ABSTRACT
Keywords:
Early Ordovician, stromatoporoid, South China, reef, Great Ordovician Biodiversification Event
Stromatoporoid-type hypercalcified sponges are known to have contributed to the global reef system since the late Middle Ordovician until their major disappearance in the latest Devonian. However, the timing of their appearance and how the earliest stromatoporoids were incorporated into the reef ecosystem remains a mystery. A stromatoporoid taxon was previously reported from the lower Floian of South China, but this example limitedly occurs within the cryptic space of a lithistid-Calathium reef and has negligible importance in reef construction, unlike the later stromatoporoids that formed the major reef frameworks during the Palaeozoic.
In this study, we describe the earliest known definitive stromatoporoids and the reefs constructed by them in the upper Tremadocian to the lower Floian of South China. The reef framework is dominated by various growth forms of stromatoporoids - ranging from laminar, domical, bulbous to digitate morphologies - that alternate with other organisms such as the calcimicrobe Girvanella and stalked echinoderms. Stromatoporoids have played a significant role in frame-building and binding associated with other reef components, contributing to the construction of a complex reef community similar to those found in the late Middle Ordovician and onwards.
In South China, late Cambrian microbial-dominant reefs were rapidly substituted by newly-emerging metazoan reef-builders in the Early Ordovician, such as lithistid sponges, quasi-sponge Calathium, bryozoans, echinoderms, the problematic Pulchrilamina and stromatoporoids. This is in contrast to other palaeocontinents where lithistid-microbial reefs dominated throughout the late Cambrian and Early Ordovician, with Calathium being incorporated in the Early Ordovician. This finding supports the idea that there was regional heterogeneity in reef evolution during this critical time of the Great Ordovician Biodiversification Event.
Received 28 March 2023
Accepted 31 March 2023
Available online 14 June 2023
Corresponding author:
Juwan Jeon
Citation:
Jeon, J., Lee, J.-H., Kershaw, S., Chen, Z.-Y., Ma, J.-Y., Liang, K. and Zhang, Y.-D. 2023. The earliest known stromatoporoid and its contribution to reef construction. Estonian Journal of Earth Sciences, 72(1), 135. https://doi.org/10.3176/earth.2023.05
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Abstract
Stromatoporoid-type hypercalcified sponges are known to have contributed to the global reef system since the late Middle Ordovician until their major disappearance in the latest Devonian. However, the timing of their appearance and how the earliest stromatoporoids were incorporated into the reef ecosystem remains a mystery. A stromatoporoid taxon was previously reported from the lower Floian of South China, but this example limitedly occurs within the cryptic space of a lithistid-Calathium reef and has negligible importance in reef construction, unlike the later stromatoporoids that formed the major reef frameworks during the Palaeozoic. In this study, we describe the earliest known definitive stromatoporoids and the reefs constructed by them in the upper Tremadocian to the lower Floian of South China. The reef framework is dominated by various growth forms of stromatoporoids - ranging from laminar, domical, bulbous to digitate morphologies - that alternate with other organisms such as the calcimicrobe Girvanella and stalked echinoderms. Stromatoporoids have played a significant role in frame-building and binding associated with other reef components, contributing to the construction of a complex reef community similar to those found in the late Middle Ordovician and onwards. In South China, late Cambrian microbial-dominant reefs were rapidly substituted by newly-emerging metazoan reef-builders in the Early Ordovician, such as lithistid sponges, quasi-sponge Calathium, bryozoans, echinoderms, the problematic Pulchrilamina and stromatoporoids. This is in contrast to other palaeocontinents where lithistid-microbial reefs dominated throughout the late Cambrian and Early Ordovician, with Calathium being incorporated in the Early Ordovician. This finding supports the idea that there was regional heterogeneity in reef evolution during this critical time of the Great Ordovician Biodiversification Event.
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Details
1 State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China
2 Department of Geological Sciences, Chungnam National University, Daejeon 34134, Republic of Korea
3 Department of Life Sciences, Brunel University, Kingston Lane, Uxbridge, UB8 3PH, UK