[1] 冯增昭，陈继新，吴胜和. 1989. 华北地台早古生代岩相古地理[J]. 沉积学报，7（4）：15-55.

Feng Zengzhao, Chen Jixin, Wu Shenghe. 1989. Lithofacies paleogeography of Early Paleozoic of North China Platform[J]. Acta Sedimentologica Sinica, 7(4): 15-55.
[2] 冯增昭，彭勇民，金振奎，等. 2002. 中国中寒武世岩相古地理[J]. 古地理学报，4（2）：1-11.

Feng Zengzhao, Peng Yongmin, Jin Zhenkui, et al. 2002. Lithofacies palaeogeography of the middle Cambrian in China[J]. Journal of Palaeogeography, 4(2): 1-11.
[3] 冯增昭，彭勇民，金振奎，等. 2004. 中国寒武纪和奥陶纪岩相古地理[M]. 北京：石油工业出版社：1- 200.

Feng Zengzhao, Peng Yongmin, Jin Zhenkui, et al. 2004.Lithofacies paleogeography of the Cambrian and Ordovician in China[M]. Beijing: Petroleum Industry Press: 1-200.
[4] 李凯楠，王敏，齐永安，等.2019. 豫西寒武系苗岭统张夏组Thalassinoides bacae中莓状黄铁矿的成因及其生态学意义[J]. 古生物学报，58（4）：445-455.

Li Kainan, Wang Min, Qi Yong'an, et al. 2019. Framboidal pyrites in Thalassinoides bacae from the Zhangxia Formation (Cambrian Miaolingian series) in Henan pro-vince: Genesis and its ecological significance[J]. Acta Palaeontologica Sinica, 58(4): 445-455.
[5] 罗茂，龚一鸣，张立军，等. 2021. 遗迹化石：探索生物与环境相互作用的重要信息载体[J]. 古生物学报，60（3）：347-356.

Luo Mao, Gong Yiming, Zhang Lijun, et al. 2021. Trace fossil: A significant agent for exploring organism-environment interactions[J]. Acta Palaeontologica Sinica, 60(3): 347-356.
[6] 牟传龙，周恳恳，陈小炜，等. 2016. 中国岩相古地理图集（埃迪卡拉纪—志留纪）[M]. 北京：地质出版社：1- 154.

Mou Chuanlong, Zhou Kenken, Chen Xiaowei, et al. 2016. Atlas of lithofacies and paleogeography of China (Ediacaran-Silurian)[M]. Beijing: Geological Publishing House: 1-154.
[7] 裴放. 2000. 河南省华北型寒武纪生物地层单位划分与对比[J]. 河南地质，18（2）：97-106.

Pei Fang. 2000. Division and correlation of the North China type Cambrian biostratigraphic units of Henan province[J]. Henan Geology, 18(2): 97-106.
[8] 裴放，张海清，阎国顺，等. 2008. 河南省地层古生物研究（第三分册）早古生代（华北型）[M]. 郑州：黄河水利出版社：1- 302.

Pei Fang, Zhang Haiqing, Yan Guoshun, et al. 2008. The third Paleozoic study of stratigraphic paleontology in Henan province, Early Paleozoic (North China)[M]. Zhengzhou: Yellow River Water Conservancy Publishing House: 1-302.
[9] 彭勇民，张荣强，陈霞，等. 2012. 四川盆地南部中下寒武统石膏岩的发现与油气勘探[J]. 成都理工大学学报（自然科学版），39（1）：63-69.

Peng Yongmin, Zhang Rongqiang, Chen Xia, et al. 2012. Dis-covery and significance of the middle-lower Cambrian gypsolith in the south of Sichuan Basin, China[J]. Journal of Chengdu University of Technology (Science & Technology Edition), 39(1): 63-69.
[10] 齐永安，王敏，李妲，等. 2012. 寒武纪底质革命：从微生物席底到生物扰动混合底[J]. 河南理工大学学报（自然科学版），31（2）：159-164.

