scholarly journals REVIEW OF INVERTEBRATE FOSSILS AND PRINCIPLES OF INVERTEBRATE PALEONTOLOGY

Evolution ◽  
1953 ◽  
Vol 7 (2) ◽  
pp. 183-185 ◽  
Author(s):  
Norman D. Newell
2000 ◽  
Vol 10 ◽  
pp. 25-36
Author(s):  
Nigel C. Hughes ◽  
Frederick J. Collier ◽  
Joanne Kluessendorf ◽  
Jere H. Lipps ◽  
Wendy L. Taylor ◽  
...  

INVERTEBRATE and micro-fossil collections vary in size, scope, degree of documentation, quality of curation, purpose, usage, and security. This chapter introduces the main categories of fossil collections and curatorial attention, and documents the sources and uses of invertebrate paleontological materials. The term ‘permanent collection’ is used to describe collections housed in professional collections-care institutions that provide long-term commitment to collection security and curation. Invertebrate fossils include the hardparts (spicules, shells, etc., other body fossils [e.g., impressions, casts, and molds]), tracks, trails, and burrows attributed to invertebrates, and organic molecules. Microfossils, included here for convenience only, include the same kinds of remains of prokaryotes, protists, and tiny invertebrates. This book is the product of an National Science Foundation funded workshop organized to address specific concerns about curatorial practices in invertebrate paleontology. For this reason the focus of this chapter is on invertebrate fossils. Nevertheless, the concepts and uses of collections described below apply directly to paleobotanic specimens, and to most vertebrate fossils.


2000 ◽  
Vol 10 ◽  
pp. 51-64
Author(s):  
Russell D. White

COLLECTIONS OF invertebrate fossils are commonly maintained in museums, at universities, and by individual researchers and interested private collectors. Twenty years ago, the Committee on North American Resources in Invertebrate Paleontology (CONARIP) estimated that there more than 550 institutions housed invertebrate paleontological macro- and micro- fossil collections (Glenister, 1977). Historically, collections have been developed, managed and maintained by paleontologists as a resource for their research (e.g., museum curator or university faculty) (Hebda, 1985). Since the early 1970s, the field of collection management has evolved and the increased professionalization of collection manager positions has been instrumental in improving the management and preservation of invertebrate fossils as well as other natural history collections (Cato, 1991; Simmons, 1993; Simmons, 1995).


2000 ◽  
Vol 10 ◽  
pp. 73-82
Author(s):  
Elizabeth Merritt ◽  
Scott Lidgard

ALL MUSEUMS have limited resources, and all acquisitions use some of these resources, whether they be space, money, staff time or materials. When museums purchase collections objects, some “costs” are evident up front, and there are frequently mechanisms in place at a high level to monitor that use of museum resources. For example, in art museums this is often a committee of the board of directors empowered to approve or deny curatorial proposals for major (i.e., expensive) acquisitions. However when the object is “free,” as in most invertebrate paleontology collections where material is either donated or collected in the field by museum staff, the cost of acquiring the object is essentially hidden. Some acquisition costs may be fixed regardless of the size or nature of the acquisition, and some vary depending the amount of space the material will require, or the amount of cleaning or conservation needed.


10.3133/pp606 ◽  
1969 ◽  
Author(s):  
Mackenzie Gordon ◽  
William J. Sando ◽  
John Pojeta ◽  
Ellis L. Yochelson ◽  
I.G. Sohn

1986 ◽  
Vol 60 (5) ◽  
pp. 1133-1133
Author(s):  
Edward C. Wilson

A specimen of the ammonoid Perrinites Böse, 1919, was collected from the McCloud Limestone east of the summit of Tombstone Mountain, Shasta County, California. This is the first record of the genus in California, an important addition to the meager Permian cephalopod fauna of the state previously reported by Miller, Furnish, and Clark (1957) and Wilson (1984). It was found 1,100 feet (335 m) above the base of the formation in a coarse-grained limestone (Los Angeles County Museum of Natural History, Invertebrate Paleontology Section locality 6184) within fusulinid zone H of Skinner and Wilde (1965), considered to be late early or early middle Leonardian in age.


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