2 edition of Pliocene benthic foraminifera from the Ontong-Java Plateau (western equatorial Pacific Ocean) found in the catalog.
Pliocene benthic foraminifera from the Ontong-Java Plateau (western equatorial Pacific Ocean)
J. Otto R. Hermelin
|Statement||J. Otto R. Hermelin.|
|Series||Special publication ;, no. 26, Special publication (Cushman Foundation for Foraminiferal Research) ;, no. 26.|
|LC Classifications||QE772 .H44 1989|
|The Physical Object|
|Pagination||143 p. :|
|Number of Pages||143|
|LC Control Number||90105556|
Full text of "Biostratigraphic And Geological Significance Of Planktonic Foraminifera Second Edition" See other formats. The Ontong Java Plateau (OJP) is the world's largest oceanic plateau and is presently the best and ideal place to do geochemical, geophysical, and geochronological investigations.
During the last deglaciation period, climate changes in the northern and southern high-latitude regions show a pattern of so-called “bipolar seesaw” on millennial scale. Previous research interpreted that the weakening of the Atlantic Meridional Overturning Circulation (AMOC) and the associated north-south migration of the Intertropical Convergence Zone (ITCZ) influenced the. Planktonic foraminifera Foraminifera are separated into two types following their life strategy, namely, the benthic and the planktonic foraminifera. The benthic forms occur at all depths in.
Benthic foraminifera in Pliocene samples indicate depths similar to water depths from which they were dredged, suggesting uplift, probably beginning in M Miocene and culminating in Pliocene) Fujita, K. & S. Kato ()- Distribution of gravel-sized empty tests of large benthic foraminifers as practical depositional indicators in tropical reef. The cause of this event was the eruption of the Ontong Java Plateau in the western Pacific, wich led to a major increase in atmospheric pCO2 and ocean acidification. This event was characterized by the occurrence of organic-carbon-rich sediments on a global basis along with evidence for warming and dramatic change in nanoplankton assemblages.
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Get this from a library. Pliocene benthic foraminifera from the Ontong-Java Plateau (western equatorial Pacific Ocean): faunal response to changing paleoenvironment. [J Otto R Hermelin]. KOHL Kohl, B., Early Pliocene benthic foraminifera from the Salina Basin, southeastern Mexico.
in Bulletins of American Paleontology, Volume. 88, Number KRIS Kristan-Tollmann, E., Die Foraminiferen aus den rhätischen Zlambachmergeln der Fischerwiese bei. PLIOCENE-PLEISTOCENE CARBON ISOTOPE RECORD, SITEONTONG JAVA PLATEAU1 Jill M. Whitman2,3 and Wolf H.
Berger2 ABSTRACT Oceanographic changes in the western equatorial Pacific during the past 6 m.y. are inferred from carbon isotopic analyses of planktonic and benthic foraminifers from Ontong Java Plateau (DSDP Site ).File Size: 4MB.
Pliocene-Pleistocene oxygen isotope record SiteOntong Java Plateau. Mar. Micropal., Oceanographic changes in the western equatorial Pacific during the past 6 Ma are inferred from oxygen isotopic analyses of planktic and benthic foraminifera from Ontong Java Plateau (DSDP Site ).Cited by: 9.
oligocene planktonic foraminifer biostratigraphy of hole d (ontong java plateau) and hole a (little bahama bank), and comparison with the southern high latitudes 1.
Biostratigraphy and assemblage composition of benthic foraminifera from the Manihiki Center for Marine Geosciences, WischhofstrasseD Kiel, Germany ABSTRACT - Pleistocene and late Pliocene benthic foraminifera from the Manihiki Plateau semblages from the Ontong Java Plateau (Burke et al., Epistominella spp Cited by: The present paper deals with the isotopic signals in the benthic foraminifera from two such cores (ERDC Bx, ERDC Bx), taken on Ontong--Java Plateau.
The aim is, ultimately, to reconstruct the recent history of abyssal circulation in this area, from the information contained in the benthic assem- by: Late Quaternary Stable Isotope Record of Benthic Foraminifers: Sites andOntong Java Plateau Article (PDF Available) April with Reads How we measure 'reads'.
