Untersuchungen stabiler ( leichter ) Isotope stehen im Mittelpunkt der Arbeiten zur Paläoumweltrekonstruktion.
C und O Isotopenverhältnisse ermöglichen Rückschlüsse zur Klimaentwicklung im Phanerozoikum sowie zur Vereisungsgeschichte.
www.gzn.uni-erlangen.deCarbon, oxygen and nitrogen isotopes are used to reconstruct the palaeoenvironment in the geological past.
Carbon and oxygen isotopes enable to record palaeoclimatic changers as well as to reconstruct the ice volume history of major glaciations in Earth History.
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