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Fossil Record A palaeontological open-access journal of the Museum für Naturkunde
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A new bioerosion trace fossil, the rosette-shaped microboring Neodendrina carnelia igen. et isp. n., is described from a giant clam (Tridacna maxima) discovered in Pleistocene to Holocene coral reef deposits of the Egyptian Red Sea coast. The trace was formed as a complex attachment scar after the host had ceased. The biological identity of the trace maker, probably either a benthic foraminiferan or a macrophyte, is discussed.
Articles | Volume 21, issue 1
Foss. Rec., 21, 1–9, 2018
https://doi.org/10.5194/fr-21-1-2018
Foss. Rec., 21, 1–9, 2018
https://doi.org/10.5194/fr-21-1-2018

Research article 10 Jan 2018

Research article | 10 Jan 2018

Large dendrinids meet giant clam: the bioerosion trace fossil Neodendrina carnelia igen. et isp. n. in a Tridacna shell from Pleistocene–Holocene coral reef deposits, Red Sea, Egypt

Max Wisshak and Christian Neumann

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Cited articles

Ashworth, J. S., Ormond, R. F., and Sturrock, H. T.: Effects of reef-top gathering and fishing on invertebrate abundance across take and no-take zones, J. Exp. Mar. Biol. Ecol., 303, 221–242, 2004.
Barnes, H. and Topinka, J. A.: Effect of the nature of the substratum on the force required to detach a common littoral alga, Am. Zool., 9, 753–758, 1969.
Benzoni, F., Ashworth, J. S., Addamo, A. M., Stefani, F., Mabrouk, A., and Galli, P.: Artisanal fisheries and no-take zones in Nabq, Egypt: Effects on molluscs and reef top benthic assemblages, in: Proceedings of the 10th International Coral Reefs Symposium, Okinawa, Japan, 1362–1367, 2006.
Bromley R. G. and Heinberg C.: Attachment strategies of organisms on hard substrates: A palaeontological view, Palaeogeogr. Palaeoclimatol. Palaeoecol., 232, 429–453, 2006.
Bromley R. G., Wisshak M., Glaub I., and Botquelen, A.: Ichnotaxonomic review of dendriniform borings attributed to foraminiferans: Semidendrina igen. nov., in: Trace fossils: concepts, problems, prospects, edited by: Miller III, W., Elsevier, Amsterdam, 518–530, 2007.
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Short summary
A new bioerosion trace fossil, the rosette-shaped microboring Neodendrina carnelia igen. et isp. n., is described from a giant clam (Tridacna maxima) discovered in Pleistocene to Holocene coral reef deposits of the Egyptian Red Sea coast. The trace was formed as a complex attachment scar after the host had ceased. The biological identity of the trace maker, probably either a benthic foraminiferan or a macrophyte, is discussed.
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