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Main Authors: Álvarez-Barra, Valentina Andrea, Giesecke, Thomas, Fontana, Sonia L
Format: Dataset Open Access
Language:en
Published: PANGAEA 2021
Subjects:
Online Access:https://doi.org/10.1594/PANGAEA.936379
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author Álvarez-Barra, Valentina Andrea
Giesecke, Thomas
Fontana, Sonia L
author_facet Álvarez-Barra, Valentina Andrea
Giesecke, Thomas
Fontana, Sonia L
collection Datos científicos de ciencias marinas y ambientales
contents Here we present pollen and charcoal counts from a small lake located within the Lanín National Park, Argentina (40°12'S; 71°30'W; 1095 m a.s.l). The lacustrine sediment core was retrieved in January 2017. Pollen samples of 0.5 cm^3 were taken every 2 cm, avoiding tephra sections. Before and after major tephra layers the sampling was carried out at an interval of 1 cm. Processing of samples for pollen analysis was conducted following Bennett and Willis (2001; doi:10.1007/0-306-47668-1), including hydrofluoric acid and acetolysis. Samples with coarse particles were sieved at 120 µm. To reconstruct the past fire regime, macroscopic charcoal particles were counted in 1 cm^3 samples contiguously along the core at 1 cm intervals avoiding tephra layers wider than 1 cm. The samples were processed according to the methodology by Stevenson and Haberle (2005; hdl:1885/144170). Particles > 125 µm were counted under a binocular dissecting microscope (Whitlock and Anderson, 2003; doi:10.1007/0-387-21710-X_1).
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_936379
institution PANGAEA
language en
publishDate 2021
publisher PANGAEA
record_format pangaea
spellingShingle Holocene changes in forest composition in northern Patagonia responded to climate with little impact of disturbance
Álvarez-Barra, Valentina Andrea
Giesecke, Thomas
Fontana, Sonia L
Charcoal; Chile; northern Patagonia; Nothofagus obliqua; Pollen
Here we present pollen and charcoal counts from a small lake located within the Lanín National Park, Argentina (40°12'S; 71°30'W; 1095 m a.s.l). The lacustrine sediment core was retrieved in January 2017. Pollen samples of 0.5 cm^3 were taken every 2 cm, avoiding tephra sections. Before and after major tephra layers the sampling was carried out at an interval of 1 cm. Processing of samples for pollen analysis was conducted following Bennett and Willis (2001; doi:10.1007/0-306-47668-1), including hydrofluoric acid and acetolysis. Samples with coarse particles were sieved at 120 µm. To reconstruct the past fire regime, macroscopic charcoal particles were counted in 1 cm^3 samples contiguously along the core at 1 cm intervals avoiding tephra layers wider than 1 cm. The samples were processed according to the methodology by Stevenson and Haberle (2005; hdl:1885/144170). Particles > 125 µm were counted under a binocular dissecting microscope (Whitlock and Anderson, 2003; doi:10.1007/0-387-21710-X_1).
title Holocene changes in forest composition in northern Patagonia responded to climate with little impact of disturbance
topic Charcoal; Chile; northern Patagonia; Nothofagus obliqua; Pollen
url https://doi.org/10.1594/PANGAEA.936379