Abstract

SummaryA phylogenetic analysis of the Neotropical members of genusLepidocyrtuswas conducted to assess the pattern of speciation in Puerto Rico while testing the phylogenetic information content of two characters used to diagnose subgenera. The analysis included twenty‐two species ofLepidocyrtusfrom the Neotropical Region for which information on the tergal chaetotaxy of the trunk was available, two species of HolarcticLepidocyrtus, three species ofPseudosinella, two species ofMetasinellaused in outgroup analysis and ninety‐two informative characters. The results do not support a monophyletic origin for the Puerto RicanLepidocyrtus, suggesting the current fauna originated through repeated invasions from abroad. Three instances of endemic speciation can be inferred from the cladograms. The geographical distribution and diversity of colour forms suggest thatL. caprilesi and L. paracaprilesispeciated sympatrically, whereas vicariance can explain speciation forL. lepargusandL. maldonadoi. The mode of speciation forL. dispar and L. biphasisremains unclear because the proportion of morphological variation between these species does not fit the proportions expected under the sympatric model suggested by their geographical distribution. The results support an early conclusion regarding appendicular scale distribution as a poor indicator of phylogenetic relationships. Taxa defined using this character are likely to be polyphyletic. The results disagree with a previous study in documenting low levels of homoplasy for the dental tubercle, implying that this character contains phylogenetic information useful in defining subgenera. However, the presence or absence of a dental tubercle is not diagnostic and should be used in combination with other characters. Comparisons of levels of homoplasy in Neotropical and HawaiianLepidocyrtussuggest that the relative position of two setae on the second abdominal tergum may be a better subgeneric character than other characters currently in use.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.