Sedimentary C/N and δ13C of the Honghu Lake sediment core

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Autores principales: Zeng, Linghan, McGowan, Suzanne, Swann, George E A, Leng, Melanie J, Chen, Xu
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2021
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author Zeng, Linghan
McGowan, Suzanne
Swann, George E A
Leng, Melanie J
Chen, Xu
author_facet Zeng, Linghan
McGowan, Suzanne
Swann, George E A
Leng, Melanie J
Chen, Xu
collection Datos científicos de ciencias marinas y ambientales
contents The sedimentary C/N and δ13C in six Yangtze floodplain (China) lake sediment cores since 1800s CE. The sediment cores were dated using lead-210. C/N ratios and δ13C were analysed at the National Environmental Isotope Facility at the British Geological Survey, after preliminary treatment (HCl (5%) to remove calcites) in the School of Geography at the University of Nottingham, using Costech Elemental Analyser (EA) and on-line VG TripleTrap and Optima dual-inlet mass spectrometer. TOC and TN content were calibrated using the acetanilide standard. δ13C was calibrated to the Vienna Pee Dee Belemnite (VPDB) using laboratory standards which were calibrated against NBS-18, NBS-19 and NBS-22.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_938039
institution PANGAEA
language en
publishDate 2021
publisher PANGAEA
record_format pangaea
spellingShingle Sedimentary C/N and δ13C of the Honghu Lake sediment core
Zeng, Linghan
McGowan, Suzanne
Swann, George E A
Leng, Melanie J
Chen, Xu
Age; AGE; Age, 210Pb; C/N; Carbon/Nitrogen ratio; Element analyser CHN (ECS4010, Costech) coupled to a VG Triple Trap and a VG Optima dual-inlet mass spectrometer (MS); Honghu Lake sediment core; SEDCO; SEDCO_HonghuLake; Sediment corer; Yangtze floodplain, China; Yangtze River; δ13C; δ13C, organic carbon
The sedimentary C/N and δ13C in six Yangtze floodplain (China) lake sediment cores since 1800s CE. The sediment cores were dated using lead-210. C/N ratios and δ13C were analysed at the National Environmental Isotope Facility at the British Geological Survey, after preliminary treatment (HCl (5%) to remove calcites) in the School of Geography at the University of Nottingham, using Costech Elemental Analyser (EA) and on-line VG TripleTrap and Optima dual-inlet mass spectrometer. TOC and TN content were calibrated using the acetanilide standard. δ13C was calibrated to the Vienna Pee Dee Belemnite (VPDB) using laboratory standards which were calibrated against NBS-18, NBS-19 and NBS-22.
title Sedimentary C/N and δ13C of the Honghu Lake sediment core
topic Age; AGE; Age, 210Pb; C/N; Carbon/Nitrogen ratio; Element analyser CHN (ECS4010, Costech) coupled to a VG Triple Trap and a VG Optima dual-inlet mass spectrometer (MS); Honghu Lake sediment core; SEDCO; SEDCO_HonghuLake; Sediment corer; Yangtze floodplain, China; Yangtze River; δ13C; δ13C, organic carbon
url https://doi.org/10.1594/PANGAEA.938039