The LR04 benthic δ 18 O stack constructed by the graphic correlation of 57 globally distributed benthic δ 18 O records. The stack is plotted using the LR04 age model described in section 5 and with new MIS labels for the early Pliocene (section ). Note that the scale of the vertical axis changes across panels.
The present work is based on agglutinated benthic foraminifera from the two ODP sites (Table 1) B (Lat. 19 0 ' S, Long. 0 ' E W ater depth m) and A (Lat. 20 0 ' S, Long. SITEONTONG JAVA PLATEAU1 H. Schmidt,2 W.H. Berger,3 T. Bickert,2 and G. Wefer2 ABSTRACT We present δ13C records spanning the last 2 m.y.
of two planktonic foraminiferal taxa (Globigerinoides sacculifer and Pulleniatiná) from Ocean Drilling Program Site on the Ontong Java Plateau, western equatorial Pacific. The sampling interval. The use of the calcium carbonate-water isotope paleothermometer has been reviewed many times since the technique was proposed by Urey () and developed and applied by Epstein et al.
() and Urey et al. Critical reviews and discussions of various aspects of the method include those by Craig (), Bowen (), Teis and Naidin (), Savin and Stehli (), Hecht (), Hudson. Hermelin O () Pliocene benthic Foraminifera from the ontong-java plateau (Western equatorial Pacific Ocean): faunal response to chaining paleoenviromental.
Cushman Found Foram Res – Google ScholarAuthor: Angélica Ballesteros-Prada. Pliocene-Holocene benthic foraminiferal assemblages and water mass history, ODP B, western Equatorial Pacific biogeography Cenozoic Buliminacea Foraminifera Holocene Invertebrata Leg Ontong Java Plateau microfossils Neogene Ocean Drilling Program ODP Site Pleistocene Pliocene Rotaliina Pacific Ocean paleoecology Quaternary Cited by: 6.
Hermelin, O. () Pliocene benthic foraminifera from the Ontong Java Plateau (Western Equatorial Pacific Ocean): foraminiferal response to changing paleoenvironment, Special Publications of the Cushman Foundation for Foraminiferal Research, 26, 1– Google ScholarCited by: Pliocene benthic foraminifera from the Ontong-Java Plateau (western equatorial Pacific Ocean): faunal response to changing paleoenvironments Journal of Foraminiferal Research Title: Senior Lecturer / Director of.
dle Eocene Discoaster assemblage (Haq et al., ) as representing low- rather than middle-latitude climate. Our interpretation is in accord with the isotopic record from the Deep Sea Drilling Project (DSDP) site (Vergnaud-Grazzini, ); data on the early Paleocene climate is also based largely on somewhat meager isotopic records.
This is the first benthic delta18O stack composed of more than three records to extend beyond ka, and we use its improved signal quality to identify 24.
TI‑ Stable isotopes in benthic foraminifera from Ontong‑Java Plateau, Box Cores ERDC‑ and ERDC‑ JN‑ Palaeogeography Palaeoclimatology Palaeoecology PY‑ VO‑ 33 NO‑ 1‑3 PG‑ ‑ AU‑ VISMARA SCHILLING, A; PARISI, E.
TI‑ Coiling patterns in four benthic foraminiferal species through the terminal Miocene and Pliocene in the Caribbean Sea JN‑ Journal of Foraminiferal Research PY‑ VO‑ 23 NO‑ 2 PG‑ ‑ AU‑ BOUDCHICHE, L; RUGET, C.
Ontong Java Plateau (1) Santa Marine conditions were restricted in the Pliocene as the Colorado River filled the Salton Trough with sediments and the Gulf of California assumed its present configuration.
Microfossils from the early part of this incursion include a diverse assemblage of benthic foraminifers (Amphistegina gibbosa, Uvigerina.Oligocene planktonic foraminiferal biostratigraphy of Hole D (Ontong Java Plateau) and Hole A (Little Bahama Bank), and comparison with the southern high latitudes.
In Berger W., Kroenke, Mayer, L.A., et al., Proceedings of the Ocean Drilling Program, Scientific Results, Vol. College Station, TX (Ocean Drilling Program), The use of tests produced by benthic foraminifera for Mg/Ca thermometry is inherently difficult because, except in very shallow water (e.g.
as in coral reef environments—see for example Raja et al. ), bottom water is cold, which means that the uptake of magnesium by the foraminifera is relatively small.
Furthermore during climate changes.