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Daniel Panario

Researcher at University of the Republic

Publications -  34
Citations -  464

Daniel Panario is an academic researcher from University of the Republic. The author has contributed to research in topics: Climate change & Holocene. The author has an hindex of 14, co-authored 32 publications receiving 368 citations.

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The relationship between emergence of mound builders in SE Uruguay and climate change inferred from opal phytolith records

TL;DR: In this paper, the relationship between paleoclimate and prehistoric mound builders development between 7.0 and 0.6 ǫ 14 C BP was studied in SE Uruguay, where the phytolith record of three lagoon sediment cores was inferred.
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The continental Uruguayan Cenozoic: an overview

TL;DR: In this paper, the authors discuss the limitations in the usage of chronostratigraphic generalizations in the Cenozoic based on a geomorphological interpretation and present a comparative preliminary table with the geological formations found in the neighbouring Argentine Provinces of Entre Rios and Corrientes.
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The irruption of new agro-industrial technologies in Uruguay and their environmental impacts on soil, water supply and biodiversity: a review

TL;DR: This review (with emphasis on Uruguay and the River Plata Basin) tries to contribute to an integrated vision of the environmental consequences of current land-use change.
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Assessing links between late Holocene climate change and paleolimnological development of Peña Lagoon using opal phytoliths, physical, and geochemical proxies

TL;DR: In this article, Opal phytolith, geochemical and sedimentological data from two cores taken in Pena Lagoon, a small water body on the Atlantic shore of Uruguay, are presented to infer late Holocene environmental and climatic changes in southeastern Uruguay, in order to improve previous models for early and middle Holocene.
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Land Use Change in a Temperate Grassland Soil: Afforestation Effects on Chemical Properties and Their Ecological and Mineralogical Implications

TL;DR: The results show that the exportation of some nutrients is not compensated due to the turnover of organic forestry debris; the process of soil acidification was not directly associated with the redistribution of cations, but with an incipient podzolization process; the loss of potassium together with soil acidisation, leads to a drastic change in clay mineralogy, which would be irreversible.