Australian Museum Journal On the origin of Crustacea

Shortform:
McKenzie, 1984, Aust. Mus. Mem. 18(3): 21–43
Author(s):
McKenzie, K. G.
Year published:
1984
Title:
On the origin of Crustacea
Serial title:
Australian Museum Memoir
Volume:
18
Issue:
3
Start page:
21
End page:
43
DOI:
10.3853/j.0067-1967.18.1984.370
Language:
English
Date published:
31 March 1984
Cover date:
31 December 1983
ISSN:
0067-1967
CODEN:
AUNMA5
Publisher:
The Australian Museum
Place published:
Sydney, Australia
Subjects:
CRUSTACEA; EVOLUTION
Digitized:
09 September 2009
Reference number:
370
EndNote package:
EndNote file
Title page:
Title page (137kb PDF)
Complete work:
Complete work (3212kb PDF)

Abstract

Crustaceans are predominantly aquatic arthropods with a characteristic naupliar stage. Their known evolutionary history extends at least from the Early Cambrian. They display many features convergent with the chelicerates, uniramians and trilobites and formerly were classified with these groups in Arthropoda. It seems more appropriate to study the origins of Crustacea by reference to their Cambrian representatives than by seeking to establish particular intuitions concerning early crustaceans based on a knowledge of living forms only. Among Cambrian fossils, the lobopod Aysheaia is irrelevant to crustacean origins. Similarly, the living Tardigrada are best consigned to a separate phylum although they seem to be a related group with several primitive characters and are likely, on zoogeographic grounds, to have had a long evolutionary history. Assuming that Crustacea are monophyletic, the existing fossil record dictates that the ancestral taxon possessed a complex of characters out of which evolved (during Cambrian times) at least: bradoriids and other primitive ostracode-like animals; Canadaspis and other phyllocarid-like forms; Branchiocaris and similar notostracan-like forms. Several other Cambrian taxa may be either true crustaceans or examples of convergence. Some show similarities to anostracans and conchostracans. The diversity and complexity of the Cambrian fossils suggest that a basic crustacean facies was already established by the Late Precambrian (Ediacaran).