Upper Cretaceous foraminifera and palynomorphs from Ekelöf coast Section, Ekelöf Point, Eastern James Ross Island, Antarctic Peninsula
A micropaleontological analysis of foraminifera and palynomorphs obtained from a partial sedimentary section cropping out at Ekelöf Point, eastern James Ross Island, Antarctic Peninsula, is presented. The section, named Ekelöf Coast, includes the lowest levels of the Upper Cretaceous Hamilton Point...
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Asociacion Paleontologica Argentina
2016
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| LEADER | 28389caa a22019937a 4500 | ||
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| 001 | PAPER-15951 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230607131905.0 | ||
| 008 | 190411s2016 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-84975252033 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Caramés, A. | |
| 245 | 1 | 0 | |a Upper Cretaceous foraminifera and palynomorphs from Ekelöf coast Section, Ekelöf Point, Eastern James Ross Island, Antarctic Peninsula |
| 260 | |b Asociacion Paleontologica Argentina |c 2016 | ||
| 506 | |2 openaire |e Política editorial | ||
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| 504 | |a Van Der Akker, T., Kaminski, M.A., Gradstein, F.M., Wood, J., Campanian to paleocene biostratigraphy and palaeoenvironments in the foula sub-basin, West of the shetland island, UK (2000) Journal of Micropaleontology, 19, pp. 23-43 | ||
| 504 | |a Versteegh, G.J.M., Recognition of cyclic and non-cyclic environmental changes in the mediterranean pliocene: A palynological approach (1994) Marine Micropaleontology, 23, pp. 147-183 | ||
| 504 | |a Walker, G., Boys, W., (1784) Testacea Minuta Rariora, Nuperrime Detecta in Arena Littoris Sandvicensis. J, pp. 1-25. , March, London | ||
| 504 | |a Wedekind, P.R., (1937) Einführung in die Grundlagen der Historischen Geologie. Band II. Mikrobiostratigraphie die Korallen- und Foraminiferenzeit, 136p. , Ferdinand Enke, Stuttgart | ||
| 504 | |a Williams, G.L., Brinkhuis, H., Pearce, M.A., Fensome, R.A., Weegink, J.W., Southern ocean and global dinoflagellate cyst events compared: Index events for the late cretaceous-neogene (2004) Proceedings of the Ocean Drilling Program, Scientific Results, 189, pp. 1-98. , N.F. Exon, J.P. Kennett, and M.J. Malone (Eds.) | ||
| 504 | |a Wood, S.A., Askin, R.A., Dinoflagellate cysts from the marambio group (Upper cretaceous) of humps island (1992) Antarctic Science, 4, pp. 327-336 | ||
| 504 | |a Wood, G.D., Gabriel, A.M., Lawson, J.C., Chapter 3: Palynological techniques - Processing and microscopy (1996) Palynology: Principles and Applications, 1, pp. 29-50. , J. Jansonius, and D.C. McGregor (Eds.) American Association of Stratigraphic Palynologists, Dallas | ||
| 520 | 3 | |a A micropaleontological analysis of foraminifera and palynomorphs obtained from a partial sedimentary section cropping out at Ekelöf Point, eastern James Ross Island, Antarctic Peninsula, is presented. The section, named Ekelöf Coast, includes the lowest levels of the Upper Cretaceous Hamilton Point Member of the Snow Hill Island Formation. Among the foraminifera, 18 benthictaxa including 10 agglutinated and eight calcareous are recognized. Palynomorphs include continental and marine species. The continental assemblage contains 44 spore and pollen