Dr. Patricio Moreno
Linea de Investigación: PaleoecologíaDoctor 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