豫西登封地区寒武系第二统朱砂洞组生物扰动构造及其地球化学特征

庆国帅; 齐永安; 杨文涛; 代明月; 白万备; 樊钰超; 刘炳辰

doi:10.3799/dqkx.2019.136

Volume 45 Issue 4

Apr. 2020

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Article Navigation > Earth Science > 2020 > 45(4): 1103-1114

Qing Guoshuai, Qi Yong'an, Yang Wentao, Dai Mingyue, Bai Wanbei, Fan Yuchao, Liu Bingchen, 2020. Bioturbated Structures and Their Geochemical Features from the Zhushadong Formation of the Cambrian Series 2 in Dengfeng Area of West Henan. Earth Science, 45(4): 1103-1114. doi: 10.3799/dqkx.2019.136

Citation:

Qing Guoshuai, Qi Yong'an, Yang Wentao, Dai Mingyue, Bai Wanbei, Fan Yuchao, Liu Bingchen, 2020. Bioturbated Structures and Their Geochemical Features from the Zhushadong Formation of the Cambrian Series 2 in Dengfeng Area of West Henan. Earth Science, 45(4): 1103-1114. doi: 10.3799/dqkx.2019.136

Citation:

Qing Guoshuai, Qi Yong'an, Yang Wentao, Dai Mingyue, Bai Wanbei, Fan Yuchao, Liu Bingchen, 2020. Bioturbated Structures and Their Geochemical Features from the Zhushadong Formation of the Cambrian Series 2 in Dengfeng Area of West Henan. Earth Science, 45(4): 1103-1114. doi: 10.3799/dqkx.2019.136

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Bioturbated Structures and Their Geochemical Features from the Zhushadong Formation of the Cambrian Series 2 in Dengfeng Area of West Henan

doi: 10.3799/dqkx.2019.136

School of Resources and Environment, Henan Polytechnic University, Jiaozuo 454000, China

Received Date: 2019-06-06
Publish Date: 2020-04-15

Abstract

Abstract

The bioturbation plays a critical role in modern marine biogeochemical cycling. It influences the character of benthic communities, decomposition rate of organic matter, chemical properties of seawater, redox properties of sediment and nutrient recycling. Abundant bioturbated structures dominated by Thalassinoides occur in carbonate rocks of the Cambrian Series 2 Zhushadong Formation in Dengfeng area of west Henan. The determination of carbon and nitrogen isotopes can help us to understand the influence of bioturbators reworking to sediment biogeochemical cycling. The determination results show that there is a great difference of δ¹³C_carb value between the Thalassinoides burrow fillings and matrix, and it also displays a dramatic difference in different bioturbated intensity. But there exists a weak difference of δ¹³C_org and δ¹⁵N values between the Thalassinoides burrow fillings and matrix. The results mean that the sediment reworking of bioturbation can greatly change the redox property, porosity and permeability of sediments. The changes may be related to the decrease of the proportion of authigenic carbonates caused by the increase of oxygen content in sediment pore water and enhancement of dolomitization during diagenesis. The sediment mixing and reworking formed by Thalassinoides bioturbators not only have significantly changed the primary physical and chemical information and promoted the biogeochemical cycle between seawater and sediments, but also may have efficiently triggered the substrate revolution, acting as ecosystem engineers as well.
- Thalassinoides,
- bioturbated structure,
- biogeochemical cycling,
- carbon isotope,
- Zhushadong Formation,
- sediments

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References(51)

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