豫西寒武系—苗岭界ROECE后底栖生态空间扩展的意义

IF 2
Da Li, Jian Fu, Yong-An Qi, Xi-Tong He, Man Li, Fu-Qiang Guo
{"title":"豫西寒武系—苗岭界ROECE后底栖生态空间扩展的意义","authors":"Da Li,&nbsp;Jian Fu,&nbsp;Yong-An Qi,&nbsp;Xi-Tong He,&nbsp;Man Li,&nbsp;Fu-Qiang Guo","doi":"10.1016/j.jop.2025.100256","DOIUrl":null,"url":null,"abstract":"<div><div>The transition period from the Cambrian Series 2 to Miaolingian was a pivotal juncture in Earth's history, marking the onset of significant shifts in biodiversity and biomass dynamics during the Phanerozoic. Concurrently, profound transformations occurred in the alteration of sedimentary deposits by trace makers, reshaping benthic ecological spaces. This study employs ichnological and ecological methodologies to construct a comprehensive three-dimensional spatial model for ecospace occupation and ecosystem engineering within the Mantou Formation in the western Henan Province, focusing on the transition between the Cambrian Series 2 and Miaolingian. A meticulous statistical analysis of 22 ichnogenera and 32 ichnospecies in the Mantou Formation revealed nuanced variations, such as a decrease in the proportion of predatory organisms in the lower part of Member 2 of the Mantou Formation and a corresponding increase in the upper part. Simultaneously, non-selective deposit-feeding animals exhibit an ascending trend in the lower part of Member 2 and a descending trend in the upper part of Member 2.</div><div>In terms of sediment bioturbation, the lower part of Member 2 is characterized by the exclusive presence of biodiffusors and conveyors, whereas regenerators make their appearance in the upper part of Member 2. Affected by the Redlichiid–Olenellid Extinction Carbon isotope Excursion (ROECE) event, metazoans experienced a shift in control dynamics, with microbial mats becoming dominant. Biological activities became intricately intertwined with microbial mats. In the upper part of Member 2, metazoans started recovering, concomitant with the emergence of <em>Thalassinoides</em> and <em>Treptichnus</em> substantially boasting ecosystem engineering impact (EEI) values. These trace makers rapidly amplified the depth and extent of sediment disturbance, giving rise to a profusion of novel ecological niches and catalyzing the transformation of builder functional groups.</div></div>","PeriodicalId":100819,"journal":{"name":"Journal of Palaeogeography","volume":"14 3","pages":"Article 100256"},"PeriodicalIF":2.0000,"publicationDate":"2025-07-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"The significance of benthic ecospace expansion following the ROECE at the Cambrian Series 2–Miaolingian boundary, western Henan Province, central China\",\"authors\":\"Da Li,&nbsp;Jian Fu,&nbsp;Yong-An Qi,&nbsp;Xi-Tong He,&nbsp;Man Li,&nbsp;Fu-Qiang Guo\",\"doi\":\"10.1016/j.jop.2025.100256\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>The transition period from the Cambrian Series 2 to Miaolingian was a pivotal juncture in Earth's history, marking the onset of significant shifts in biodiversity and biomass dynamics during the Phanerozoic. Concurrently, profound transformations occurred in the alteration of sedimentary deposits by trace makers, reshaping benthic ecological spaces. This study employs ichnological and ecological methodologies to construct a comprehensive three-dimensional spatial model for ecospace occupation and ecosystem engineering within the Mantou Formation in the western Henan Province, focusing on the transition between the Cambrian Series 2 and Miaolingian. A meticulous statistical analysis of 22 ichnogenera and 32 ichnospecies in the Mantou Formation revealed nuanced variations, such as a decrease in the proportion of predatory organisms in the lower part of Member 2 of the Mantou Formation and a corresponding increase in the upper part. Simultaneously, non-selective deposit-feeding animals exhibit an ascending trend in the lower part of Member 2 and a descending trend in the upper part of Member 2.</div><div>In terms of sediment bioturbation, the lower part of Member 2 is characterized by the exclusive presence of biodiffusors and conveyors, whereas regenerators make their appearance in the upper part of Member 2. Affected by the Redlichiid–Olenellid Extinction Carbon isotope Excursion (ROECE) event, metazoans experienced a shift in control dynamics, with microbial mats becoming dominant. Biological activities became intricately intertwined with microbial mats. In the upper part of Member 2, metazoans started recovering, concomitant with the emergence of <em>Thalassinoides</em> and <em>Treptichnus</em> substantially boasting ecosystem engineering impact (EEI) values. These trace makers rapidly amplified the depth and extent of sediment disturbance, giving rise to a profusion of novel ecological niches and catalyzing the transformation of builder functional groups.</div></div>\",\"PeriodicalId\":100819,\"journal\":{\"name\":\"Journal of Palaeogeography\",\"volume\":\"14 3\",\"pages\":\"Article 100256\"},\"PeriodicalIF\":2.0000,\"publicationDate\":\"2025-07-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Palaeogeography\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S2095383625000628\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Palaeogeography","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S2095383625000628","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0

