Functional Morphology and Biomechanics of Articulate Brachiopod Shells

2001 ◽  
Vol 7 ◽  
pp. 145-170 ◽  
Author(s):  
Richard R. Alexander

In the first Paleontological Society short course dealing with functional morphology of extinct brachiopod taxa, Grant (1981, p. 127) emphasized analogy with living species in reconstruction of life habits, but then cited many pitfalls of taxonomic uniformitarianism. The present is hardly the key as to how brachiopod shells functioned in the past, given the plethora of morphologic structures that have vanished since the Paleozoic diversity climax of articulates. Although direct observations (Table 1), such as clasping spines encircling a blastoid columnal (Grant, 1963), or biomechanical tests (e.g., Thayer, 1975a) and flume experiments (e.g., LaBarbera, 1978) on living articulate brachiopods, enable convincing assertion of a morphologic structure's function, indirect methodologies (Savazzi, 1999)(Table 1) have supplanted mere analogies with living brachiopods. Indirect methodologies (Savazzi, 1999, p. 6) reconstruct and infer the function of skeletal structures from theoretical (morphospace) and actual scaled models of extinct taxa, hydrodynamic and biomechanical tests on empty shells, commensal associations with fossilized epibionts, clinal variations in structures over paleogeographic and paleobathymetric gradients, and post-mortem, post-burial orientational evidence. The common denominator of indirect methodologies is that inferences are made on dead shells usually, but not always, from extinct taxa. Although such inferences of skeletal function of extinct taxa vary in the rigor by which they are deduced, indirect methodologies have been increasingly refined over the last 20 years (Table 1).

2004 ◽  
Vol 10 ◽  
pp. 1-4 ◽  
Author(s):  
Jere H. Lipps

The Neoproterozoic—Cambrian biological and geological events between 630 to 530 or so million years ago, are among the most fascinating topics in life history today because the first animals appeared and radiated amidst environmental changes of major magnitude. Not only are paleontologists and geologists interested in these events, but so are the general public, biologists, and theologians, among others. Indeed, this interest was manifested in a cover story in Time Magazine (Nash, 1995), another in the National Geographic (Monastersky, 1998), and in newspapers and other outlets. It is an intriguing time period, for most people are interested in our origins-of life itself, of animals, and of humans. The topics of this book then are nearly unique in this respect. The Paleontological Society is therefore pleased to present a Short Course and book summarizing the evidence, interpretations and hypotheses relating to this interval of time, with a focus on the origin and early evolution of the first known animals through a period of about 100 million years. Like all of the Society's Short Course books, this one is designed to provide a current review an important topic in paleontology for college instructors, interested professionals, and students. Such a book cannot cover the topics in great detail, but the authors have provided up-to-date references to additional sources.


1993 ◽  
Vol 6 ◽  
pp. 1-8 ◽  
Author(s):  
Susan M. Kidwell ◽  
Anna K. Behrensmeyer

Since their inception in 1978, the annual short courses sponsored by the Paleontological Society have aimed to broaden and to enhance the professional education of paleontologists, including students new to the field. The 1993 short course continues in that tradition, but differs from many previous courses in focussing not on a taxonomic group but on a broader aspect of the fossil record, namely the time resolution of fossil assemblages. This seemed an especially good topic for a short course because questions of absolute and relative time – how old? how fast? how synchronously? – pervade paleontology and historical geology in general.


1985 ◽  
Vol 13 ◽  
pp. 258-267
Author(s):  
Stephen Jay Gould

We don't need paleontological perspective to regard 30 years as a short time. Many in this audience, and several speakers in this symposium (but not yours truly, who was busy celebrating the Yankees' unprecedented fifth consecutive world series victory and wondering how a 12-year old boy could turn into a paleontologist), were already practicing our profession when the Paleontological Society marked the beginning of its great Treatise project with a symposium at the 1953 G.S.A. meeting on the status of our field (Kummel, 1954).


2008 ◽  
Vol 58 (2) ◽  
pp. 123-172 ◽  
Author(s):  
Rui Diogo

AbstractThe Osteichthyes, including bony fishes and tetrapods, is a highly speciose group of vertebrates, comprising more than 42000 living species. The anatomy of osteichthyans has been the subject of numerous comparative studies, but these mainly concern osteological structures; much less attention has been paid to muscles. In fact, the most detailed and comprehensive myological comparative analyses that were actually based on a direct observation of representatives of various major osteichthyan groups were provided various decades by authors such as Luther, Kesteven and principally Edgeworth. The present work provides an updated discussion of the homologies and evolution of the osteichthyan mandibular, hyoid and hypobranchial muscles, based on the author's own analyses and on a survey of the literature, both old and recent. The risks of discussing muscle homologies on the basis of a single line of evidence, even when it concerns innervation or development, is emphasized. It is stressed than only by taking into consideration various lines of evidence (e.g. developmental biology, comparative anatomy, functional morphology, paleontology, molecular biology, experimental embryology, innervation and/or phylogeny) it is possible to establish well-grounded hypotheses of muscle homology.


2001 ◽  
Vol 7 ◽  
pp. 5-10
Author(s):  
J. Thomas Dutro

The Paleontological Society Short Course this year features the history of brachiopod research, especially since the beginning of the revision of Part H, Treatise on Invertebrate Paleontology, in the early 1990s. The first version of Part H was published in 1965 and the only previous Paleontological Society Short Course to deal with brachiopods was held in 1981 at the Cincinnati meeting of the Geological Society of America. At that time, the day was split between the bryozoans and brachiopods, with a nod to the phoronids, under the rubric of lophophorates.


1985 ◽  
Vol 13 ◽  
pp. 1-3
Author(s):  
Ellis L. Yochelson

Because the first Paleontological Society short course covered the Mollusca, it may be appropriate to record a few words concerning that occasion and give belated thanks to those who participated. After being president of the Society, it occurred to me that most of the membership associated the Journal of Paleontology with it, but did not seriously consider the organization as a focal point for other activities. By giving a short course annually, I felt we could inform the membership on scientific matters, and also build up additional interest in society activities. The annual short courses on the various fossil groups and phyla have more than fulfilled that expectation. They tell the world that paleontology is alive and well.


2017 ◽  
Vol 373 (1739) ◽  
pp. 20160492 ◽  
Author(s):  
Carolin Haug

The key to understanding fossil ecosystems is to understand the life habits of long extinct organisms. Yet, as direct observations are no longer possible, morphological details are usually the only available data source. One important aspect of lifestyle is feeding strategies, which can be inferred from morphological structures in comparison with those of extant relatives. The Lower Devonian Rhynie and Windyfield cherts preserve even minute structures to a high degree of detail, which allows investigation of the functional morphology of structures possibly involved in feeding. In this contribution, the feeding structures of different arthropods from the Rhynie and Windyfield cherts are described and the corresponding feeding strategies of the animals are discussed. This overview illustrates that in this early non-marine biota, a wide range of feeding strategies already existed. This article is part of a discussion meeting issue ‘The Rhynie cherts: our earliest terrestrial ecosystem revisited’.


Author(s):  
R. A. Fortey

ABSTRACTThis 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.


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