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2020
Abstract This chapter summarizes global patterns and mechanisms of both ecological and historical crustacean biogeography resulting in the contemporary species distributions described over the past decades. In the pelagic realm, hydrographic features such as ocean currents, physical depth profiles, and latitudinal temperature gradients ...
Halsband, C. +6 more
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Abstract This chapter summarizes global patterns and mechanisms of both ecological and historical crustacean biogeography resulting in the contemporary species distributions described over the past decades. In the pelagic realm, hydrographic features such as ocean currents, physical depth profiles, and latitudinal temperature gradients ...
Halsband, C. +6 more
openaire +2 more sources
Pattern Identification in Biogeography
IEEE/ACM Transactions on Computational Biology and Bioinformatics, 2006Identifying common patterns among area cladograms that arise in historical biogeography is an important tool for biogeographical inference. We develop the first rigorous formalization of these pattern-identification problems. We develop metrics to compare area cladograms.
Ganeshkumar Ganapathy +5 more
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Systematic Biology, 2002
In the past two decades, vicariance biogeography has become a major subdiscipline of biogeography. The subject of vicariance biogeography is the study of area relationships (e.g., Nelson and Platnick, 1981; Morrone and Crisci, 1995; Humphries and Parenti, 1999).
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In the past two decades, vicariance biogeography has become a major subdiscipline of biogeography. The subject of vicariance biogeography is the study of area relationships (e.g., Nelson and Platnick, 1981; Morrone and Crisci, 1995; Humphries and Parenti, 1999).
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1991
Abstract The fossil history of the Chrysididae is scant. The only specimens are from upper Cretaceous and lower Tertiary shale and amber, and belong to the Cleptinae, Amiseginae, and Chrysidinae (Elampini) (Table 2). The oldest of these are cleptines.
Lynn S Kimsey, Richard M Bohart
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Abstract The fossil history of the Chrysididae is scant. The only specimens are from upper Cretaceous and lower Tertiary shale and amber, and belong to the Cleptinae, Amiseginae, and Chrysidinae (Elampini) (Table 2). The oldest of these are cleptines.
Lynn S Kimsey, Richard M Bohart
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The biogeography of infection revisited
Nature Reviews Microbiology, 2022Marvin Whiteley +2 more
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