Pelagic trilobites as an example of deducing the life habits of extinct arthropods
- 1 January 1985
- journal article
- life and-environment-of-fossil-forms
- Published by Cambridge University Press (CUP) in Earth and Environmental Science Transactions of the Royal Society of Edinburgh
- Vol. 76 (2-3) , 219-230
- https://doi.org/10.1017/s0263593300010452
Abstract
This paper reviews the methods which have been used to deduce the life habits of trilobites. The most reliable conclusions are those that satisfy three independent criteria of evidence: (1) functional morphology of the exoskeleton; (2) analogy with living arthropods; and (3) geological evidence, as from facies relationships, or palaeogeography. Pelagic trilobites are one of the better examples for life habit reconstruction. The Ordovician trilobites that were most probably pelagic are those with hypertrophied eyes—Telephinidae, Opipeuteridae, Bohemillidae and Cyclopygidae—which satisfy the threefold requirements for evidence. Opipeuter, Carolinites (and other telephinids) were probably epipelagic, whereas cyclopygids and Bohemilla were likely to have been mesopelagic, living in exterior sites around the perimeter of Gondwana in the earlier Ordovician. These pelagics divide into two morphological groups: poorly streamlined, sluggish species somewhat like the living hyperiid Parathemisto, and well-streamlined species which are larger, and are considered to have been fast and active swimmers, with predatory habits. The streamlining of this group has been demonstrated by experiment. Other trilobites may also have been pelagic, but the evidence is less complete: Irvingella and its homeomorphs, and Remopleurides. Most Olenidae, however, which have been supposed to have been pelagic, were benthic forms inhabiting a specialised environment low in oxygen and possibly below the thermocline; only the leptoplastines may have been pelagic.It is also shown that there are cases where ventral terrace ridges did not function to grip sediment during filter feeding. This applies not only to pelagic trilobites, but also to benthic ones in which the width and disposition of the doublure renders engagement with the sediment unlikely.Keywords
This publication has 32 references indexed in Scilit:
- The ecological, significance of variation in the generic composition of Rawtheyan (late Ordovician) trilobite faunas from North Wales, U.K.Geological Journal, 1984
- Definition of the Tremadoc Series and the series of the Ordovician System in BritainGeological Magazine, 1984
- Structure, patterns and function of cuticular terraces in trilobitesLethaia, 1981
- Prospectatrix genatenta(Stubblefield) and the trilobite superfamily CyclopygaceaGeological Magazine, 1981
- Evolution in a cline: the trilobiteTriarthrusalong an Ordovician depth gradientLethaia, 1980
- Distributional model for marine isopod crustaceans and its bearing on early Paleozoic paleozoogeography and continental driftGSA Bulletin, 1979
- Structure, patterns, and function of cuticular terraces in recent and fossil arthropodsZoomorphology, 1978
- Methods and conclusions in functional analysis: a replyLethaia, 1975
- Trilobite Eyes: Calcified Lenses in vivoScience, 1973
- IV. Part of a letter from Mr. Edw. Lhwyd to Dr. Martin Lister, Fell. of the Coll. of Phys. and R. S. concerning several regularly figured stones lately found by him.Philosophical Transactions of the Royal Society of London, 1698