Interhemispheric synchrony of Late‐glacial climatic instability as recorded in proglacial Lake Mascardi, Argentina

Regional vegetation and climate changes during the last 13 kyr from a marine pollen record in Seno Reloncaví, southern Chile

“…7). These conditions, also recorded at the Huelmo site (Moreno and León, 2003) and Lago Condorito (Moreno, 2004), represent the end of the Last Glacial-Interglacial Transition synchronous with the end of the Huelmo-Mascardi Cold Reversal between ~13.5 and 11.5 cal kyr BP (Ariztegui et al, 1997;Moreno et al, 2001;Hajdas et al, 2003). At 12.3 cal kyr BP, the abrupt expansion of Weinmannia recorded in core MD07-3104 corresponds roughly with the expansion of Weinmannia observed in the terrestrial pollen records, varying from site to site:…”

Regional vegetation and climate changes during the last 13 kyr from a marine pollen record in Seno Reloncaví, southern Chile

“…7). These conditions, also recorded at the Huelmo site (Moreno and León, 2003) and Lago Condorito (Moreno, 2004), represent the end of the Last Glacial-Interglacial Transition synchronous with the end of the Huelmo-Mascardi Cold Reversal between ~13.5 and 11.5 cal kyr BP (Ariztegui et al, 1997;Moreno et al, 2001;Hajdas et al, 2003). At 12.3 cal kyr BP, the abrupt expansion of Weinmannia recorded in core MD07-3104 corresponds roughly with the expansion of Weinmannia observed in the terrestrial pollen records, varying from site to site:…”

The chronology of the Last Glacial Maximum and deglacial events in central Argentine Patagonia

“…cal ka during the Huelmo/Mascardi Cold Reversal (11.4 -10.2 14 C ka), which is approximately coincident with the Younger Dryas stadial but began 550 years earlier ([Ariztegui et al, 1997] and [Hajdas et al, 2003] Hemisphere influences as previously suggested for southernmost Patagonia .…”

Late Holocene Glacier fluctuations in southernmost Patagonia.

“…Glaciers adjust their thickness, width and length in response to long-term changes in precipitation and temperature (Denton and Karlen, 1973;Ariztegui et al, 1997). Changes in length are typically the most obvious indicators of a glacier's response to past climate change (Osbom et al, 2007;Menounos et al, 2009).…”

Regional vegetation and climate changes during the last 13 kyr from a marine pollen record in Seno Reloncaví, southern Chile

“…7). These conditions, also recorded at the Huelmo site (Moreno and León, 2003) and Lago Condorito (Moreno, 2004), represent the end of the Last Glacial-Interglacial Transition synchronous with the end of the Huelmo-Mascardi Cold Reversal between ~13.5 and 11.5 cal kyr BP (Ariztegui et al, 1997;Moreno et al, 2001;Hajdas et al, 2003). At 12.3 cal kyr BP, the abrupt expansion of Weinmannia recorded in core MD07-3104 corresponds roughly with the expansion of Weinmannia observed in the terrestrial pollen records, varying from site to site:…”

The chronology of the Last Glacial Maximum and deglacial events in central Argentine Patagonia

“…cal ka during the Huelmo/Mascardi Cold Reversal (11.4 -10.2 14 C ka), which is approximately coincident with the Younger Dryas stadial but began 550 years earlier ([Ariztegui et al, 1997] and [Hajdas et al, 2003] Hemisphere influences as previously suggested for southernmost Patagonia .…”

Late Holocene Glacier fluctuations in southernmost Patagonia.

“…Glaciers adjust their thickness, width and length in response to long-term changes in precipitation and temperature (Denton and Karlen, 1973;Ariztegui et al, 1997). Changes in length are typically the most obvious indicators of a glacier's response to past climate change (Osbom et al, 2007;Menounos et al, 2009).…”

Regional vegetation and climate changes during the last 13 kyr from a marine pollen record in Seno Reloncaví, southern Chile

“…7). These conditions, also recorded at the Huelmo site (Moreno and León, 2003) and Lago Condorito (Moreno, 2004), represent the end of the Last Glacial-Interglacial Transition synchronous with the end of the Huelmo-Mascardi Cold Reversal between ~13.5 and 11.5 cal kyr BP (Ariztegui et al, 1997;Moreno et al, 2001;Hajdas et al, 2003). At 12.3 cal kyr BP, the abrupt expansion of Weinmannia recorded in core MD07-3104 corresponds roughly with the expansion of Weinmannia observed in the terrestrial pollen records, varying from site to site:…”

The chronology of the Last Glacial Maximum and deglacial events in central Argentine Patagonia

“…cal ka during the Huelmo/Mascardi Cold Reversal (11.4 -10.2 14 C ka), which is approximately coincident with the Younger Dryas stadial but began 550 years earlier ([Ariztegui et al, 1997] and [Hajdas et al, 2003] Hemisphere influences as previously suggested for southernmost Patagonia .…”

Late Holocene Glacier fluctuations in southernmost Patagonia.

“…Glaciers adjust their thickness, width and length in response to long-term changes in precipitation and temperature (Denton and Karlen, 1973;Ariztegui et al, 1997). Changes in length are typically the most obvious indicators of a glacier's response to past climate change (Osbom et al, 2007;Menounos et al, 2009).…”