Abstract

The objectives of this work are to use gene sequence data to assess the hypothesis that the Lithodinae arose from ancestors with uncalcified abdomens in shallow waters of the North-East Pacific, investigate the monophyly and interrelationships of genera within the Lithodinae and to estimate the scale and minimum number of biogeographic transitions from the shallow environment to the deep sea and vice versa. To do this, phylogenetic analysis from three mitochondrial and three nuclear markers was conducted using minimum evolution, maximum likelihood and Bayesian methods. The Lithodinae as defined to include North Pacific genus Cryptolithodes may be paraphyletic, with the Hapalogastrinae and Cryptolithodes as sister taxa. This implies that the soft-bodied abdomen of the Hapalogastrinae might not be plesiomorphic for the Lithodidae. Paralomis, Lopholithodes, Phyllolithodes, Lithodes and Neolithodes share a common ancestor, from which the North Pacific Hapalogastrinae did not descend. Lithodid ancestors are likely to have had a north Pacific, shallow water distribution and to have had planktotrophic larvae. North Pacific genus Paralithodes is paraphyletic; P. brevipes is the most basal member of the genus (as sampled) while P. camtschaticus and P. platypus are more closely related to the genera Lithodes and Neolithodes. Genera Lithodes, Neolithodes and Paralomis (as sampled) are monophyletic if Glyptolithodes is included within Paralomis. Lopholithodes is closely related to, but not included within, the Paralomis genus. Paralomis is divided into at least two major lineages: one containing South Atlantic, West African, and Indian Ocean species, and the other containing Pacific and South American species. Several species of Paralomis do not resolve consistently with any other groups sampled, implying a complex and possibly rapid global evolution early in the history of the genus. Relationships within the Lithodes genus vary between analytical methods, suggesting that conclusions may not be stable. Consistently, however, Indian Ocean and Pacific forms—L. murrayi, L. longispina and L. nintokuae form a group separated from Atlantic species such as L. santolla, L. confundens, L. maja and L. ferox.

Highlights

  • IntroductionStudy of the origins of the Lithodidae has increased in recent decades (Zaklan 2002; Hall and Thatje 2009; Bracken-Grissom et al 2013), with particular interest being placed on the putative relationship between ‘primitive’ (morphologically less derived) lithodids and hermit crabs of the family Paguridae (Bracken-Grissom et al 2013; Noever and Glenner 2017)

  • The anomuran LithodidaeThe anomuran crab family Lithodidae Samouelle 1819 comprises a great diversity of morphological and ecological forms: Communicated by: Claus-Dieter Hillenbrand Electronic supplementary material The online version of this article contains supplementary material, which is available to authorized users.from abyssal crabs with walking legs longer than a metre to intertidal forms such as the genus Cryptolithodes Brandt 1848, which has tiny legs covered by a laterally expanded carapace (Bowman 1972; see Hall and Thatje 2010)

  • The results obtained from a database search on GenBank using Megablast (BLASTN v2.2.18) showed that the sequences from formalin-fixed specimens were homologous to the available lithodid sequences

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Summary

Introduction

Study of the origins of the Lithodidae has increased in recent decades (Zaklan 2002; Hall and Thatje 2009; Bracken-Grissom et al 2013), with particular interest being placed on the putative relationship between ‘primitive’ (morphologically less derived) lithodids and hermit crabs of the family Paguridae (Bracken-Grissom et al 2013; Noever and Glenner 2017). It has been hypothesised that the uncalcified abdomen uniting the subfamily Hapalogastrinae reflects the retention of a primitive condition, and that primitive groups from the shallow north Pacific were the seeding populations for the global deep-water expansion of the Lithodinae. This hypothesis remains a source of controversy (McLaughlin et al 2007)

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