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The\udrosette-shaped microboring trace fossil <i>Neodendrina carnelia</i> igen. et isp. n. – a large representative of the ichnofamily Dendrinidae – is\udidentified on the inner side of the giant clam <i>Tridacna maxima</i> from\udPleistocene to Holocene coral reef deposits of the El Quseir district at the\udEgyptian Red Sea coast. The new dendritic bioerosion trace fossil is\uddiagnosed as a radial rosette comprised of a prostrate system of roofless\udcanals that ramify in a strictly dichotomous fashion forming intermittent\udbranches of uniform width and rounded terminations. The trace appears to be\udrare, although in the type material it occurs in a cluster of more than a\udhundred specimens. The location of traces on the interior surface of the\udshell suggests that boring occurred post-mortem to the host. Its\udrecord is presently restricted to shallow marine, euphotic, tropical coral\udreef settings in the Western Indo-Pacific (Red Sea and Madagascar). The\udbiological identity of the trace maker cannot be resolved yet, but several\udlines of reasoning allow speculations directed towards a complex attachment\udscar, perhaps produced by a benthic foraminiferan or a macrophyte

fossil record

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