When Black Sea waters reshaped Eastern Mediterranean circulation 11,000 years ago Title * Field is limited to 255 characters. Media * Max File Size: 100 MB Allowed Extensions: jpeg, jpg, jpe, gif, png Caption * License * (IMAGE)
Caption
Marine sediment core scanned using an Avaatech X-ray fluorescence (XRF) core scanner at the CORELAB, Universitat de Barcelona (Spain) to obtain high-resolution geochemical records. The dark sedimentary unit visible in the upper part of the core corresponds to the organic-rich sapropel S1 layer, which is characterized by elevated organic matter content relative to the surrounding sediments.
Credit
UNIVERSITY OF BARCELONA
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CC BY