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2 The Way the Earth Works: Plate Tectonics
3 Patterns in Nature: Minerals
4 Up From the Inferno: Magma and Igneous Rocks
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6 Change in the Solid State: Metamorphic Rocks
7 The Wrath of Vulcan: Volcanic Eruptions
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9 Crags, Cracks, and Crumples: Crustal Deformation and Mountain Building
10 Deep Time: How Old is Old?
11 A Biography of Earth
12 Riches in Rock: Energy and Mineral Resources
13 Unsafe Ground: Landslides and Other Mass Movements
14 Streams and Floods: The Geology of Running Water
15 Restless Realm: Oceans and Coasts
16 A Hidden Reserve: Groundwater
17 Dry Regions: The Geology of Deserts
18 Amazing Ice: Glaciers and Ice Ages
19 Global Change in the Earth System


Clues in the Fossil Record

by Stephen Marshak
Overview Image

Early Cambrian fossil

Credit: Science

Paleontologists have the unenviable task of trying to piece together the history of evolution using tiny bits of information separated by huge gaps of time. This effort is particularly difficult in the Precambrian where the fossil record is exceptionally sparse. Mysteriously following this scarcity, almost all the main types of animals (or phyla) that exist today, suddenly appear in the fossil record at the beginning of the Cambrian, around 545 million years ago. 

Many paleontologists concluded that an explosion of evolutionary activity during the early Cambrian must be responsible. But others aren't convinced that evolution that rapid is possible. They have suggested a longer period of evolution that left no fossil record must have preceded the Cambrian.

German and British researchers recently made a discovery that lends support to the idea that the Cambrian explosion might not have been that explosive after all, and may have been preceded by a long evolutionary fuse in the Precambrian.  They found some of the oldest known crustaceans in Lower Cambrian limestone deposits in Shropshire, England. The 511 year-old fossils are very well preserved with some of the soft body parts cast in calcium phosphate, allowing them to be identified with confidence unlike other rare fossils of this age. 

Crustaceans such as these, as well as modern animals like crabs, lobsters and shrimp, are members of the arthropod phylum. Previously, the oldest undoubted crustaceans were from the late Cambrian, which left 40 million years for them to evolve from a primitive arthropod at the beginning of the Cambrian. But the new discovery of early Cambrian crustaceans suggests the process must have started sooner to allow enough time for all the necessary evolutionary steps from arthropod to crustacean.

Though the newly discovered fossils are good evidence for Precambrian evolution, paleontologists would like to find an early arthropod fossil that can be identified with confidence. The search is on, but uncovering such a fossil is akin to finding the proverbial needle in a haystack. The ancestral arthropods would most certainly have been very small and lacking a shell or skeleton that could be preserved for discovery by scientists millions of years later. Still, soft animal parts may be phosphatized as in the case of the recently discovered crustaceans. In spite of the odds mounted against them, fossil hunters continue their search in hopes of finding a Precambrian piece to the evolutionary puzzle.

REFERENCES:

  • Siveter, D.J., Williams, M., Waloszek, D. 2001, A phosphatocopid crustacean with appendages from the Lower Cambrian:  Science, v.293, p. 479-481.

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