δ¹⁸O record and Th230 dating results of espeleothems from Jaraguá cave, Brazil, 2017

Fuente: PANGAEA
Salvato in:
Dettagli Bibliografici
Autori principali: Novello, Valdir Felipe, da Cruz Junior, Francisco William, Vuille, Mathias, Stríkis, Nicolás Misailidis, Edwards, R Lawrence, Cheng, Hai, Emerick, Suellyn, Saito de Paula, Marcos, Li, Xianglei, Barreto, Eline de Souza, Karmann, Ivo, Santos, Roberto Ventura
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 2017
Soggetti:
Accesso online:
Tags: Aggiungi Tag
Nessun Tag, puoi essere il primo ad aggiungerne!!
_version_ 1867172224264306688
author Novello, Valdir Felipe
da Cruz Junior, Francisco William
Vuille, Mathias
Stríkis, Nicolás Misailidis
Edwards, R Lawrence
Cheng, Hai
Emerick, Suellyn
Saito de Paula, Marcos
Li, Xianglei
Barreto, Eline de Souza
Karmann, Ivo
Santos, Roberto Ventura
author_facet Novello, Valdir Felipe
da Cruz Junior, Francisco William
Vuille, Mathias
Stríkis, Nicolás Misailidis
Edwards, R Lawrence
Cheng, Hai
Emerick, Suellyn
Saito de Paula, Marcos
Li, Xianglei
Barreto, Eline de Souza
Karmann, Ivo
Santos, Roberto Ventura
collection Datos científicos de ciencias marinas y ambientales
contents The exact extent, by which the hydrologic cycle in the Neotropics was affected by external forcing during the last deglaciation, remains poorly understood. Here we present a new paleo-rainfall reconstruction based on high-resolution speleothem d18O records from the core region of the South American Monsoon System (SAMS), documenting the changing hydrological conditions over tropical South America (SA), in particular during abrupt millennial-scale events. This new record provides the best-resolved and most accurately constrained geochronology of any proxy from South America for this time period, spanning from the Last Glacial Maximum (LGM) to the mid-Holocene.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_878258
institution PANGAEA
language en
publishDate 2017
publisher PANGAEA
record_format pangaea
spellingShingle δ¹⁸O record and Th230 dating results of espeleothems from Jaraguá cave, Brazil, 2017
Novello, Valdir Felipe
da Cruz Junior, Francisco William
Vuille, Mathias
Stríkis, Nicolás Misailidis
Edwards, R Lawrence
Cheng, Hai
Emerick, Suellyn
Saito de Paula, Marcos
Li, Xianglei
Barreto, Eline de Souza
Karmann, Ivo
Santos, Roberto Ventura
Brazil; JAR; Jaraguá_Cave; LAND; Sampling/measurement on land
The exact extent, by which the hydrologic cycle in the Neotropics was affected by external forcing during the last deglaciation, remains poorly understood. Here we present a new paleo-rainfall reconstruction based on high-resolution speleothem d18O records from the core region of the South American Monsoon System (SAMS), documenting the changing hydrological conditions over tropical South America (SA), in particular during abrupt millennial-scale events. This new record provides the best-resolved and most accurately constrained geochronology of any proxy from South America for this time period, spanning from the Last Glacial Maximum (LGM) to the mid-Holocene.
title δ¹⁸O record and Th230 dating results of espeleothems from Jaraguá cave, Brazil, 2017
topic Brazil; JAR; Jaraguá_Cave; LAND; Sampling/measurement on land
url https://doi.org/10.1594/PANGAEA.878258