By Ann Holbourn, Visit Amazon's Andrew S. Henderson Page, search results, Learn about Author Central, Andrew S. Henderson, , Norman Macleod
Deep-sea benthic foraminifera have performed a imperative position in biostratigraphic, paleoecological, and paleoceanographical study for over a century. those single–celled marine protists are very important as a result of their geographic ubiquity, contrast morphologies and fast evolutionary premiums, their abundance and variety deep–sea sediments, and due to their software as signs of environmental stipulations either at and less than the sediment–water interface. additionally, sturdy isotopic info bought from deep–sea benthic foraminiferal assessments supply paleoceanographers with environmental info that's proving to be of significant importance in experiences of worldwide climatic swap. This paintings collects jointly, for the 1st time, new morphological descriptions, taxonomic placements, stratigraphic prevalence info, geographical distribution summaries, and palaeoecological details, in addition to cutting-edge color photomicrographs (most taken in mirrored gentle, simply as you'll see them utilizing mild microscopy), of three hundred universal deep-sea benthic foraminifera species spanning the period from Jurassic - contemporary. This quantity is meant as a reference and learn source for post-graduate scholars in micropalaeontology, geological pros (stratigraphers, paleontologists, paleoecologists, palaeoceanographers), taxonomists, and evolutionary (paleo)biologists.
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Extra info for Atlas of Benthic Foraminifera
282, pl. 10, ﬁgs. 27–28. Type Specimen Depository not given. Lectotype from red clay outcropping in the right bank of the Wislok River at Kroscienko Nizne, designated and illustrated by Kaminski et al. (1993). Lectotype and syntypic material (No. UJ-132-P, 1/38) deposited in the Grzybowski Collection at the Jagiellonian University, Kraków, Poland. Type Level Uppermost Eocene; red and gray clay. Type Locality Not designated. Localities given: Hanover-Galicia Company wells nos 33 and 34, at Potok; Duniecki well no.
Biogeography Neritic to abyssal (2740 fathoms at “Challenger” Station 217A, off Papua New Guinea, Paciﬁc, Jones, 1994). , 1881, Notes on some of the reticularian Rhizopoda of the Challenger Expedition, Part III. Quarterly Journal of Microscopical Science (New Series), vol. 21, pp. 31–71. S. Challenger during the years 1873–1876. S. Challenger during the years 1873–1876. Zoology, vol. 9, pp. 1–814. , 1927, An outline of a re-classiﬁcation of the foraminifera. Contributions from the Cushman Laboratory for Foraminiferal Research, vol.
Ammodiscus pennyi. Lizard Springs well, near Guayaguayare, southeastern Trinidad, British West Indies, depth 720 feet. Collected by W. Jarvis. Deposited in the collections of the United States National Museum, Washington, DC; CC 9670. Holotype. Umbilical view, NHMUK PM DI 0030, scale bar = 230 μm. Original Designation Ammodiscus pennyi Cushman and Jarvis, 1928, p. 87, pl. 12, ﬁgs. 4–5. Type Specimen Holotype (CC 9670) deposited in the collections of the United States National Museum, Washington, DC.
Atlas of Benthic Foraminifera by Ann Holbourn, Visit Amazon's Andrew S. Henderson Page, search results, Learn about Author Central, Andrew S. Henderson, , Norman Macleod