δ18O and δ13C from sediment core of Lake Alchichica in Mexico

Fuente: PANGAEA
Guardado en:
Detalles Bibliográficos
Autores principales: Safaierad, Reza, Israde-Alcántara, Isabel, Rantala, Marttiina V, Domínguez-Vázquez, Gabriela, Schefuß, Enno, Tylmann, Wojciech, Francus, Pierre, Mattielli, Nadine, Metcalfe, Sarah, Fagel, Nathalie
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2026
Materias:
Acceso en línea:
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
_version_ 1867171052354797568
author Safaierad, Reza
Israde-Alcántara, Isabel
Rantala, Marttiina V
Domínguez-Vázquez, Gabriela
Schefuß, Enno
Tylmann, Wojciech
Francus, Pierre
Mattielli, Nadine
Metcalfe, Sarah
Fagel, Nathalie
author_facet Safaierad, Reza
Israde-Alcántara, Isabel
Rantala, Marttiina V
Domínguez-Vázquez, Gabriela
Schefuß, Enno
Tylmann, Wojciech
Francus, Pierre
Mattielli, Nadine
Metcalfe, Sarah
Fagel, Nathalie
collection Datos científicos de ciencias marinas y ambientales
contents The proxy data are measured from a 57-cm long sediment core collected from Lake Alchichica (19° 24' 38 N, 97° 24' 14 W, 2322 masl) at a water depth of ~ 60 m using a Uwitec® coring device equipped with a 9-cm coring tube. The core was split lengthwise, analyzed using XRF core scanning, and subsampled. A Bayesian chronology was created using 210Pb data and three 14C dates. For stable isotope geochemistry (δ¹⁸O and δ¹³C) of bulk sediments, samples collected at 1 cm intervals were analyzed at MARUM, University of Bremen, using a Finnigan MAT252 mass spectrometer with a Kiel III carbonate preparation device. Results are reported in delta notation (δ) relative to VPDB. Calibration involved a house standard (Solnhofen limestone) referenced to NBS 19 calcite, with standard deviations of 0.06‰ for both δ¹³C and δ¹⁸O.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_982934
institution PANGAEA
language en
publishDate 2026
publisher PANGAEA
record_format pangaea
spellingShingle δ18O and δ13C from sediment core of Lake Alchichica in Mexico
Safaierad, Reza
Israde-Alcántara, Isabel
Rantala, Marttiina V
Domínguez-Vázquez, Gabriela
Schefuß, Enno
Tylmann, Wojciech
Francus, Pierre
Mattielli, Nadine
Metcalfe, Sarah
Fagel, Nathalie
AGE; Age, Bayesian based model Plum on Pb-210 and C-14 data; carbon isotope; DEPTH, sediment/rock; Deuterium Isotopes; Lake_Alchichica; leaf waxes; Mass spectrometer, Finnigan, MAT 252; Mexico; oxygen isotope; Pollen; Sediment core; Sediment corer, UWITEC; XRD; XRF core scanner data; δ13C; δ13C, standard deviation; δ18O; δ18O, standard deviation
The proxy data are measured from a 57-cm long sediment core collected from Lake Alchichica (19° 24' 38 N, 97° 24' 14 W, 2322 masl) at a water depth of ~ 60 m using a Uwitec® coring device equipped with a 9-cm coring tube. The core was split lengthwise, analyzed using XRF core scanning, and subsampled. A Bayesian chronology was created using 210Pb data and three 14C dates. For stable isotope geochemistry (δ¹⁸O and δ¹³C) of bulk sediments, samples collected at 1 cm intervals were analyzed at MARUM, University of Bremen, using a Finnigan MAT252 mass spectrometer with a Kiel III carbonate preparation device. Results are reported in delta notation (δ) relative to VPDB. Calibration involved a house standard (Solnhofen limestone) referenced to NBS 19 calcite, with standard deviations of 0.06‰ for both δ¹³C and δ¹⁸O.
title δ18O and δ13C from sediment core of Lake Alchichica in Mexico
topic AGE; Age, Bayesian based model Plum on Pb-210 and C-14 data; carbon isotope; DEPTH, sediment/rock; Deuterium Isotopes; Lake_Alchichica; leaf waxes; Mass spectrometer, Finnigan, MAT 252; Mexico; oxygen isotope; Pollen; Sediment core; Sediment corer, UWITEC; XRD; XRF core scanner data; δ13C; δ13C, standard deviation; δ18O; δ18O, standard deviation
url https://doi.org/10.1594/PANGAEA.982934