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11 p, 587.7 KB Latitudinal variation of planktonic foraminifera shell masses during Termination I / Zarkogiannis, Stergios (Panepistēmio Athēnōn. Department of Historical Geology and Paleontology) ; Kontakiotis, George (Panepistēmio Athēnōn. Department of Historical Geology and Paleontology) ; Antonarakou, Assimina (Panepistēmio Athēnōn. Department of Historical Geology and Paleontology) ; Mortyn, Peter Graham (Universitat Autònoma de Barcelona. Institut de Ciència i Tecnologia Ambiental) ; Drinia, Hara (Panepistēmio Athēnōn. Department of Historical Geology and Paleontology)
The oceans' surface layer holds large amounts of dissolved inorganic carbon that is exchanged rapidly with the atmosphere. Carbon enters the ocean mainly through the dissolution of atmospheric carbon dioxide (CO2), and a part of it is converted into carbonate by marine organisms. [...]
2019 - 10.1088/1755-1315/221/1/012052
IOP conference series. Earth and environmental science, Vol. 221 (2019) , art. 012052  

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