A Pleistocene (MIS 5e) mollusk assemblage from Ezeiza (Buenos Aires Province, Argentina)

被引:10
作者
Martinez, Sergio [1 ]
Julia del Rio, Claudia [2 ]
Rojas, Alejandra [1 ]
机构
[1] Univ Republica, Fac Ciencias, Igua 4225, Montevideo 11400, Uruguay
[2] Museo Argentino Ciencias Nat Bernardino Rivadavia, Angel Gallardo 470, RA-1405 Buenos Aires, DF, Argentina
关键词
Mollusks; Paleoecology; Biogeography; MIS; 5e; Pleistocene; Argentina; SEA-LEVEL HIGHSTANDS; LAST GLACIAL MAXIMUM; MARINE TERRACES; TEMPERATURE-CHANGES; 40-DEGREES SOUTH; ATLANTIC COAST; ICE VOLUME; EVOLUTION; HOLOCENE; DEPOSITS;
D O I
10.1016/j.jsames.2016.05.008
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
A fossil assemblage collected around 3.5 m amsi from Ezeiza, Buenos Aires province, have AMS C-14 ages of ca. 33,000 to ca. 40,000 yr BP, whereas in the literature is a report of a conventional C-14 age of >43,000 yr BR An OSL age from the overlying deposit corresponds to ca. 22,000 yr. The samples contain marine fossils: mollusks, balanids and corals (Astrangia). La Coronilla (Uruguay, attributed to MIS 5e) is the locality most related to Ezeiza faunistically, despite is not the nearest one. In consequence, the relationship should be addressed to a more similar age and environment than others. The fauna indicates a higher water temperature than today. In Ezeiza exclusively cold water taxa are absent, and we found seven warm taxa with their southern distribution limit displaced northwards today, plus other six at their southern distribution limit. Around 60% of all the species and more than 70% of the individuals are of warm-temperate waters. In sum, although prima facie the numerical ages would locate the deposit in MIS3, faunistic, temperature, and height evidences show that the Ezeiza mollusk assemblage belong to MIS5e. A stronger than presently Brazil warm current, reaching Southern latitudes, may explain the changes in geographical ranges. (C) 2016 Elsevier Ltd. All rights reserved.
引用
收藏
页码:174 / 187
页数:14
相关论文
共 86 条
  • [1] ACUMAR, 2009, EV AMB PROYECT DES S
  • [2] Aguirre M.L., 2004, Instituto Superior de Correlacion Geologica (INSUGEO) Miscelanea, V12, P55
  • [3] LATE QUATERNARY MARGINAL MARINE DEPOSITS AND PALEOENVIRONMENTS FROM NORTHEASTERN BUENOS-AIRES PROVINCE, ARGENTINA - A REVIEW
    AGUIRRE, ML
    WHATLEY, RC
    [J]. QUATERNARY SCIENCE REVIEWS, 1995, 14 (03) : 223 - 254
  • [4] Soil genesis, optical dating, and geoarchaeological evaluation of two upland Alfisol pedons within the Tertiary Gulf Coastal Plain
    Ahr, Steven W.
    Nordt, Lee C.
    Forman, Steven L.
    [J]. GEODERMA, 2013, 192 : 211 - 226
  • [5] Ameghino F., 1880, OBRAS COMPLETAS, VIII, P868
  • [6] Ameghino F., 1889, Contribucion al conocimiento de los mamiferos fosiles de la Republica Argentina, V6, P1, DOI DOI 10.5962/BHL.TITLE.121288
  • [7] [Anonymous], 2006, BASES CONSERVACION M
  • [8] [Anonymous], 2009, COMPENDIUM BRAZILIAN
  • [9] [Anonymous], 2004, MUSEO NACL HIST NATU
  • [10] ARCHER A W, 1987, Palaios, V2, P609, DOI 10.2307/3514498