摘要

从寒武纪二系到苗岭期的过渡时期是地球历史上的一个关键时期,标志着显生宙生物多样性和生物量动态的重大转变。与此同时,痕迹制造者对沉积物的改造也发生了深刻的变化,重塑了底栖生态空间。本文采用技术和生态学方法,以寒武纪二系与苗岭期过渡带为研究对象,构建了豫西地区满头组生态空间占用与生态系统工程的三维综合空间模型。通过对曼头组22个鱼属和32个鱼种的精细统计分析,发现了曼头组二段下部捕食生物比例下降,上部捕食生物比例相应增加的细微变化。同时,非选择性沉积饲养动物在2段下部呈上升趋势,在2段上部呈下降趋势。在沉积物生物扰动方面,第二段下部的特征是生物扩散器和传送带的专属存在,而再生器则出现在第二段上部。受Redlichiid-Olenellid灭绝碳同位素偏移(ROECE)事件的影响,后生动物经历了控制动力学的转变,微生物席成为主导。生物活动与微生物席错综复杂地交织在一起。在成员2的上部,后生动物开始恢复,同时出现了具有生态系统工程影响(EEI)值的Thalassinoides和Treptichnus。这些痕迹制造者迅速扩大了沉积物扰动的深度和程度,产生了大量新的生态位,并催化了建造者功能群的转变。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The significance of benthic ecospace expansion following the ROECE at the Cambrian Series 2–Miaolingian boundary, western Henan Province, central China
The transition period from the Cambrian Series 2 to Miaolingian was a pivotal juncture in Earth's history, marking the onset of significant shifts in biodiversity and biomass dynamics during the Phanerozoic. Concurrently, profound transformations occurred in the alteration of sedimentary deposits by trace makers, reshaping benthic ecological spaces. This study employs ichnological and ecological methodologies to construct a comprehensive three-dimensional spatial model for ecospace occupation and ecosystem engineering within the Mantou Formation in the western Henan Province, focusing on the transition between the Cambrian Series 2 and Miaolingian. A meticulous statistical analysis of 22 ichnogenera and 32 ichnospecies in the Mantou Formation revealed nuanced variations, such as a decrease in the proportion of predatory organisms in the lower part of Member 2 of the Mantou Formation and a corresponding increase in the upper part. Simultaneously, non-selective deposit-feeding animals exhibit an ascending trend in the lower part of Member 2 and a descending trend in the upper part of Member 2.
In terms of sediment bioturbation, the lower part of Member 2 is characterized by the exclusive presence of biodiffusors and conveyors, whereas regenerators make their appearance in the upper part of Member 2. Affected by the Redlichiid–Olenellid Extinction Carbon isotope Excursion (ROECE) event, metazoans experienced a shift in control dynamics, with microbial mats becoming dominant. Biological activities became intricately intertwined with microbial mats. In the upper part of Member 2, metazoans started recovering, concomitant with the emergence of Thalassinoides and Treptichnus substantially boasting ecosystem engineering impact (EEI) values. These trace makers rapidly amplified the depth and extent of sediment disturbance, giving rise to a profusion of novel ecological niches and catalyzing the transformation of builder functional groups.
求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术官方微信