Taxonomic notes on the abyssal agglutinated benthic foraminifera of the HEBBLE area (lower Nova Scotian Continental Rise)
Kaminski, Michael A.
MetadataShow full item record
Eighty species and morphological varieties of agglutinated benthic foraminifera were identified in sediments from the HEBBLE Site (4800 m depth) and the HEBBLE Shallow Site (4185 m) on the lower Nova Scotian Continental Rise. Details of their morphology and classification are included in descriptions of each species, and representative specimens are illustrated using SEM, light microscopy, and X-radiography.
Suggested CitationTechnical Report: Kaminski, Michael A., "Taxonomic notes on the abyssal agglutinated benthic foraminifera of the HEBBLE area (lower Nova Scotian Continental Rise)", 1983-09, DOI:10.1575/1912/8904, https://hdl.handle.net/1912/8904
Showing items related by title, author, creator and subject.
Last deglaciation in the Okinawa Trough : subtropical northwest Pacific link to Northern Hemisphere and tropical climate Sun, Youbin; Oppo, Delia W.; Xiang, Rong; Liu, Weiguo; Gao, Shu (American Geophysical Union, 2005-06-23)Detailed deglacial and Holocene records of planktonic δ18O and Mg/Ca–based sea surface temperature (SST) from the Okinawa Trough suggest that at ∼18 to 17 thousand years before present (kyr B.P.), late spring/early summer ...
Combined carbonate carbon isotopic and cellular ultrastructural studies of individual benthic foraminifera : method description Martin, Jonathan B.; Bernhard, Joan M.; Curtis, Jason H.; Rathburn, Anthony E. (American Geophysical Union, 2010-06-11)Carbon isotopes of foraminiferal tests provide a widely used proxy for past oceanographic environmental conditions. This proxy can be calibrated using live specimens, which are reliably identified with observations of cell ...
Active eukaryotes in microbialites from Highborne Cay, Bahamas, and Hamelin Pool (Shark Bay), Australia Edgcomb, Virginia P.; Bernhard, Joan M.; Summons, Roger E.; Orsi, William D.; Beaudoin, David J.; Visscher, Pieter T. (2013-06-26)Microbialites are organosedimentary structures that are formed through the interaction of benthic microbial communities and sediments and include mineral precipitation. These lithifying microbial mat structures include ...