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DC Field | Value | Language |
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dc.contributor.author | Brunelle, Andrea | - |
dc.contributor.author | Crespo Sanchez, Patricio Javier | - |
dc.date.accessioned | 2018-10-19T15:56:07Z | - |
dc.date.available | 2018-10-19T15:56:07Z | - |
dc.date.issued | 2018 | - |
dc.identifier.issn | 1477-0911 | - |
dc.identifier.uri | http://dspace.ucuenca.edu.ec/handle/123456789/31436 | - |
dc.identifier.uri | https://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85045052071&origin=inward | - |
dc.description | Previous paleoclimate studies have suggested a warm/dry event during the mid-Holocene in páramo vegetation of the tropical Andes of South America. However, the timing of the mid- Holocene warm/dry event in Tres Lagunas, Ecuador, remains uncertain, since a previously reported bog core record characterized the warm/dry event during a hiatus in sediment deposition. In order to understand the timing of the warm/dry event in Tres Lagunas in relation to regional records, a lake sediment core was collected. Subsamples from the core were analyzed for radiocarbon dates, pollen, magnetic susceptibility, and charcoal to reconstruct the depositional, vegetational, and fire history of the area. A near-constant sedimentation rate in the lake core indicated that the lake did not dry, in contrast to the adjacent previously reported bog core. Increases in lower elevation pollen types suggest … | - |
dc.description.abstract | Previous paleoclimate studies have suggested a warm/dry event during the mid-Holocene in páramo vegetation of the tropical Andes of South America. However, the timing of the mid- Holocene warm/dry event in Tres Lagunas, Ecuador, remains uncertain, since a previously reported bog core record characterized the warm/dry event during a hiatus in sediment deposition. In order to understand the timing of the warm/dry event in Tres Lagunas in relation to regional records, a lake sediment core was collected. Subsamples from the core were analyzed for radiocarbon dates, pollen, magnetic susceptibility, and charcoal to reconstruct the depositional, vegetational, and fire history of the area. A near-constant sedimentation rate in the lake core indicated that the lake did not dry, in contrast to the adjacent previously reported bog core. Increases in lower elevation pollen types suggest … | - |
dc.language.iso | es_ES | - |
dc.source | Holocene | - |
dc.subject | Charcoal | - |
dc.subject | Holocene Warmdry Period | - |
dc.subject | Magnetic Susceptibility | - |
dc.subject | Paleoenvironment | - |
dc.subject | Pollen | - |
dc.title | Reconstruction of the mid-Holocene paleoclimate of the Ecuadorian Andean páramo at Tres Lagunas, Ecuador | - |
dc.type | ARTÍCULO | - |
dc.ucuenca.idautor | 0000-0001-6552-0056 | - |
dc.ucuenca.idautor | 0102572773 | - |
dc.identifier.doi | 10.1177/0959683618761547 | - |
dc.ucuenca.embargoend | 2050-12-28 | - |
dc.ucuenca.version | Versión publicada | - |
dc.ucuenca.embargointerno | 2050-12-28 | - |
dc.ucuenca.areaconocimientounescoamplio | 05 - CIENCIAS FISICAS, CIENCIAS NATURALES, MATEMATICAS Y ESTADISTICAS | - |
dc.ucuenca.afiliacion | Brunelle, A., University of Utah, Salt Lake City, Estados unidos | - |
dc.ucuenca.afiliacion | Crespo, P., Universidad de Cuenca, Departamento de Recursos Hídricos y Ciencias Ambientales, Cuenca, Ecuador | - |
dc.ucuenca.volumen | volumen 28, número 7 | - |
dc.ucuenca.indicebibliografico | SCOPUS | - |
dc.ucuenca.factorimpacto | 1.202 | - |
dc.ucuenca.cuartil | Q2 | - |
dc.ucuenca.numerocitaciones | 0 | - |
dc.ucuenca.areaconocimientofrascatiamplio | 1. CIENCIAS NATURALES Y EXACTAS | - |
dc.ucuenca.areaconocimientofrascatiespecifico | 1.5 CIENCIAS DE LA TIERRA Y EL AMBIENTE | - |
dc.ucuenca.areaconocimientofrascatidetallado | 1.5.1 CIENCIAS DE LA TIERRA, MULTIDISCIPLINARIOS | - |
dc.ucuenca.areaconocimientounescoespecifico | 052 - MEDIO AMBIENTE | - |
dc.ucuenca.areaconocimientounescodetallado | 0521 - CIENCIAS AMBIENTALES | - |
dc.ucuenca.urifuente | http://hol.sagepub.com/ | - |
Appears in Collections: | Artículos |
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documento.pdf Until 2050-12-28 | document | 111.03 kB | Adobe PDF | View/Open Request a copy |
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