T12 EARTHTIMEs and EarthRates: Exploring the Tempo and Mode of Earth-System Processes and Evolution
Sunday, 4 November 2018
8:00 AM - 12:00 PM
Room 143-144
MESOZOIC PALEOCOMMUNITY STRUCTURE AND DYNAMICS IN THE WESTERN TETHYS
Paper number: T12-11
Program: Technical Sessions
Time: 10:30 AM – 10:45 AM
Authors
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Ashley A. DineenCalifornia Academy of Sciences, San Francisco, CA
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Carrie L. TylerMiami University, Oxford, OH
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Peter D. RoopnarineCalifornia Academy of Sciences, San Francisco, CA
Abstract
Here we compare the topology of food web models of western Tethys shallow marine paleocommunities from the Triassic (Anisian) and Jurassic (Bathonian) to identify differences in ecosystem structure and functioning associated with the Mesozoic Marine Revolution (MMR). Richness increased from the Anisian (1182 species) to Bathonian (1325 species) as did the number of guilds (from 105 to 110), suggesting the MMR led to an increase in functional richness. Although the Bathonian network is partitioned into fewer subcommunities, suspension feeders form the largest subcommunity. The increase in the prevalence of suspension feeders coincides with radiations of phytoplankton in the Jurassic. Furthermore, Bathonian guilds include larger size classes and longer trophic chains (average path length increases from 1.879 to 1.889), supporting the hypothesis that an increase in primary productivity led to increased energy transfer and higher trophic levels during the MMR.
These findings suggest that new evolutionary innovations and biotic expansions observed during the MMR may have triggered significant ecosystem restructuring and changes in energy transfer pathways, facilitated by the radiation of phytoplankton. Given the current biodiversity crisis, understanding how and why ecological changes occur is vital for effective resource management.
Geological Society of America Abstracts with Programs. Vol. 50, No. 6
doi: 10.1130/abs/2018AM-324032
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