Annelida Lamarck 1809
- Dataset
- Identification of fossil worm tubes from Phanerozoic hydrothermal vents and cold seeps
- Rank
- PHYLUM
Classification
- kingdom
- Animalia
- phylum
- Annelida
description
Description. Carbonate tube sections measuring 2.9 – 5.7 mm in diameter, all fairly straight, and not attached to other tubes. The long tube appears unornamented (Fig. 14 A) and the tube with a black wall is smooth and shows no ornamentation apart from a possible small collar (Fig. 14 B), while the remaining tube fragment bears what may be faint longitudinal wrinkles (Fig. 14 C). In thin section, some of the tubes exhibit thick, neatly multi-layered walls (Fig. 14 D, E). Curving delaminated layers can also be observed in some of the tube sections (Fig. 14 F), suggesting that they were originally organic in composition. A subset of tubes exhibit diffuse (poorly preserved?) tube walls (Fig. 14 G).
description
‘ Sassenfjorden area tubes’ (Fig. 14) 2011 ‘ vestimentiferan’ worm tubes Hammer et al. 21, fig. 5 d. 2012 worm tubes Hryniewicz, Hammer et al. 118, fig. 5 a.
discussion
Remarks. Non-serpulid, originally organic-walled tubes from the Sassenfjorden area were suggested to have been made by siboglinids (Hammer et al. 2011; Hryniewicz et al. 2015). However, the tubes examined do not clearly group with the tubes of modern annelid families included in cladistic and cluster analyses (Figs 22, 24). The tube sections with thick, neatly multi-layered walls that were observed within this study were possibly made by vestimentiferans, in which this tube structure is widely observed. However, the broad morphology of this tube is presently unknown, and tubes from this deposit in general warrant further investigation as several different tube types are present. Hence, these tubes are broadly ascribed to the annelids.
materials_examined
Material. Svalbard 2007 - 03, long tube with yellowish wall. PMO 2009 - 01, single tube with dark black wall. PMO 2009 - 03: single tube with longitudinal wrinkles. 171.002 D, 170.996, 171.027, selection of thin sections of different tubes. Donated by K. Hryniewicz. Occurrence. Sassenfjorden area, Svalbard. Seep carbonates in shale and shale and siltstone, Slottsmøya Member, upper Agardhfjellet Formation, Volgian – Ryazanian (latest Jurassic – earliest Cretaceous) (Hammer et al. 2011; Hryniewicz et al. 2012, 2015; Vinn et al. 2014).