Qi Yong'an, Wang Min, Li Da, et al. 2012. Cambrian substrate revolution: From matgrounds to bioturbated mixgrounds[J]. Journal of Henan Polytechnic University (Natural Science), 31(2): 159-164.
[11] 许晴旸，范若颖，龚一鸣. 2023. 海相遗迹化石对显生宙生物大辐射事件的响应[J]. 古地理学报，2023，25（2）：431-450.

Xu Qingyang, Fan Ruoying, Gong Yiming. 2023. Marine ichnofossils as a record of major biodiversification events in the Phanerozoic[J]. Journal of Palaeogeography, 25(2): 431-450.
[12] 朱茂炎，杨爱华，袁金良，等. 2019. 中国寒武纪综合地层和时间框架[J]. 中国科学：地球科学，49（1）：26-65.

Zhu Maoyan, Yang Aihua, Yuan Jinliang, et al. 2019. Cambrian integrative stratigraphy and timescale of China[J]. Science China Earth Sciences, 49(1): 26-65.
[13] Bromley R G, Ekdale A A. 1984. Trace fossil preservation in flint in the European chalk[J]. Journal of Paleontology, 58(2): 298-311.
[14] Buatois L A, Mángano M G. 2004. Animal-substrate interactions in freshwater environments: Applications of ichnology in facies and sequence stratigraphic analysis of fluvio-lacustrine successions[J]. Geological Society, London, Special Publications, 228(1): 311-333.
[15] Buatois L A, Mángano M G. 2011. Ichnology: Organism-substrate interactions in space and time[M]. Cambridge: Cambridge University Press: 1-358.
[16] Carmona N B, Buatois L A, Mángano M G. 2004. The trace fossil record of burrowing decapod crustaceans: Evaluating evolutionary radiations and behavioural convergence[J]. Fossils and Strata, 51: 141-153.
[17] Droser M L, Bottjer D J. 1986. A semiquantitative field classification of ichnofabric[J]. Journal of Sedimentary Research, 56(4): 558-559.
[18] Dworschak P C, Rodrigues S D A. 1997. A modern analogue for the trace fossil Gyrolithes: Burrows of the thalassinidean shrimp Axianassa australis [J]. Lethaia, 30(1): 41-52.
[19] Ekdale A A, Bromley R G. 2003. Paleoethologic interpretation of complex Thalassinoides in shallow-marine limestones, Lower Ordovician, southern Sweden[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 192(1/2/3/4): 221-227.
[20] Ekdale A A, Lamond R E. 2003. Behavioral cladistics of trace fossils: Evolution of derived trace-making skills[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 192(1/2/3/4): 335-343.
[21] El-Sabbagh A, El-Hedeny M, Al Farraj S. 2017. Thalassinoides in the Middle Miocene succession at Siwa Oasis, northwestern Egypt[J]. Proceedings of the Geologists' Association, 128(2): 222-233.
[22] Erwin D H. 2008. Macroevolution of ecosystem engineering, niche construction and diversity[J]. Trends in Ecology & Evolution, 23(6): 304-310.
[23] Feng X Q, Chen Z Q, Benton M J, et al. 2019. A diverse trackway-dominated marine ichnoassemblage from the Lower Triassic in the northern Paleotethys: Ichnology and implications for biotic reco-very[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 519: 124-140.
[24] Griffis R B, Suchanek T H.1991. A model of burrow architecture and trophic modes in thalassinidean shrimp (Decapoda: Thalassinidea)[J]. Marine Ecology Progress Series, 79: 171-183.
[25] Jin J S, Harper D A T, Cocks L R M, et al. 2013. Precisely locating the Ordovician equator in Laurentia[J]. Geology, 41(2): 107-110.
[26] Jin J S, Harper D A T, Rasmussen J A, et al. 2012. Late Ordovician massive-bedded Thalassinoides ichnofacies along the palaeoequator of Laurentia[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 367/368: 73-88.
[27] Joseph J K, Patel S J, Bhatt N Y. 2012. Trace fossil assemblages in mixed siliciclastic-carbonate sediments of the Kaladongar Formation (Middle Jurassic), Patcham Island, Kachchh, western India[J]. Journal of the Geological Society of India, 80(2): 189-214.
