Skip navigation

The NaturePlus Forums will be offline from mid August 2018. The content has been saved and it will always be possible to see and refer to archived posts, but not to post new items. This decision has been made in light of technical problems with the forum, which cannot be fixed or upgraded.

We'd like to take this opportunity to thank everyone who has contributed to the very great success of the forums and to the community spirit there. We plan to create new community features and services in the future so please watch this space for developments in this area. In the meantime if you have any questions then please email:

Fossil enquiries: esid@nhm.ac.uk
Life Sciences & Mineralogy enquiries: bug@nhm.ac.uk
Commercial enquiries: ias1@nhm.ac.uk

Currently Being Moderated

Earth Science Department Seminar

Posted by C Lowry on Nov 22, 2012 12:55:59 PM

Palaeontology Seminar

 

Microstructure of modern sea pen axes – a tool for the systematics of fossil pennatulaceans (Octocorallia)

 

Dr Mike Reich, University of Göttingen

 

Thursday 29th November

Neil Chalmers Seminar Room, DC2, 12:00 (the first of two talks that day)

 

 

 

Pennatulaceans are considered to be a very distinct and specialised group of octocorallian cnidarians, known from soft bottom areas of the intertidal to the deep sea. Since they are largely composed of soft tissue, the systematics of modern sea pens (Anthozoa: Octocorallia) are mostly based on soft-part morphology. Among the only hard parts (an axial rod and various sclerites) present in most species, only the sclerites have been employed as systematic traits. However, both types of hard parts, especially the calcareous axial rod, are often the only remnants of fossil Pennatulacea. Fossil sea pen axes (known since the Late Cretaceous) have therefore mostly been placed in the ‘collective genus’ Graphularia without any further systematic assignment. A study of hard-part morphology, using 20 modern sea pen species from 10 of the 14 valid families, has shown that the microstructure of the axial rod is relatively consistent within a genus, whereas the cross-section may vary between the distal ends of the rachis and the peduncle. Using field emission SEM, the microstructure of at least a dozen fossil Graphularia species have been studied. By comparing the microstructure of modern and fossil sea pens, similarities allow a placement of fossil pennatulacean species close to modern genera and within modern families, demonstrating the value of axis microstructure as a systematic trait.

 

 

 

 

For additional details on attending this or other seminars see http://www.nhm.ac.uk/research-curation/seminars-events/index.html

Comments (0)