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The Journal of Foraminiferal Research; October 2008; v. 38; no. 4; p. 337-356; DOI: 10.2113/gsjfr.38.4.337
© 2008 Cushman Foundation for Foraminiferal Research
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DOWNCORE DISTRIBUTION OF LIVING CALCAREOUS FORAMINIFERA AND STABLE ISOTOPES IN THE WESTERN BARENTS SEA

Elena V. Ivanova1,3, Ekaterina A. Ovsepyan1, Bjørg Risebrobakken2 and Alexander A. Vetrov1

1 Shirshov Institute of Oceanology RAS, 36 Nakhimovsky Prosp., 117997, Moscow, Russia.
2 Bjerknes Centre for Climate Research, Alle'gaten 55, 5007 Bergen, Norway.

3 Correspondence author. E-mail: e_v_ivanova{at}ocean.ru and e_v_ivanova{at}mail.ru

The density and vertical distribution of living calcareous foraminifera have been studied in six box cores from the shelf depressions in the Western Barents Sea in relation to total organic carbon content and flux to the seafloor, primary production, sedimentation rates, bottom-water masses and stable isotopes. It appears that at least several infaunal species—like Melonis barleeanus, Islandiella norcrossi and perhaps Nonionellina labradorica, Cribroelphidium excavatum clavatum and Cassidulina reniforme—might penetrate down to 8–10 cm below the sediment surface searching for a favorable microhabitat. A deep penetration of some living specimens, notably epifaunal Cibicides lobatulus, into the sediment might result from bioturbation and survival inside polychaete tubes. The highest foraminiferal abundances (up to 130–240 sp/50 cm3) of the six cores were found in the most productive areas on the West Spitsbergen shelf and in the mouth of the Isfjorden (Svalbard) and likely resulted from fast sedimentation and mass accumulation rates of marine organic matter. These factors seemed to be responsible for deeper penetration and habitat depth of the above-mentioned species on the shelf as compared to the northern Barents Sea continental slope. However, the abundance of living calcareous foraminifera on the slope was much higher than in our study, probably due to a greater flux of particulate organic matter produced during the seasonal phytoplankton bloom along the ice-edge margin. In general, more depleted {delta}18O values (of unstained foraminifera) are found in the box cores obtained beneath pure Atlantic water compared to those beneath cooler bottom water. Estimated {delta}18O disequilibrium effects for Nonionellina labradorica (0.28{per thousand}), Cibicides lobatulus (–0.76{per thousand}) and Melonis barleeanus (–0.41{per thousand}) support previous findings for these species.







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