High-resolution paired carbon isotopic records from the Meishucun section in South China: Implications for carbon cycling and environmental changes during the Ediacaran-Cambrian transition
•Close link between transgressions and negative δ13C excursions during the E-C transition.•Incursion of 13C-depleted anoxic/euxinic deep waters into shallow-water environment.•Ocean stratification and vertical δ13C gradients.•Reduction of vertical δ13C gradient reflects deep ocean ventilation and ox...
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| Published in | Precambrian research Vol. 337; p. 105561 |
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| Main Authors | , , |
| Format | Journal Article |
| Language | English |
| Published |
Elsevier B.V
01.02.2020
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| Abstract | •Close link between transgressions and negative δ13C excursions during the E-C transition.•Incursion of 13C-depleted anoxic/euxinic deep waters into shallow-water environment.•Ocean stratification and vertical δ13C gradients.•Reduction of vertical δ13C gradient reflects deep ocean ventilation and oxygenation.•Deep ocean oxygenation facilitated the radiation of metazoans during the Cambrian explosion.
Several prominent negative carbon isotope (δ13C) excursions are observed during the Ediacaran-Cambrian (E-C) transition, reflecting large perturbations of the carbon cycle in the ocean–atmosphere system. These negative δ13C excursions have been linked to dramatic paleoenvironmental changes and been widely used as regional and global chemostratigraphic correlation tools. However, there is still much debate about their causes and mechanisms. In this study, we report high-resolution δ13C records of both carbonate (δ13Ccarb) and organic carbon (δ13Corg) from the Meishucun section in South China. Combined with lithological variations and intrabasinal correlations, we find that the negative δ13C excursions during the E-C transition in South China are tightly linked with transgressive events. The existence of a large vertical (surface-to-deep water) δ13C gradient in a stratified ocean, and episodic incursions of 13C-depleted anoxic/euxinic deep waters into shallow water environment through enhanced upwelling or shoaling of the chemocline, may have contributed to these negative δ13C excursions. In addition, our results also imply a large reduction in the vertical δ13Corg gradient during the E-C transition, which may reflect the ventilation and oxygenation of the deep ocean. The corresponding expansion of oxic seafloor conditions and a large increase in the extent of habitable space for animals may have facilitated the radiation of metazoans during the Cambrian explosion. |
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| AbstractList | •Close link between transgressions and negative δ13C excursions during the E-C transition.•Incursion of 13C-depleted anoxic/euxinic deep waters into shallow-water environment.•Ocean stratification and vertical δ13C gradients.•Reduction of vertical δ13C gradient reflects deep ocean ventilation and oxygenation.•Deep ocean oxygenation facilitated the radiation of metazoans during the Cambrian explosion.
Several prominent negative carbon isotope (δ13C) excursions are observed during the Ediacaran-Cambrian (E-C) transition, reflecting large perturbations of the carbon cycle in the ocean–atmosphere system. These negative δ13C excursions have been linked to dramatic paleoenvironmental changes and been widely used as regional and global chemostratigraphic correlation tools. However, there is still much debate about their causes and mechanisms. In this study, we report high-resolution δ13C records of both carbonate (δ13Ccarb) and organic carbon (δ13Corg) from the Meishucun section in South China. Combined with lithological variations and intrabasinal correlations, we find that the negative δ13C excursions during the E-C transition in South China are tightly linked with transgressive events. The existence of a large vertical (surface-to-deep water) δ13C gradient in a stratified ocean, and episodic incursions of 13C-depleted anoxic/euxinic deep waters into shallow water environment through enhanced upwelling or shoaling of the chemocline, may have contributed to these negative δ13C excursions. In addition, our results also imply a large reduction in the vertical δ13Corg gradient during the E-C transition, which may reflect the ventilation and oxygenation of the deep ocean. The corresponding expansion of oxic seafloor conditions and a large increase in the extent of habitable space for animals may have facilitated the radiation of metazoans during the Cambrian explosion. |
| ArticleNumber | 105561 |
| Author | Hu, Dongping Zhou, Xin Zhang, Xiaolin |
| Author_xml | – sequence: 1 givenname: Xiaolin surname: Zhang fullname: Zhang, Xiaolin email: zhxl2012@ustc.edu.cn organization: School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China – sequence: 2 givenname: Xin surname: Zhou fullname: Zhou, Xin organization: School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China – sequence: 3 givenname: Dongping surname: Hu fullname: Hu, Dongping organization: School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China |
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| CitedBy_id | crossref_primary_10_1016_j_gca_2021_04_011 crossref_primary_10_1016_j_oregeorev_2022_105146 crossref_primary_10_1007_s11631_022_00571_w crossref_primary_10_3390_min12070876 crossref_primary_10_1111_1755_6724_14972 crossref_primary_10_1007_s11631_024_00681_7 crossref_primary_10_1016_j_gloplacha_2024_104364 crossref_primary_10_1016_j_earscirev_2022_104017 crossref_primary_10_1016_j_precamres_2021_106501 crossref_primary_10_1007_s12594_021_1736_9 crossref_primary_10_1093_nsr_nwad237 crossref_primary_10_1016_j_palaeo_2024_112281 |
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| Keywords | Vertical carbon isotope gradient Negative carbon isotope excursions Ocean stratification Yangtze Block Transgression |
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| Title | High-resolution paired carbon isotopic records from the Meishucun section in South China: Implications for carbon cycling and environmental changes during the Ediacaran-Cambrian transition |
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