Dr. Patricio Moreno
Doctor en Biología Vegetal de la Universidad de Maine, Estados Unidos. Actualmente es profesor asociado de la Universidad de Chile.
Área de investigación: estudio de los patrones, tasas y mecanismos de cambio en ecosistemas terrestres y clima durante el Cuaternario (los últimos 2.5 millones de años). Su trabajo se concentra en Patagonia y busca entender el contexto ambiental (climático y no climático) en el cual han ocurrido las profundas transformaciones biológicas asociadas al último ciclo glacial-interglacial.
Artículos Científicos Recientes
- Glacier fluctuations in the northern Patagonian Andes (44 degrees S) imply wind-modulated interhemispheric in-phase climate shifts during Termination 1
- The large MIS 4 and long MIS 2 glacier maxima on the southern tip of South America
- Vegetation, disturbance, and climate history since the onset of ice-free conditions in the Lago Rosselot sector of Chiloe continental (44 degrees S), northwestern Patagonia
- Development and resilience of deciduous Nothofagus forests since the Last Glacial Termination and deglaciation of the central Patagonian Andes
- The role of climate and disturbance regimes upon temperate rainforests during the Holocene: A stratigraphic perspective from Lago Fonk (-40 degrees S), northwestern Patagonia
- The last glacial termination in northwestern Patagonia viewed from the Lago Fonk (similar to 40 degrees S) record
- An early Holocene westerly minimum in the southern mid-latitudes
- Centennial and millennial-scale dynamics in Araucaria-Nothofagus forests in the southern Andes
- The deglaciation of the Americas during the Last Glacial Termination
- Timing and structure of vegetation, fire, and climate changes on the Pacific slope of northwestern Patagonia since the last glacial termination