Abstract
The aim of the present study is to demonstrate the usefulness of stable carbon and nitrogen isotopes in bat guano as proxies for paleoclimate changes. We show a 2500-year record of environmental change in Romania using δ 13 C, δ 15 N, and (C:N) derived from precisely 14 C-dated bat guano cores recovered from Gaura cu Musca (GM), Zidita (ZC), and Magurici (MC) caves
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Schedule a callMore From: GEOREVIEW: Scientific Annals of Stefan cel Mare University of Suceava. Geography Series
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