ON THE RELATIONSHIP BETWEEN HOLOCENE ENVIRONMENTAL VARIABILITy AND THE DIATOM COMPOSITION IN THE PEÑA LAGOON, SE URUGUAY

Carolina Celeste Cuña Rodriguez, Eduardo Piovano, Laura del Puerto, Hugo Inda, Felipe García Rodriguez

Abstract


Uruguayan Southern lagoons exhibit high Holocene resolution paleoenvironmental-paleoclimatic records for inferring long-term regional
changes. The multiproxy analysis of three sediment cores enabled the recognition of Holocene climatic variability from the paleolimnological
record of the Peña lagoon over the last 2,458 cal. years BP. Four main stages were identified throughout the record. The first stage
(2,458–1,500 cal. years BP) was characterized as a shallow meso-eutrophic system with high abundances of aerophilic benthic species, epiphytic
taxa and planktonic taxa. The second stage (1,415–390 cal. years BP) showed a noticeable change in the diatom assemblage dominated
by the fresh-brackish benthic species Staurosira construens, but also presented fluctuations in the abundance of Aulacoseira ambigua and Aulacoseira granulata, which indicate the occurrence of temperate to cold and semiarid climatic conditions including intervals of high rainfall. The core
chronology allowed us to ascribe this stage to the Little Ice Age (LIA). The third stage, post 390 cal. years BP, showed the highest proportion
of freshwater planktonic species throughout the entire core, thus indicating the development of an eutrophic system under relatively warm and
wet conditions, which were assigned to the Current Warm Period. After ca. 1,962 AD, a sharp increase in the abundance of epiphytic species
highlights the onset of the fourth stage, which was characterized by littoral expansion and, consequently, the proliferation of associated macrophytes
due to anthropogenic impacts.

Keywords


Diatoms; Holocene; Southeastern Uruguay; Paleoecology

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