Precambrian Sponges with Cellular Structures

Author:

Li Chia-Wei12,Chen Jun-Yuan12,Hua Tzu-En12

Affiliation:

1. C.-W. Li and T.-E. Hua, Department of Life Science, National Tsing Hua University, Hsinchu, Taiwan, China.

2. J.-Y. Chen, Nanjing Institute of Geology and Palaeontology, Academia Sinica, Nanjing, China.

Abstract

Sponge remains have been identified in the Early Vendian Doushantuo phosphate deposit in central Guizhou (South China), which has an age of ∼580 million years ago. Their skeletons consist of siliceous, monaxonal spicules. All are referred to as the Porifera, class Demospongiae. Preserved soft tissues include the epidermis, porocytes, amoebocytes, sclerocytes, and spongocoel. Among thousands of metazoan embryos is a parenchymella-type of sponge larvae having a shoe-shaped morphology and dense peripheral flagella. The presence of possible amphiblastula larva suggests that the calcareous sponges may have an extended history in the Late Precambrian. The fauna indicates that animals lived 40 to 50 million years before the Cambrian Explosion.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference45 articles.

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2. A. P. Benus in Trace Fossil Small Shelly Fossils and the Precambrian-Cambrian Boundary E. Landing G. M. Narbonne P. Myrow Eds. ( Bull. 463 New York State Museum Albany 1988 ) p. 8.;

3. Animal Origins

4. B. Runnegar Neues Jahrb. Geol. Palaeontol. Abh. 195 305 (1995)

5. A. H. Knoll Paleobiology 22 1 (1996);

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