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Brian D. Farrell

Researcher at Harvard University

Publications -  88
Citations -  8344

Brian D. Farrell is an academic researcher from Harvard University. The author has contributed to research in topics: Monophyly & Coalescent theory. The author has an hindex of 45, co-authored 84 publications receiving 7737 citations. Previous affiliations of Brian D. Farrell include University of Maryland, College Park.

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"Inordinate Fondness" Explained: Why Are There So Many Beetles?

TL;DR: Repeated origins of angiosperm-feeding beetle lineages are associated with enhanced rates of beetle diversification, indicating a series of adaptive radiations.
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The Phylogenetic Study of Adaptive Zones: Has Phytophagy Promoted Insect Diversification?

TL;DR: The adaptive-zone hypothesis predicts that if multiple lineages have invaded a new adaptive zone, they should be consistently more diverse than their (equally old) sister groups, when the latter retain the more primitive way of life.
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The beetle tree of life reveals that Coleoptera survived end‐Permian mass extinction to diversify during the Cretaceous terrestrial revolution

TL;DR: A phylogeny of beetles based on DNA sequence data from eight nuclear genes, including six single‐copy nuclear protein‐coding genes, for 367 species representing 172 of 183 extant families provides a uniquely well‐resolved temporal and phylogenetic framework for studying patterns of innovation and diversification in Coleoptera.
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Escalation of plant defense: do latex and resin canals spur plant diversification?

TL;DR: The evidence for Ehrlich and Raven's postulate that rapid diversification follows innovation in plant defense is quantified by comparing the diversities of lineages that have independently evolved canal systems with their sister groups for as many plant lineages as current taxonomic evidence allows.
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A Simple Approximate Result for the Maximum Growth Rate of Baroclinic Instabilities

TL;DR: In this article, it was shown that the growth rate of the most rapidly growing instability is linearly proportional to the surface meridional temperature gradient, and the coefficient of proportionality is also easily determined.