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Organic Geochemical Reconstruction of Palaeo-Environmental Conditions During The Deposition of Pliocene Sapropels in The Eastern Mediterranean Sea
The Mediterranean is a region of transition between the sub-oceanic, cool temperate zone of Europe, and the high-pressure, aird subtropics of North Africa straddling the pressure systems of the Atlantic and the monsoon climates of the Indian subcontinent and East Africa.
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