Coralliths of tabulate corals from the Devonian of the Holy Cross Mountains (Poland)

Zapalski, Mikołaj K., Król, Jan J., Halamski, Adam T., Wrzołek, Tomasz, Rakociński, Michał, and Baird, Andrew H. (2022) Coralliths of tabulate corals from the Devonian of the Holy Cross Mountains (Poland). Palaeogeography, Palaeoclimatology, Palaeoecology, 585. 110745.

[img]
Preview
PDF (Published Version) - Published Version
Available under License Creative Commons Attribution.

Download (11MB) | Preview
View at Publisher Website: https://doi.org/10.1016/j.palaeo.2021.11...
 
7
515


Abstract

Tabulates, an extinct Palaeozoic group of corals, developed diverse colony morphologies during the Silurian to Devonian peak of reef development. Coralliths, or circumrotatory colonies, are passively motile coral colonies constantly overturned by wave action or currents. Such overturning allows tissue growth on all sides of the colony. They are among the most rarely reported growth forms. Recent corallith-forming scleractinian corals mostly inhabit the shallowest reef environments, but coralliths can also develop at greater depths in areas of low topographic relief, unconsolidated substratum, low coral cover and high water movement. Here, we report on Devonian (Givetian Favosites goldfussi and Frasnian Alveolites? tenuissimus) coralla from the Holy Cross Mountains, Poland. Our analysis suggests these colonies are coralliths, although less mature than usually reported. These corals, unlike previously described growth forms of this kind, lived in relatively deep environments: probably the upper mesophotic (Givetian, Miłoszów), or deep reef fore-slope (Frasnian, Jaźwica and Kowala). Microfacies analysis of the Jaźwica site suggests unconsolidated substratum and high hydrodynamic energy. We conclude that these corals lived in deeper environments where bottom currents caused their autorotation. A good modern analogue for such a corallith-forming environment is the Wistari Channel (Southern Great Barrier Reef), where bottom tidal currents at nearly 30 m of depth are strong enough to overturn colonies of Stylocoeniella cf. guentheri reaching 15 cm in diameter. Our discovery shows that the spectrum of coral growth forms during the Devonian peak of reef development was broader than previously assumed, and that tabulate corals displayed numerous adaptive strategies to various environments.

Item ID: 74812
Item Type: Article (Research - C1)
ISSN: 1872-616X
Keywords: Frasnian, Givetian, Heron Island, Mesophotic, Reef fore-slope
Copyright Information: © 2021 The Authors. Published by Elsevier B.V. This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/4.0/).
Funders: Australian Research Council (ARC)
Date Deposited: 12 Dec 2022 04:38
FoR Codes: 37 EARTH SCIENCES > 3705 Geology > 370501 Biomineralisation @ 80%
31 BIOLOGICAL SCIENCES > 3109 Zoology > 310913 Invertebrate biology @ 20%
SEO Codes: 28 EXPANDING KNOWLEDGE > 2801 Expanding knowledge > 280102 Expanding knowledge in the biological sciences @ 40%
28 EXPANDING KNOWLEDGE > 2801 Expanding knowledge > 280107 Expanding knowledge in the earth sciences @ 60%
Downloads: Total: 515
Last 12 Months: 90
More Statistics

Actions (Repository Staff Only)

Item Control Page Item Control Page