TY - JOUR
T1 - The Kallisti Limnes, carbon dioxide-accumulating subsea pools
AU - Camilli, Richard
AU - Nomikou, Paraskevi
AU - Escartín, Javier
AU - Ridao, Pere
AU - Mallios, Angelos
AU - Kilias, Stephanos P.
AU - Argyraki, Ariadne
AU - Andreani, Muriel
AU - Ballu, Valerie
AU - Campos, Ricard
AU - Deplus, Christine
AU - Gabsi, Taoufic
AU - Garcia, Rafael
AU - Gracias, Nuno
AU - Hurtós, Natàlia
AU - Magí, Lluis
AU - Mével, Catherine
AU - Moreira, Manuel
AU - Palomeras, Narcís
AU - Pot, Olivier
AU - Ribas, David
AU - Ruzié, Lorraine
AU - Ruzie, Lorraine
AU - Sakellariou, Dimitris
PY - 2015
Y1 - 2015
N2 - Natural CO2 releases from shallow marine hydrothermal vents are assumed to mix into the water column, and not accumulate into stratified seafloor pools. We present newly discovered shallow subsea pools located within the Santorini volcanic caldera of the Southern Aegean Sea, Greece, that accumulate CO2 emissions from geologic reservoirs. This type of hydrothermal seafloor pool, containing highly concentrated CO2, provides direct evidence of shallow benthic CO2 accumulations originating from sub-seafloor releases. Samples taken from within these acidic pools are devoid of calcifying organisms, and channel structures among the pools indicate gravity driven flow, suggesting that seafloor release of CO2 at this site may preferentially impact benthic ecosystems. These naturally occurring seafloor pools may provide a diagnostic indicator of incipient volcanic activity and can serve as an analog for studying CO2 leakage and benthic accumulations from subsea carbon capture and storage sites.
AB - Natural CO2 releases from shallow marine hydrothermal vents are assumed to mix into the water column, and not accumulate into stratified seafloor pools. We present newly discovered shallow subsea pools located within the Santorini volcanic caldera of the Southern Aegean Sea, Greece, that accumulate CO2 emissions from geologic reservoirs. This type of hydrothermal seafloor pool, containing highly concentrated CO2, provides direct evidence of shallow benthic CO2 accumulations originating from sub-seafloor releases. Samples taken from within these acidic pools are devoid of calcifying organisms, and channel structures among the pools indicate gravity driven flow, suggesting that seafloor release of CO2 at this site may preferentially impact benthic ecosystems. These naturally occurring seafloor pools may provide a diagnostic indicator of incipient volcanic activity and can serve as an analog for studying CO2 leakage and benthic accumulations from subsea carbon capture and storage sites.
U2 - 10.1038/srep12152
DO - 10.1038/srep12152
M3 - Article
SN - 2045-2322
VL - 5
JO - uk-ac-man-jrn:706477
JF - uk-ac-man-jrn:706477
ER -