In vivo and post-mortem bioerosion traces in solitary corals from the upper Pliocene deposits of Tunisia
The polychaete borings Caulostrepsis taeniola, Caulostrepsis cretacea, Caulostrepsis avipes, Caulostrepsis penicillus isp. nov., Maeandropolydora elegans, Maeandropolydora sulcans, Sulcichnus sigillum, the bryozoan boring Pinaceocladichnus onubensis and the phoronid boring Talpina cf. hackberryens...
| Main Authors: | , , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Institute of Paleobiology PAS
2023-12-01
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| Series: | Acta Palaeontologica Polonica |
| Subjects: | |
| Online Access: | https://www.app.pan.pl/archive/published/app68/app010952023.pdf |
| Summary: | The polychaete borings Caulostrepsis taeniola, Caulostrepsis cretacea, Caulostrepsis avipes, Caulostrepsis penicillus
isp. nov., Maeandropolydora elegans, Maeandropolydora sulcans, Sulcichnus sigillum, the bryozoan boring
Pinaceocladichnus onubensis and the phoronid boring Talpina cf. hackberryensis occur in coralla of the solitary scleractinian
coral Ceratotrochus (Edwardsotrochus) duodecimcostatus in the upper Pliocene middle/lower neritic to upper
bathyal fine-grained deposits of NE Tunisia. This very rich assemblage of borings is produced in vivo as suggested by
(i) their occurrence close to the surface and mostly in the upper part of coralla (Caulostrepsis ispp., M. elegans), even if
they are known to penetrate deeply in the substrate, or (ii) evidence of corallum deformation in response to the boring
action (Sulcichnus sulcans). The remaining borings were probably produced post mortem; they penetrate deeply into
the corallum (M. sulcans) or always occur shallowly in the substrate (Talpina) and, in addition, cross cut other borings
(Pinaceocladichnus). The polychaete borings are dominant. The abundance of the borings is probably caused by ecological
pressure from shallower zones in subtropical waters. This resulted in the colonization of hard, small-sized substrates
located in relatively deep (offshore) waters. The interpretation of age and palaeoenvironment was elucidated by the
analysis of benthic and planktonic foraminifers. |
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| ISSN: | 0567-7920 1732-2421 |