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 important 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 charges, their abundance and variety deep–sea sediments, and thanks to their software as signs of environmental stipulations either at and lower than the sediment–water interface. furthermore, solid isotopic information got from deep–sea benthic foraminiferal checks offer paleoceanographers with environmental info that's proving to be of significant value in reviews of worldwide climatic swap. This paintings collects jointly, for the 1st time, new morphological descriptions, taxonomic placements, stratigraphic prevalence facts, geographical distribution summaries, and palaeoecological info, besides cutting-edge color photomicrographs (most taken in mirrored gentle, simply as you will 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 examine source for post-graduate scholars in micropalaeontology, geological execs (stratigraphers, paleontologists, paleoecologists, palaeoceanographers), taxonomists, and evolutionary (paleo)biologists.
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Extra resources for Atlas of Benthic Foraminifera
Glomospirella biedai Samuel, 1977, p. 29, pl. 3, ﬁg. 16; pl. 21, ﬁg. 3. Glomospirella grzybowskii (Jurkiewicz). –Hemleben and Tröster, 1984, p. 519, pl. 1, ﬁg. 24. –Charnock and Jones, 1990, p. 157, pl. 2, ﬁg. 13; pl. 14, ﬁg. 10. –Bubik, 1995, p. 81, pl. 12. Annectina grzybowskii (Jurkiewicz). –Kaminski and Gradstein, 2005, pp. 192–195, ﬁg. 28, pl. 28. Type Specimen Depository not given. The Jurkiewicz Collection was originally deposited at the Polish Petroleum Company in Jaslo but the status of the holotype is unknown (Kaminski and Gradstein, 2005).
Loeblich and Tappan, 1987, p. 49, pl. 36, ﬁg. 16. –Zheng, 1988, p. 39, pl. 6, ﬁg. 6. , 1990, p. 365, pl. 3, ﬁg. 1. –Charnock and Jones, 1990, p. 155, pl. 2, ﬁg. 8; pl. 14, ﬁg. 6. –Jones, 1994, p. 46, pl. 41, ﬁgs. 12–16. –Loeblich and Tappan, 1994, p. 14, pl. 4, ﬁgs. 1–4. –Holbourn and Kaminski, 1997, p. 36, pl. 5, ﬁg. 6. –Kaminski and Gradstein, 2005, pp. 165–168, ﬁg. 21, pl. 21. –Milker and Schmiedl, 2012, p. 28, ﬁg. 5. Remarks Type species of the genus Ammolagena Eimer and Fickert, 1899. Test is often found attached to shell fragments or to other foraminiferal tests.
Special Publications of the Cushman Laboratory for Foraminiferal Research, vol. 24, pp. 1–42. Geroch, S. , 1984, Proposal of zonation for the late Tithonian–late Eocene, based upon arenaceous foraminifera from the outer Carpathians, Poland. , Benthos ’83, 2nd International Symposium on Benthic Foraminifera, Pau (France), April 11–15, 1983. Elf Aquitaine, ESSO REP and TOTAL CFP, Pau et Bordeaux, pp. 225–239. , 1994, Cenozoic biostratigraphy of the Central North Sea and Labrador Shelf. Micropaleontology, vol.