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News

Innovative study clarifies evolutionary history of early complex single-celled organisms

Virginia Polytechnic Institute And State University : 16 March, 2004  (Technical Article)
A billion years ago (the Neoproterozoic age), complex single-celled organisms, acritarchs, began to develop, grow, and thrive. Almost a billion years later, the study of the evolutionary history of acritarchs began to bog down amid inconsistencies in the reporting of the diversity of species.
A billion years ago (the Neoproterozoic age), complex single-celled organisms, acritarchs, began to develop, grow, and thrive. Almost a billion years later, the study of the evolutionary history of acritarchs began to bog down amid inconsistencies in the reporting of the diversity of species.

Now, a Virginia Tech graduate student has devised a new way to study the ebb and flow of life in the Neoproterozoic and Early Cambrian ages, a period that includes two mass extinctions.

John Warren Huntley, of Asheville, N.C., a Ph.D. student in geosciences in the College of Science, will report on his strategy and results at the joint meeting of the Northeastern and Southeastern Sections of the Geological Society of America to be held March 25-27 in Tysons Corner, Va. Huntley received his bachelor's degree from Appalachian State University and his master's degree from the University of North Carolina at Wilmington.

'The evolutionary history of acritarchs reported in the literature has been based on the number of species,' explains Huntley. 'But there have been many workers collecting information and there is variation among these researchers on what is considered a species. This variation among workers could alter our understanding of what actually happened.'

The strategy of a group of geoscientists at Virginia Tech is to use the quantitative data reported in the scientific literature to look at size and morphological complexity of specimens collected. So far, they have examined acritarch data spanning more than 700 million years, from 1270-million-year-old rocks deposited long before Neoproterozoic ice ages to Early Cambrian successions rocks deposited during the explosive evolution of early animals.

'Our preliminary results seem to confirm previous anecdotal evidence,' says Huntley. 'We're finding that complexity increases through time, which is to be expected.'

However, complexity leveled off. 'It appears that morphological complexity may have remained steady at high values, even when species diversity was fluctuating greatly,' Huntley says.

As to size, there was a steady increase in size for at least 500 million years until the Ediacaran extinction, after which acritarchs remained very small compared to their pre-Ediacaran extinction size. 'There had been anecdotal observations of the size change, which we have now quantified,' Huntley says.

Huntley will present the paper, 'Secular patterns in morphological disparity and body size of acritarchs through the Neoproterozoic and early Cambrian' (47-2) at 1:20 p.m. Friday, March 26, as part of the session on Pre-Cenozoic Paleontology in the Gunston A room at the Hilton McLean-Tysons Corner hotel. Co-authors are Virginia Tech geosciences professors Shuhai Xiao and Michal Kowalewski.

The trio began their study of acritarchs last October. 'It is interesting to use novel techniques to study early life and this is a good opportunity to increase my knowledge in this important area,' says Huntley, who has been studying mollusk evolution.
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