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dc.contributor.author
Garcia Rodriguez, Felipe
dc.contributor.author
Stutz, Silvina Maria
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Inda, Hugo
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del Puerto, Laura
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Bracco, Roberto
dc.contributor.author
Panario, Daniel
dc.date.available
2020-01-29T15:02:16Z
dc.date.issued
2010-06
dc.identifier.citation
Garcia Rodriguez, Felipe; Stutz, Silvina Maria; Inda, Hugo; del Puerto, Laura; Bracco, Roberto; et al.; A multiproxy approach to inferring Holocene paleobotanical changes linked to sea-level variation, paleosalinity levels, and shallow lake alternative states in Negra Lagoon, SE Uruguay; Springer; Hydrobiologia; 646; 1; 6-2010; 5-20
dc.identifier.issn
0018-8158
dc.identifier.uri
http://hdl.handle.net/11336/96096
dc.description.abstract
A multiproxy analysis of diatoms, chrysophyte cysts, opal phytoliths, and palynomorphs was undertaken in Negra Lagoon, to decipher Holocene changes in paleobotanical proxies associated with sea-level changes and paleolimnological conditions. Before the Holocene transgression (7000 yr BP), a terrestrial system was inferred as no aquatic palynomorphs or biogenic silica remains were recorded. During the sea-level maximum (5200 yr BP), marine/brackish conditions were established as indicated by diatoms, Chenopodiaceae, and a high content of cysts of Peridinioideae. The catchment consisted of grasslands and wetlands as indicated by the opal phytolith data. The Holocene transgression was followed by a sea-level decrease, which led to the onset of brackish/freshwater conditions as inferred from the co-dominance of freshwater and marine/brackish diatoms. This is also supported not only by the concomitant increase in non-siliceous freshwater microalgae and emergent macrophytes, but also by the presence of Myriophyllum. As sea level continued to decrease during late Holocene, a freshwater system was observed because of the complete separation from the ocean. Chrysophyte cysts were consistently recorded and brackish diatoms exhibited reduced abundances. The observed limnological changes are consistent with the alternative states hypothesis of Scheffer’s model (1998). That is, the clear water phases were explained because of high macrophyte abundances, low phytoplankton frequencies, high cyst to diatom ratios, and increase in frequencies of benthic diatom species. Conversely, turbid phases were likely to occur when low cyst to diatom ratios together with increase in planktonic diatoms and decrease in macrophytes values were detected. This highlights the importance of this approach to detect long-term changes in shallow lake alternative states.
dc.format
application/pdf
dc.language.iso
eng
dc.publisher
Springer
dc.rights
info:eu-repo/semantics/restrictedAccess
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.subject
Alternative States
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Diatoms
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Chrysophyte cysts
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Opal phytoliths
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Pollen
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Paleolimnology
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Paleontología
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Ciencias de la Tierra y relacionadas con el Medio Ambiente
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CIENCIAS NATURALES Y EXACTAS
dc.title
A multiproxy approach to inferring Holocene paleobotanical changes linked to sea-level variation, paleosalinity levels, and shallow lake alternative states in Negra Lagoon, SE Uruguay
dc.type
info:eu-repo/semantics/article
dc.type
info:ar-repo/semantics/artículo
dc.type
info:eu-repo/semantics/publishedVersion
dc.date.updated
2020-01-28T15:01:37Z
dc.journal.volume
646
dc.journal.number
1
dc.journal.pagination
5-20
dc.journal.pais
Alemania
dc.description.fil
Fil: Garcia Rodriguez, Felipe. Universidad de la República; Uruguay
dc.description.fil
Fil: Stutz, Silvina Maria. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de Mar del Plata. Facultad de Ciencias Exactas y Naturales. Laboratorio de Paleoecología y Palinología; Argentina
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Fil: Inda, Hugo. Universidad de la República; Uruguay
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Fil: del Puerto, Laura. Museo de Historia Natural y Antropología; Uruguay
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Fil: Bracco, Roberto. Universidad de la República; Uruguay. Museo de Historia Natural y Antropología; Uruguay
dc.description.fil
Fil: Panario, Daniel. Universidad de la República; Uruguay
dc.journal.title
Hydrobiologia
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://link.springer.com/article/10.1007/s10750-010-0184-0
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1007/s10750-010-0184-0
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