Pregled bibliografske jedinice broj: 371140
Deep water ventilation traced by Synechococcus cyanobacteria
Deep water ventilation traced by Synechococcus cyanobacteria // Workshop Recent advances in Adriatic oceanography and marine meteorology : Book of abstracts / Orlić, Mirko ; Pasarić, Miroslava (ur.).
Zagreb: Geofizički odsjek Prirodoslovno-matematičkog fakulteta Sveučilišta u Zagrebu, 2008. str. 58-58 (predavanje, nije recenziran, sažetak, znanstveni)
CROSBI ID: 371140 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Deep water ventilation traced by Synechococcus cyanobacteria
Autori
Vilibić, Ivica ; Šantić, Danijela
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
Workshop Recent advances in Adriatic oceanography and marine meteorology : Book of abstracts
/ Orlić, Mirko ; Pasarić, Miroslava - Zagreb : Geofizički odsjek Prirodoslovno-matematičkog fakulteta Sveučilišta u Zagrebu, 2008, 58-58
ISBN
978-953-6076-18-5
Skup
Recent advances in Adriatic oceanography and marine meteorology
Mjesto i datum
Dubrovnik, Hrvatska, 05.11.2008. - 07.11.2008
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Nije recenziran
Ključne riječi
deep water masses; biological tracer; Adriatic Sea
Sažetak
Adriatic waters during the spring of 2006. The maximum abundance in early May was positioned at 800 m, being of order of the values referred for the surface waters in the Adriatic Sea. Both open-ocean convection (South Adriatic deep water generation) and shallow water intense cooling (North Adriatic dense water generation) were supposed to occur in winter of 2006 in the South Adriatic Pit and broad Northern Adriatic shelf, respectively. By using CTD, satellite and Synechoccocus abundance data during preconditioning and post-generation phases, these processes were successfully detected, explained and put in the context of the respective literature. The first process was responsible for bringing the cyanobacteria down to 600 m depth in the area of convection, and the second one triggered the downslope transport of the cyanobacteria to the very bottom of South Adriatic Pit. Also, the nature of the deep-convection process in the Adriatic, which lasts usually for a couple of days, enabled the estimation of Synechococcus loss rate characteristic time in the extremely hostile environment (no solar radiation), which is estimated to be of the order of one month. Last but not least, another important implication of this study is the persistence of phytoplankton at great depths and its relevance for the biogeochemical cycle.
Izvorni jezik
Engleski
Znanstvena područja
Biologija
POVEZANOST RADA
Projekti:
001-0013077-0845 - Uloga planktonskih zajednica u protoku energije i kruženju tvari u Jadranu (Krstulović, Nada, MZOS ) ( CroRIS)
001-0013077-1122 - Istraživanje i sustavi praćenja neuobičajene dinamike Jadrana (Vilibić, Ivica, MZOS ) ( CroRIS)
Ustanove:
Institut za oceanografiju i ribarstvo, Split