Difference between revisions of "RECENT PUBLICATIONS ON FORAMINIFERA"
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| + | ==BASAL FORAMINIFERA AND GROMIIDS AT THE HÅKON-MOSBY MUD VOLCANO (BARENTS SEA SLOPE)== | ||
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| + | We describe the occurrence of basal (‘primitive’) foraminifera and gromiids (a distinct taxon related to the foraminifera) in different bathyal habitats of the Håkon Mosby Mud Volcano (HMMV, Barents Sea). ...... The number of basal foraminiferal and gromiid morphospecies varied considerably from site to site. It was relatively high north of the volcano (42 morphospecies in 4 samples) and in the ‘warm centre’ (28 morphospecies in 2 samples), somewhat lower southwest of the volcano (at least 13 morphospecies in 2 samples) and in the siboglinid field (14 morphospecies in three samples), and substantially reduced in the bacterial mat area (5 morphospecies in 6 samples). ...... Saccamminid sp. 5, by far the most common species in our samples, belongs to a ‘lamp-like’ morphotype that is widely distributed in the oceans. The wall structure, and the presence of what appears to be an internal partition across the base of the neck, is reminiscent of some komokiaceans. | ||
| + | <font size="2">([http://link.springer.com/article/10.1007%2Fs12526-013-0148-5 ABSTRACT]) | ||
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| + | ----Gooday, A.J., Kamenskaya, O.E., Soltwedel, T., in press. [http://link.springer.com/article/10.1007%2Fs12526-013-0148-5 'Basal foraminifera and gromiids (Protista) at the Håkon-Mosby Mud Volcano (Barents Sea slope)]. Marine Biodiversity, doi:10.1007/s12526-013-0148-5 | ||
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==''Siphodinarella costata'', A NEW BENTHIC FORAMINIFER FROM THE CONIACIAN OF THE ADRIATIC CARBONATE PLATFORM== | ==''Siphodinarella costata'', A NEW BENTHIC FORAMINIFER FROM THE CONIACIAN OF THE ADRIATIC CARBONATE PLATFORM== | ||
