Problems of stable isotopes in tree-rings, lake sediments and peat-bogs as climatic evidence for the Holocene
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Beschreibung
Contents:
Stable isotopes in lake sediments: The "catchment effect" on the isotopic composition of lake waters: its importance in palaeolimnological interpretations - Temperature-dependent carbon-isotope fractionation of organic matter: a potential palaeoclimatic indicator in Holocene lacustrine wequences - Stable oxygen and carbon isotope analyses on lacustrine carbonate sediments - The stable isotope composition of the Holocene deposits from East European interior seas and its interpretation - Stable isotopes in bones: Stable isotope ratios in phosphate from mammal bone and tooth as climatic indicators - Factors determining stable isotope ratios in plants: Parameters determining carbon isotope ratios in plants - Isotopes in tree-rings and other plants as palaeoclimatic indicators: Using d13C in tree-rings as a bio-indicator of environmental variations and ecophysiological changes in tree functioning - Indirect effects of winter climate on the d13C and dD characteristics of annual growth segments in the long-lived, arctic plant Cassiope tetragona: a preliminary analysis - Stable carbon isotopes in tree-rings of a Scots pine from northern Finland - Stable isotope studies in tree-rings from oeak-techniques and some preliminary results - Isotope coherence in oak cellulose - Biological considerations in the interpretation of stable isotope ratios in oak tree-rings - Stable isotopes in tree-rings: a palaeoclimatic tool for studying climatic changes - Climatic control of stable isotopes in precipitation as a basis for palaeoclimatic reconstructions
Die Beiträge dieses Bandes befassen sich mit stabilen Isotopen als paläoklimatischen Indikatoren für das Holozän.
Autor*in
Burkhard Frenzel
Themen in »Problems of stable isotopes in tree-rings, lake sediments and peat-bogs as climatic evidence for the Holocene«
Holozän Klimaschwankung Paläoklimatologie