扬子板块西北缘下泥盆统平驿铺组双壳类遗迹化石<sup>&#x0002A;</sup>

doi:10.7605/gdlxb.2023.02.024

古地理学报 ›› 2023, Vol. 25 ›› Issue (2): 392-404. doi: 10.7605/gdlxb.2023.02.024

• 生物古地理学及古生态学 • 上一篇下一篇

扬子板块西北缘下泥盆统平驿铺组双壳类遗迹化石^*

张小乐^1,2, 王怿¹, 刘建波³, 黄璞¹, 徐洪河¹

1 现代古生物学和地层学国家重点实验室,中国科学院南京地质古生物研究所,江苏南京 210008;
2 生物地质与环境地质国家重点实验室,中国地质大学(武汉),湖北武汉 430074;
3 北京大学地球与空间科学学院,北京 100871

收稿日期:2022-08-27 修回日期:2022-10-24 出版日期:2023-04-01 发布日期:2023-04-14
作者简介:张小乐,男,1986年生,中国科学院南京地质古生物研究所助理研究员,研究方向为沉积学、遗迹学。E-mail: xlzh@nigpas.ac.cn。
基金资助:
*中国科学院南京地质古生物研究所现代古生物学和地层学国家重点实验室项目(编号: 20192112),中国地质大学(武汉)生物地质与环境地质国家重点实验室项目(编号:GBL22002),中国科学院战略性先导科技专项(编号: XDB26000000)以及国家自然科学基金项目(编号: 42172003)共同资助

Bivalvian trace fossils from the Lower Devonian Pingyipu Formation in northwestern Yangtze Platform

ZHANG Xiaole^1,2, WANG Yi¹, LIU Jianbo³, HUANG Pu¹, XU Honghe¹

1 State Key Laboratory of Palaeobiology and Stratigraphy,Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences,Nanjing 210008,China;
2 State Key Laboratory of Biogeology and Environmental Geology,China University of Geosciences(Wuhan),Wuhan 430074,China;
3 School of Earth and Space Sciences,Peking University,Beijing 100871,China

Received:2022-08-27 Revised:2022-10-24 Online:2023-04-01 Published:2023-04-14
About author:ZHANG Xiaole,born in 1986,is an assistant research fellow in Nanjing Institute of Geology and Palaeontology,Chinese Academy of Sciences. He is engaged in sedimentology and ichnology. E-mail: xlzh@nigpas.ac.cn.
Supported by:
State Key Laboratory of Palaeobiology and Stratigraphy of Nanjing Institute of Geology and Palaeontology,Chinese Academy of Sciences(No.20192112),the State Key Laboratory of Biogeology and Environmental Geology,China University of Geosciences(Wuhan)(No. GBL22002),the Strategic Priority Program of CAS(No. XDB26000000),and the National Natural Science Foundation of China(No.42172003)]

摘要/Abstract

摘要： 四川北部广元地区下泥盆统平驿铺组产出丰富的双壳类遗迹化石,但尚未开展过系统的遗迹学工作,也未进行过行为学与古生态学分析。文中针对四川广元马家剖面平驿铺组中部地层开展沉积学和系统遗迹学研究,在陆棚至近滨带下部沉积中共识别出3个属种的双壳类遗迹化石,包括Lockeia siliquaria,Protovirgularia rugosa, Ptychoplasma vagans,以及其他无脊椎动物门类遗迹化石Cruziana problematica,Dimorphichnus isp.,Lophoctenium isp.等。对双壳类遗迹化石的出现方式、形态以及保存特征的分析表明,平驿铺组中部曾出现过2种类型的双壳类,分属具分叉足(原鳃目)和楔状足的类群。原鳃目分布于过渡带和陆棚区,营沉积物摄食生活; 受高能事件或沉积物掩埋影响,它们由停息状态变为“逃逸”状态的行为产生了Pro. rugosa。具楔状足的双壳类依生态类型可分为2类: 在过渡带与陆棚区,漫游的、营沉积物摄食的类型产生了Pty. vagans;而在近滨下部,滤食性双壳类居群则在不同期次高能事件的间隙对沉积物进行大规模殖居,产生了L. siliquaria。平驿铺组中部遗迹群落面貌的垂向变化,反映了随着浅海环境水动力增强,发育在具有一定硬度基底的Cruziana遗迹相被Skolithos遗迹相逐渐替代的过程。本研究强调,通过对双壳类遗迹化石的出现形式、保存和形态的精细观察,可以对造迹生物类群、古生态学和行为习性学特征等进行可靠的解释。

关键词: 古生态学, 行为学, 古环境, 双壳类, 遗迹化石

Abstract: Abundant bivalve trace fossils are found in the Lower Devonian Pingyipu Formation in Guangyuan area,northern Sichuan Province,but systematic ichnological work and behavioral and paleoecological analysis have not been carried out. Close observations on the occurrence,preservation style and morphological features of bivalvian traces provide invaluable information to guide the interpretation of their trace maker,ethological and paleoecological features. Here we carried out sedimentary and systematic ichnology studies on the middle part of the Lower Devonian Pingyipu Formation at the Majia section,Guangyuan area. The results suggest occurrence of bivalvian trace fossils,including Lockeia siliquaria,Protovirgularia rugosa, Ptychoplasma vagans as well as trace fossils of other invertebrate groups such as Cruziana problematica, Dimorphichnus isp.,and Lophoctenium isp. in the lower shoreface to off shore settings. The overall morphological and taphonomic features of the trace fossils suggest that,two major groups,including the cleft-footed(protobranchia)and wedge-footed bivalves occurred in the middle part of the Pingyipu Formation. The protobranchia were deposit-feeding bivalves distributed in the transitional zone and off shore settings. The transition from resting to “escape”state of these bivalves,probably due to erosive events or a higher sedimentation rates,produced the trace fossil Pro. rugosa. The wedge-footed bivalves could be further divided into two groups. The vagile,deposit-feeding type occupied the transitional zone and off shore settings. Their crawling behavior,probably linked to an effort to search for edible material from the sediment generated the trace fossil Pty. vagans. While in the lower shoreface setting,colonies of suspension-feeding bivalves colonized the sediment during relatively tranquil intervals between erosional events. The vertical transition of trace fossil composition in the middle Pingyipu Formation suggests a substitution of Cruziana ichnofacies developed on a relative stiff substrate by the latter Skolithos ichnofacies in an upward shallowing succession.

Key words: paleoecology, ethology, paleoenvironment, bivalve, ichnofossils

中图分类号:

Q911.28

张小乐, 王怿, 刘建波, 黄璞, 徐洪河. 扬子板块西北缘下泥盆统平驿铺组双壳类遗迹化石^*[J]. 古地理学报, 2023, 25(2): 392-404.

ZHANG Xiaole, WANG Yi, LIU Jianbo, HUANG Pu, XU Honghe. Bivalvian trace fossils from the Lower Devonian Pingyipu Formation in northwestern Yangtze Platform[J]. JOPC, 2023, 25(2): 392-404.

http://www.gdlxb.cn/CN/Y2023/V25/I2/392

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扬子板块西北缘下泥盆统平驿铺组双壳类遗迹化石^*

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扬子板块西北缘下泥盆统平驿铺组双壳类遗迹化石*

Bivalvian trace fossils from the Lower Devonian Pingyipu Formation in northwestern Yangtze Platform

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扬子板块西北缘下泥盆统平驿铺组双壳类遗迹化石^*