Sulfur Isotopic Analysis and Sulfur Source Study of Phosphorite-associated Sulfate from the Ediacaran Doushantuo Formation in Guizhou Province

BACKGROUND Phosphate deposit of the Ediacaran Doushantuo Formation in Guizhou province is a typical representative of the global phosphorite formation event in the late Neoproterozoic, which is closely related to climate change and evolution of life. However, the current research on the deposition o...

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Main Authors: LI Xuanbo, WANG Ruimin, HUANG Tianzheng, SHUAI Gewei, SHEN Bing
Format: Article
Language:English
Published: Science Press, PR China 2022-07-01
Series:Yankuang ceshi
Subjects:
Online Access:http://www.ykcs.ac.cn/en/article/doi/10.15898/j.cnki.11-2131/td.202202210026
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author LI Xuanbo
WANG Ruimin
HUANG Tianzheng
SHUAI Gewei
SHEN Bing
author_facet LI Xuanbo
WANG Ruimin
HUANG Tianzheng
SHUAI Gewei
SHEN Bing
author_sort LI Xuanbo
collection DOAJ
description BACKGROUND Phosphate deposit of the Ediacaran Doushantuo Formation in Guizhou province is a typical representative of the global phosphorite formation event in the late Neoproterozoic, which is closely related to climate change and evolution of life. However, the current research on the deposition of phosphorus deposits is limited to the mechanism of phosphorus formation and the source of phosphorus, and research on the phosphorus formation process of this deposit and its correlation with the paleo-ocean environment of the same period by isotopic geochemical indicators is relatively weak. OBJECTIVES In order to determine the sulfur source of phosphorite-associated sulfate. METHODS Based on the field section observation and the study of petrological characteristics under the microscope, elemental analyzer-isotope ratio mass spectrometry (EA-IRMS) was used to measure the sulfur isotopic composition of phosphorite-associated sulfate from the Ediacaran Doushantuo Formation. RESULTS: The sulfur isotopic composition of phosphorite-associated sulfate ranged from 32.7‰ to 36.9‰ (n=32, mean=34.1‰), which was 11‰ lower than that of the seawater of the same period, indicating that the phosphorite-associated sulfate was not all from the surface seawater. CONCLUSIONS The idealized early ocean (>520Ma) chemical zoning model indicates that there is a relatively 34S-depleted H2S zone in the seawater at the same time. Combined with the understanding that the source of phosphorus in the phosphorite is closely related to the upwelling, it can be considered that the sulfur isotopic composition of phosphorite-associated sulfate of the Doushantuo Formation represents the mixed signal of surface seawater and upwelling.
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spelling doaj.art-80b900b5e48a4e5b9ff8e7627bde9b7e2023-01-13T05:06:15ZengScience Press, PR ChinaYankuang ceshi0254-53572022-07-0141453154010.15898/j.cnki.11-2131/td.202202210026yk202202210026Sulfur Isotopic Analysis and Sulfur Source Study of Phosphorite-associated Sulfate from the Ediacaran Doushantuo Formation in Guizhou ProvinceLI Xuanbo0WANG Ruimin1HUANG Tianzheng2SHUAI Gewei3SHEN Bing4Key Laboratory of Orogenic Belts and Crustal Evolution, Peking University; School of Earth and Space Sciences, Peking University, Beijing 100871, ChinaKey Laboratory of Orogenic Belts and Crustal Evolution, Peking University; School of Earth and Space Sciences, Peking University, Beijing 100871, ChinaKey Laboratory of Orogenic Belts and Crustal Evolution, Peking University; School of Earth and Space Sciences, Peking University, Beijing 100871, ChinaKey Laboratory of Orogenic Belts and Crustal Evolution, Peking University; School of Earth and Space Sciences, Peking University, Beijing 100871, ChinaKey Laboratory of Orogenic Belts and Crustal Evolution, Peking University; School of Earth and Space Sciences, Peking University, Beijing 100871, ChinaBACKGROUND Phosphate deposit of the Ediacaran Doushantuo Formation in Guizhou province is a typical representative of the global phosphorite formation event in the late Neoproterozoic, which is closely related to climate change and evolution of life. However, the current research on the deposition of phosphorus deposits is limited to the mechanism of phosphorus formation and the source of phosphorus, and research on the phosphorus formation process of this deposit and its correlation with the paleo-ocean environment of the same period by isotopic geochemical indicators is relatively weak. OBJECTIVES In order to determine the sulfur source of phosphorite-associated sulfate. METHODS Based on the field section observation and the study of petrological characteristics under the microscope, elemental analyzer-isotope ratio mass spectrometry (EA-IRMS) was used to measure the sulfur isotopic composition of phosphorite-associated sulfate from the Ediacaran Doushantuo Formation. RESULTS: The sulfur isotopic composition of phosphorite-associated sulfate ranged from 32.7‰ to 36.9‰ (n=32, mean=34.1‰), which was 11‰ lower than that of the seawater of the same period, indicating that the phosphorite-associated sulfate was not all from the surface seawater. CONCLUSIONS The idealized early ocean (>520Ma) chemical zoning model indicates that there is a relatively 34S-depleted H2S zone in the seawater at the same time. Combined with the understanding that the source of phosphorus in the phosphorite is closely related to the upwelling, it can be considered that the sulfur isotopic composition of phosphorite-associated sulfate of the Doushantuo Formation represents the mixed signal of surface seawater and upwelling.http://www.ykcs.ac.cn/en/article/doi/10.15898/j.cnki.11-2131/td.202202210026elemental analyzer-isotope ratio mass spectrometryphosphoritesulfur isotope of phosphorite-associated sulfatedoushantuo formationupwellingh2s zone
spellingShingle LI Xuanbo
WANG Ruimin
HUANG Tianzheng
SHUAI Gewei
SHEN Bing
Sulfur Isotopic Analysis and Sulfur Source Study of Phosphorite-associated Sulfate from the Ediacaran Doushantuo Formation in Guizhou Province
Yankuang ceshi
elemental analyzer-isotope ratio mass spectrometry
phosphorite
sulfur isotope of phosphorite-associated sulfate
doushantuo formation
upwelling
h2s zone
title Sulfur Isotopic Analysis and Sulfur Source Study of Phosphorite-associated Sulfate from the Ediacaran Doushantuo Formation in Guizhou Province
title_full Sulfur Isotopic Analysis and Sulfur Source Study of Phosphorite-associated Sulfate from the Ediacaran Doushantuo Formation in Guizhou Province
title_fullStr Sulfur Isotopic Analysis and Sulfur Source Study of Phosphorite-associated Sulfate from the Ediacaran Doushantuo Formation in Guizhou Province
title_full_unstemmed Sulfur Isotopic Analysis and Sulfur Source Study of Phosphorite-associated Sulfate from the Ediacaran Doushantuo Formation in Guizhou Province
title_short Sulfur Isotopic Analysis and Sulfur Source Study of Phosphorite-associated Sulfate from the Ediacaran Doushantuo Formation in Guizhou Province
title_sort sulfur isotopic analysis and sulfur source study of phosphorite associated sulfate from the ediacaran doushantuo formation in guizhou province
topic elemental analyzer-isotope ratio mass spectrometry
phosphorite
sulfur isotope of phosphorite-associated sulfate
doushantuo formation
upwelling
h2s zone
url http://www.ykcs.ac.cn/en/article/doi/10.15898/j.cnki.11-2131/td.202202210026
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