Large glaciers and ice caps formed in the Mediterranean mountains during the cold stages
of the Pleistocene and some small glaciers remain today. Here we review 157 outputs that …

One of the most important problems in glacial geomorphology is the disagreement regarding
the dates of glacial advances. During the Last Glacial Maximum (LGM,~ 29 to 19 ka), the …

Studies of the upper 447 m of the DEEP site sediment succession from central Lake Ohrid,
Balkan Peninsula, North Macedonia and Albania provided important insights into the …

Abstract The Chornohora and Svydovets massifs represent the highest part of the Ukrainian
Carpathians (2061 m asl) and the north-eastmost mountain area in Europe, which was …

The element mercury (Hg) is a key pollutant, and much insight has been gained by studying
the present-day Hg cycle. However, many important processes within this cycle operate on …

The O 2: CO 2 exchange ratio (ER) between terrestrial ecosystems and the atmosphere is a
key parameter for partitioning global ocean and land carbon fluxes. The long-term terrestrial …

Koločep bay is a 30 km elongated karst basin located between the Elafiti Islands and the
mainland with a NW–SE general direction. The bay lies within the seismically active …

The studied dataset from the Southern Carpathians permitted the quantification of a
considerable amount of inherited 10 Be in the glacial boulders and bedrock samples in the …

Abstract The Eastern Carpathians are the northeasternmost sector of the European Alpine
Mountain system and comprise 14 formerly glaciated massifs that stretch over 300 km into …

Abstract In the Northern Romanian Carpathians (NRC) small Pleistocene cirque glaciers
have formed in several isolated mountain massifs exceeding 1800 m asl. This paper brings …