxic water, and in sediment. Changes in their carbon (C) and nitrogen (N) content and isotope compositions were
measured. Most changes in isotope composition of exoskeletons took place when they settled through the water column. Once
buried in the sediment, however, the δ13C and δ15N values of cladoceran exoskeletons did not undergo further change. Taphonomic processes resulted in an increase in δ13C and δ15N of the cladoceran remains and this was related to microbial degradation, which selectively removed isotopically light C
and N compounds from the remains. For δ13C, changes were minimal (<1‰) and occured within the first 3 months. Taphonomic effects on δ15N were larger, from +2 to +5‰, and occurred within the first 2–3 weeks. These effects depended on incubation conditions and
were greater in anoxic waters than under oxic conditions. Monthly changes in the isotope composition of sedimenting cladoceran
exoskeletons were also recorded in the field using sediment traps, and were compared to the isotope composition of the living
cladoceran community. The isotope composition of sedimenting remains displayed values consistent with those that might be
expected, considering the effects of taphonomic processes observed in the experiment. Because C and N in cladoceran exoskeletons
might involve a different isotope routing, the δ15N value of the remains provides an annual record of the value in the parent community, with a 1-month delay, while δ13C of remains essentially reflects that of the parent community during the period of lake thermal stratification. These findings
provide insights into paleolimnological interpretation of isotopic changes in cladoceran remains from sediment cores. |
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