species. The marine assemblage consists of 10 peridinioid dinoflagellate cysts species, dominating in number of specimens, and 10 gonyaulacoids. Although the palynomorph assemblage supports a late Campanian age for the section, an earliest Maastrichtian age is not excluded. The paleoenvironmental interpretation based on the distribution of foraminiferal morphogroups indicates an outer shelf-upper bathyal environment in agreement with sedimentological data. The paleoenvironmental inference based on the S/D ratio (sporomorph versus din of lagellate cysts) and the P/G ratio (pendinioid versus gonyaulacoid cysts) suggest a coastal to inner neritic setting with a continuous continental supply from the continent to the marine environment, evidenced by the slight dominance of the peridionoids over gonyaulacoids cysts. The discrepancy observed between palynological and micropaleontological-sedimentological data may be linked to the development of a narrow continental shelf during the Late Cretaceous. In such continental shelf, terrestrial palynomorphs and peridinoid cysts would quickly run down the slope and would be deposited in the deep marine environment together with gonyaulacoid cysts. |l eng | |
| 593 | |a Institute de Estudios Andinos Don Pablo Groeber, Universidad de Buenos Aires, CONICET, Departamento de Ciencias Geológicas, Ciudad Universitaria, Intendente Guiraldes 2160, Buenos Aires, C1428EGA, Argentina | ||
| 593 | |a Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Buenos Aires, Argentina | ||
| 593 | |a Instituto Antártico Argentino, 25 de Mayo 1151, 3er piso, San-Martín, Provincia de Buenos Aires, 1650, Argentina | ||
| 690 | 1 | 0 | |a ANTARCTIC PENINSULA |
| 690 | 1 | 0 | |a FORAMINIFERA |
| 690 | 1 | 0 | |a JAMES ROSS ISLAND |
| 690 | 1 | 0 | |a PALYNOMORPHS |
| 690 | 1 | 0 | |a UPPER CRETACEOUS |
| 690 | 1 | 0 | |a CAMPANIAN |
| 690 | 1 | 0 | |a COASTAL SEDIMENT |
| 690 | 1 | 0 | |a CONTINENTAL SHELF |
| 690 | 1 | 0 | |a CRETACEOUS |
| 690 | 1 | 0 | |a DINOFLAGELLATE CYST |
| 690 | 1 | 0 | |a FORAMINIFERA |
| 690 | 1 | 0 | |a MAASTRICHTIAN |
| 690 | 1 | 0 | |a MARINE ENVIRONMENT |
| 690 | 1 | 0 | |a MICROPALEONTOLOGY |
| 690 | 1 | 0 | |a PALEOECOLOGY |
| 690 | 1 | 0 | |a PALEOENVIRONMENT |
| 690 | 1 | 0 | |a PALYNOMORPH |
| 690 | 1 | 0 | |a POLLEN |
| 690 | 1 | 0 | |a ANTARCTIC PENINSULA |
| 690 | 1 | 0 | |a ANTARCTICA |
| 690 | 1 | 0 | |a JAMES ROSS ISLAND |
| 690 | 1 | 0 | |a SNOW HILL ISLAND |
| 690 | 1 | 0 | |a WEST ANTARCTICA |
| 690 | 1 | 0 | |a DINOPHYCEAE |
| 690 | 1 | 0 | |a FORAMINIFERA |
| 700 | 1 | |a Amenábar, C.R. | |
| 700 | 1 | |a Concheyro, A. | |
| 773 | 0 | |d Asociacion Paleontologica Argentina, 2016 |g v. 53 |h pp. 333-357 |k n. 3 |p Ameghiniana |x 00027014 |w (AR-BaUEN)CENRE-497 |t Ameghiniana | |
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| 856 | 4 | 0 | |u https://doi.org/10.5710/AMGH.27.01.2016.2963 |y DOI |
| 856 | 4 | 0 | |u https://hdl.handle.net/20.500.12110/paper_00027014_v53_n3_p333_Carames |y Handle |
| 856 | 4 | 0 | |u https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00027014_v53_n3_p333_Carames |y Registro en la Biblioteca Digital |
| 961 | |a paper_00027014_v53_n3_p333_Carames |b paper |c NP | ||
| 962 | |a info:eu-repo/semantics/article |a info:ar-repo/semantics/artículo |b info:eu-repo/semantics/publishedVersion | ||
| 963 | |a NORI | ||
| 999 | |c 76904 | ||