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Trace Fossil Thalassinoides and Its Paleoenvironmental Factors from the Cambrian in Henan Province
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Min WANG1, 2, Dan XIONG1, YongAn QI1, 2, WenTao YANG1, 2, KeJia FENG1
Acta Sedimentologica Sinica | 2026, 44(3) : 1019 - 1030
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Acta Sedimentologica Sinica | 2026, 44(3): 1019-1030
Trace Fossil Thalassinoides and Its Paleoenvironmental Factors from the Cambrian in Henan Province
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Min WANG1, 2, Dan XIONG1, YongAn QI1, 2, WenTao YANG1, 2, KeJia FENG1
Affiliations
  • 1.Institute of Resource and Environment, Henan Polytechnic University, Jiaozuo, Henan 454003, China
  • 2.Henan International Joint Laboratory of Biogenic Traces and Sedimentary Minerals, Jiaozuo, Henan 454003, China
Published: 2026-06-10 doi: 10.14027/j.issn.1000-0550.2024.127
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Objective A large number of Thalassinoides trace fossils developed in the Cambrian strata of Henan province. We studied the morphology and distribution characteristics of different ichnospecies and analyzed the sedimentary environment-controlling factors. Methods Based on lithology and ichnography, the morphology, size, disturbance depth, and disturbance intensity of Thalassinoides in this area were combined with sedimentary environment parameters. Results The dense network Thalassinoides suevicus featuresY-shaped branches with enlarged intersections, developed in the intertidal zone where water is turbulent and oxygen is abundant. Sparse Thalassinoides horizontalis Type 1, which is Y-shaped long branches with large diameters, formed in the shallow water area in front of the oolitic beach with abundant oxygen and nutrients due to water turbulence. Thalassinoides horizontalis Type 2, T-shaped short branches with smaller diameters, occurred in deeper waters on the seaward side in front of the oolitic beach. The three-dimensional, boxwork burrows of Thalassinoides bacae, featuring vertical tubes, branches, and thick lining walls, developed in interbeach-confined seas and deep subtidal zones where oxygen and nutrients were deficient. Conclusions The variation in different ichnospecies and morphologies of Thalassinoides is controlled by factors such as water depth, water kinetic energy, nutrients, and oxygen content of the sedimentary environment. The trace maker adopted different strategies to cope with the changing sedimentary environment.

Cambrian  /  carbonate platform  /  bioturbation  /  sedimentary environment
Min WANG, Dan XIONG, YongAn QI, WenTao YANG, KeJia FENG. Trace Fossil Thalassinoides and Its Paleoenvironmental Factors from the Cambrian in Henan Province[J]. Acta Sedimentologica Sinica, 2026 , 44 (3) : 1019 -1030 . DOI: 10.14027/j.issn.1000-0550.2024.127
  • National Natural Science Foundation of China(42272130)
Year 2026 volume 44 Issue 3
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doi: 10.14027/j.issn.1000-0550.2024.127
  • Receive Date:2024-10-22
  • Online Date:2026-09-17
  • Published:2026-06-10
Article Data
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History
  • Received:2024-10-22
  • Revised:2024-11-29
  • Accepted:2025-01-08
Funding
National Natural Science Foundation of China(42272130)
Affiliations
    1.Institute of Resource and Environment, Henan Polytechnic University, Jiaozuo, Henan 454003, China
    2.Henan International Joint Laboratory of Biogenic Traces and Sedimentary Minerals, Jiaozuo, Henan 454003, China
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表12种不同金属材料的力学参数

Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)

Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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