[28] Knaust D. 2021. Balanoglossites-burrowed firmgrounds:The most common ichnofabric on earth?[J]. Earth-Science Reviews, 220: 103747.
[29] Knaust D. 2024. The trace fossil Thalassinoides paradoxicus Kennedy, 1967 revisited from its type locality (Albian-Cenomanian chalk, SE England)[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 634: 111913.
[30] Knaust D, Bromley R G. 2012. Trace fossils as indicators of sedimentary environments[M]. Amsterdam: Elsevier Science: 1-924.
[31] Leonowicz P. 2015. Ichnofabrics of shallow-marine mudstone, the result of changing environmental conditions: An example from the Middle Jurassic ore-bearing clay from southern Poland[J]. Facies, 61(3): 11.
[32] Liu B C, Qi Y A, Wang M, et al. 2024. Thalassinoides ichnofabrics from the Zhangxia Formation (Cambiran Miaolingian series) in Henan province: Bioturbators as Ecosystem engineers[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 640: 112103.
[33] Marusin V V, Kochnev B B, Izokh O P. 2022. Thalassinoides and Olenichnus in the Terreneuvian carbonates of the Igarka uplift, NW Siberian Platform[J]. Lethaia, 55(2): 1-17.
[34] McIlroy D, Logan G A. 1999. The impact of bioturbation on infaunal ecology and evolution during the Proterozoic-Cambrian transition[J]. Palaios, 14(1): 58-72.
[35] Rodríguez-Tovar F J, Miguez-Salas O, Duarte L V. 2017. Toarcian Oceanic Anoxic Event induced unusual behaviour and palaeobiological changes in Thalassinoides tracemakers[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 485: 46-56.
[36] Scholle P A, Ulmer-Scholle D S. 2003. A color guide to the petrography carbonate rocks: Grains, textures, porosity, diagenesis[M]. Tulsa: American Association of Petroleum Geologists: 1-459.
[37] Seilacher A. 2007. Trace fossil analysis[M]. Berlin: Springer: 1-226.
[38] Sharafi M, Ashuri M, Mahboubi A, et al. 2012. Stratigraphic application of Thalassinoides ichnofabric in delineating sequence stratigraphic surfaces (Mid-Cretaceous), Kopet-Dagh Basin, northeastern Iran[J]. Palaeoworld, 21(3/4): 202-216.
[39] Sheehan P M, Schiefelbein D R J. 1984. The trace fossil Thalassinoides from the Upper Ordovician of the eastern Great Basin: Deep burrowing in the Early Paleozoic[J]. Journal of Paleontology, 58(2): 440-447.
[40] Solan M, Kennedy R. 2002. Observation and quantification of in situ animal-sediment relations using time-lapse sediment profile imagery (t-SPI)[J]. Marine Ecology Progress Series, 228: 179-191.
[41] Taylor A, Goldring R, Gowland S. 2003. Analysis and application of ichnofabrics[J]. Earth-Science Reviews, 60(3/4): 227-259.
[42] Torsvik T H, Cocks L R M. 2019. The integration of palaeomagnetism, the geological record and mantle tomography in the location of ancient continents[J]. Geological Magazine, 156(2): 242-260.
[43] Uchman A, Wetzel A. 2012. Deep-sea fans[J]. Developments in Sedimentology, 64: 643-671.
[44] Wang M, Li K N, Yang W T, et al. 2019. The trace fossil Thalassinoides bacae in the Cambrian Zhangxia Formation (Miaolingian series) of North China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 534: 109333.
[45] Wetzel A, Rodríguez-Tovar F J. 2021. Preface: Ichnology, trace fossils and depositional environments[J]. Palaeogeography, Palaeo-climatology, Palaeoecology, 565: 110220.
[46] Zhang X L, Wang Y, Wang Y X. 2024. Widespread Thalassinoides facies from the Upper Silurian of South China: A case study from the northwestern Hunan province, Middle to Upper Yangtze Block[J]. Palaeoworld, 33(6): 1545-1563.