Oxygen isotope ratios of chironomids, aquatic macrophytes and ostracods for lake-water isotopic reconstructions - Results of a calibration study in Patagonia

Oxygen stable isotopes (δ18O) of biogenic sedimentary components from lake sediment archives, such as ostracod valves, are frequently used for palaeoclimatic reconstructions. However, the effects of host water isotope changes, temperature-dependent fractionations, and vital effects on the isotopic r...

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Detalles Bibliográficos
Autores principales:	Mayr, C., Laprida, C., Lücke, A., Martín, R.S., Massaferro, J., Ramón-Mercau, J., Wissel, H.
Formato:	JOUR
Materias:	18O/16O ratios Climate proxies Isotope fractionation Lacustrine systems Stable isotopes Water temperature Animals Cellulose Fractionation Lakes Oxygen Repair Water temperatures Isotopes aquatic organism biochemical composition biogenic deposit calcite calibration cellulose dicotyledon fly isotopic fractionation lacustrine deposit larva macrophyte moss ostracod oxygen isotope ratio paleoclimate proxy climate record reconstruction seasonality stable isotope stream subfossil water temperature Patagonia Bryophyta Chironomidae Myriophyllum Ostracoda
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_00221694_v529_nP2_p600_Mayr
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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