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ABSTRACT SUPPLIED BY ORIGINATOR: The volcanogenic lake Laguna Potrok Aike, Santa Cruz, Argentina, reveals an unprecedented continuous high resolution climatic record for the steppe regions of southern Patagonia. With the applied multi-proxy approach rapid climatic changes before the turn of the first millennium were detected followed by medieval droughts which are intersected by moist and/or cold periods of varying durations and intensities. The &apos;total inorganic carbon&apos; content was identified as a sensitive lake level indicator. This proxy suggests that during the late Middle Ages (ca. AD 1230-1410) the lake level was rather low representing a signal of the &apos;Medieval Climate Anomaly&apos; in southeastern Patagonia. At the beginning of the &apos;Little Ice Age&apos; the lake level rose considerably staying on a high level during the whole period. Subsequently, the lake level lowered again in the course of the 20th century.</gco:CharacterString>
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