globalchange  > 过去全球变化的重建
DOI: 10.1016/j.palaeo.2014.10.032
Title:
Marine connections of Amazonia: Evidence from foraminifera and dinoflagellate cysts (early to middle Miocene, Colombia/Peru)
Author: Boonstra M.; Ramos M.I.F.; Lammertsma E.I.; Antoine P.-O.; Hoorn C.
Source Publication: Palaeogeography, Palaeoclimatology, Palaeoecology
ISSN: 0031-0182
Publishing Year: 2015
Volume: 417
pages begin: 176
pages end: 194
Language: 英语
Keyword: Marginal marine ; Marine palynomorphs ; Micropaleontology ; Neogene ; Pebas
English Abstract: Species composition in the present-day Amazonian heartland has an imprint of past marine influence. The exact nature, timing and extent of this marine influence, however, are largely unresolved. Here we use calcareous tests of foraminifera and marine palynomorphs from Miocene sediments in northwestern Amazonia to extend on current estimates for salinity ranges, paleoenvironments and paleogeography. Our samples mostly contain tests and/or organic linings of euryhaline (tolerant to a wide range of salinity) foraminifera of the genera Ammonia, Trochammina and Elphidium, with Ammonia being by far the dominant genus at all locations. Organic-walled dinoflagellate cysts (dinocysts), such as Spiniferites, Brigantedinium and Tuberculodinium vancampoae, are also common at a number of sites. This association of foraminifera and dinocyst taxa points at varying salinities, with aberrant forms of Ammonia indicating lower limits of 0-10. psu (practical salinity units) whereas dinocyst associations suggest more marine conditions. Such regional heterogeneity is common at the interface of shallow marine to freshwater environments, like estuaries. We conclude that during the early and middle Miocene marginal marine conditions reached at least 2000. km inland from the Caribbean portal. Global high sea level and fast subsidence in the sub-Andean zone are thought to be the controlling mechanisms of the marine incursions. Lowering of global sea level and a change in tectonic regime terminated the incursions in the course of the Plio-Pleistocene. © 2014 Elsevier B.V.
Citation statistics:
被引频次[WOS]:27   [查看WOS记录]     [查看WOS中相关记录]
Document Type: 期刊论文
Identifier: http://119.78.100.158/handle/2HF3EXSE/69074
Appears in Collections:过去全球变化的重建

Files in This Item:

There are no files associated with this item.


Affiliation: Paleoecology and Landscape Ecology, Institute for Biodiversity and Ecosystem Dynamics (IBED), University of Amsterdam, P.O. Box 94248, Amsterdam, Netherlands; Museu Paraense Emílio Goeldi, CCTE, Campus de Pesquisa, Av. Perimetral, 1901, Belém, PA, Brazil; Institut des Sciences de l'Évolution, CC064, CNRS, IRD, Université Montpellier 2, Place Eugène Bataillon, Montpellier, France

Recommended Citation:
Boonstra M.,Ramos M.I.F.,Lammertsma E.I.,et al. Marine connections of Amazonia: Evidence from foraminifera and dinoflagellate cysts (early to middle Miocene, Colombia/Peru)[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2015-01-01,417
Service
Recommend this item
Sava as my favorate item
Show this item's statistics
Export Endnote File
Google Scholar
Similar articles in Google Scholar
[Boonstra M.]'s Articles
[Ramos M.I.F.]'s Articles
[Lammertsma E.I.]'s Articles
百度学术
Similar articles in Baidu Scholar
[Boonstra M.]'s Articles
[Ramos M.I.F.]'s Articles
[Lammertsma E.I.]'s Articles
CSDL cross search
Similar articles in CSDL Cross Search
[Boonstra M.]‘s Articles
[Ramos M.I.F.]‘s Articles
[Lammertsma E.I.]‘s Articles
Related Copyright Policies
Null
收藏/分享
所有评论 (0)
暂无评论
 

Items in IR are protected by copyright, with all rights reserved, unless otherwise indicated.