A description is given of syringoporids found as Pleistocene erratics from the northern part of the Netherlands. A new morphogenetic interpretation of the syringoporid skeleton is suggested: tubules (modified pores) and so-called fundibular tabulae (which actually consist of series of tabellae) are considered as adaptions to the fructicose morphology of the colony. Lateral increase has been observed.

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Grondboor & Hamer

CC BY 3.0 NL ("Naamsvermelding")

Nederlandse Geologische Vereniging

H. Huisman. (1979). Noordelijke zwerfsteenkoralen (12). Grondboor & Hamer, 33(1), 2–16.