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Lobster (Decapoda) diversity and evolutionary patterns through time

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Analyses of diversity patterns at the infraorder, superfamily and family level demonstrate that the lobsters as a group were significantly more diverse in the Mesozoic, especially the Triassic and Jurassic, than in the Cenozoic and Holocene. Peaks in numbers of genera occurred in the Late Jurassic (Oxfordian and Tithonian), Upper Cretaceous (Cenomanian and Campanian), and Holocene. Smaller peaks occurred in the Lower Triassic (Anisian) and Eocene (Lutetian). Analysis of substrate preferences for various families, based upon rock type enclosing the fossils, suggests that Nephropoidea and Erymidae were quite variable in substrate preference. When examined by energy-level preferences, most lobster groups exhibit preferences; some preferences changed through time. A long-standing preference for low energy substrates appears to support the long held hypotheses that Nephropidae moved into deeper water either because of the end-Cretaceous events, or due to competition with brachyurans. Inhabitation of many types of substrates seems to predict survival of mass-extinction events in lobsters as does a shift in substrate preference through time. Lobsters can be arranged into three evolutionary faunas, Triassic, Jurassic, and Modern, that are distinct and exhibit discrete body plan and faunal turnover patterns. Several biases in the dataset have been identified. These include a strong bias toward European, Mesozoic occurrences at the expense of other locations and times; an environmental bias toward epicontinental versus oceanic or active margin occurrences; and monographic biases.

Affiliations: 1: 1Department of Geology, Kent State University at Stark, 6000 Frank Ave. NW, North Canton, OH 44720, USA; 2: 2Department of Geology, Kent State University, Kent, OH 44242, USA

10.1163/1937240X-00002288
/content/journals/10.1163/1937240x-00002288
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