δ¹³C stalagmite records from South America

Fuente: PANGAEA
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Hauptverfasser: Novello, Valdir Felipe, Azevedo, Vitor, Apaéstegui, James, Wang, Xianfeng
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2020
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_version_ 1867171020911149056
author Novello, Valdir Felipe
Azevedo, Vitor
Apaéstegui, James
Wang, Xianfeng
author_facet Novello, Valdir Felipe
Azevedo, Vitor
Apaéstegui, James
Wang, Xianfeng
collection Datos científicos de ciencias marinas y ambientales
contents Measurements of carbon isotope (δ¹³C) ratios are essential for (paleo)environmental studies, such as those regarding the carbon cycle, past food consumption by pre-historic societies, paleo-vegetation reconstructions, soil dynamics, aspects regarding animal migration and food consumption, etc. Our main goal with this study is to introduce new cave records to the speleothem community and contextualize their interpretation in a regional framework for South America during the last two millennia. The dataset presented (named δ¹³C_2k_SA) comprises thirteen new δ¹³C speleothem records that were integrated to other 12 records already published to test the influence of local hydroclimate, altitude, temperature and changing vegetation types on δ¹³C values in stalagmites.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_919050
institution PANGAEA
language en
publishDate 2020
publisher PANGAEA
record_format pangaea
spellingShingle δ¹³C stalagmite records from South America
Novello, Valdir Felipe
Azevedo, Vitor
Apaéstegui, James
Wang, Xianfeng
Age; AGE; ALTITUDE; Area/locality; Botuverá_Cave; Brazil; Curupita_Cave; d13C; Depth, relative; Diva_de_Maura_Cave; Event label; Furna_Nova; Identification; JAR; Jaraguá_Cave; Lada_dos_Anjos_Cave; LAND; Lapa_Doce_Cave; Latitude of event; Longitude of event; paleohydrology; paleovegetation; Palestina_Cave; Sampling/measurement on land; Sao_Bernardo_Cave; Sao_Matheus_Cave; South America; stalagmite; Torrinha_Cave; Trapiá_Cave; Umajalanta_Chiflonkhakha_Cave; δ13C, calcite
Measurements of carbon isotope (δ¹³C) ratios are essential for (paleo)environmental studies, such as those regarding the carbon cycle, past food consumption by pre-historic societies, paleo-vegetation reconstructions, soil dynamics, aspects regarding animal migration and food consumption, etc. Our main goal with this study is to introduce new cave records to the speleothem community and contextualize their interpretation in a regional framework for South America during the last two millennia. The dataset presented (named δ¹³C_2k_SA) comprises thirteen new δ¹³C speleothem records that were integrated to other 12 records already published to test the influence of local hydroclimate, altitude, temperature and changing vegetation types on δ¹³C values in stalagmites.
title δ¹³C stalagmite records from South America
topic Age; AGE; ALTITUDE; Area/locality; Botuverá_Cave; Brazil; Curupita_Cave; d13C; Depth, relative; Diva_de_Maura_Cave; Event label; Furna_Nova; Identification; JAR; Jaraguá_Cave; Lada_dos_Anjos_Cave; LAND; Lapa_Doce_Cave; Latitude of event; Longitude of event; paleohydrology; paleovegetation; Palestina_Cave; Sampling/measurement on land; Sao_Bernardo_Cave; Sao_Matheus_Cave; South America; stalagmite; Torrinha_Cave; Trapiá_Cave; Umajalanta_Chiflonkhakha_Cave; δ13C, calcite
url https://doi.org/10.1594/PANGAEA.919050