Abstract

BackgroundLake Tanganyika belongs to the East African Great Lakes and is well known for harbouring a high proportion of endemic and morphologically distinct genera, in cichlids but also in paludomid gastropods. With about 50 species these snails form a flock of high interest because of its diversity, the question of its origin and the evolutionary processes that might have resulted in its elevated amount of taxa. While earlier debates centred on these paludomids to be a result of an intralacustrine adaptive radiation, there are strong indications for the existence of several lineages before the lake formation. To evaluate hypotheses on the evolution and radiation the detection of actual adaptations is however crucial. Since the Tanganyikan gastropods show distinct radular tooth morphologies hypotheses about potential trophic specializations are at hand.ResultsHere, based on a phylogenetic tree of the paludomid species from Lake Tanganyika and adjacent river systems, the mechanical properties of their teeth were evaluated by nanoindentation, a method measuring the hardness and elasticity of a structure, and related with the gastropods’ specific feeding substrate (soft, solid, mixed). Results identify mechanical adaptations in the tooth cusps to the substrate and, with reference to the tooth morphology, assign distinct functions (scratching or gathering) to tooth types. Analysing pure tooth morphology does not consistently reflect ecological specializations, but the mechanical properties allow the determination of eco-morphotypes.ConclusionIn almost every lineage we discovered adaptations to different substrates, leading to the hypothesis that one main engine of the flock’s evolution is trophic specialization, establishing distinct ecological niches and allowing the coexistence of taxa.

Highlights

  • Lake Tanganyika belongs to the East African Great Lakes and is well known for harbouring a high proportion of endemic and morphologically distinct genera, in cichlids and in paludomid gastropods

  • Paludomids feeding on sand have comparatively soft and flexible tooth cusps, species foraging on stone have the stiffest and hardest tooth cusps (E = 6.08 ± 1.52 GPa, H = 0.26 ± 0.11 GPa), Fig. 3 Radular teeth of: a, b Bridouxia ponsonbyi Museum für Naturkunde Berlin (ZMB) 220.137-1, a overview, b marginals; c, d B. grandidieriana ZMB 220.139-4, c overview, d centrals and laterals; e, f B. rotundata ZMB 220063-1, e overview, f marginals; g, h B. praeclara ZMB 220.063-2, g overview, h marginals

  • In Group 1, Spekiini Ancey, 1906 [58], Reymondia Bourguignat, 1885 [45] and riverine Cleopatrini Pilsbry and Bequaert, 1927 [60], Group 2, Hauttecoeuriini Bourguignat, 1885 [45], Syrnolopsini, Bourguignat, 1890 [47], and Group 3, Tiphobiini Bourguignat, 1886 [46], some species feed on biofilm that covers stones, some select algae from sandy and muddy surfaces and few feed either on both (Paramelania damoni, Limnotrochus thomsoni) or on algae attached to plants and covering sand (Bridouxia grandidieriana)

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Summary

Introduction

Lake Tanganyika belongs to the East African Great Lakes and is well known for harbouring a high proportion of endemic and morphologically distinct genera, in cichlids and in paludomid gastropods. There are spectacular examples of invertebrate species flocks exhibiting a great diversity, especially among molluscs [see 31, 32], the lacustrine and riverine freshwater gastropods on Sulawesi [33,34,35,36,37,38], Madagascar [39], in the Thai rivers [40, 41], or “ancient” Lake Tanganyika [42,43,44] The latter is well known for its unique assemblage of endemic species and has been a natural laboratory for research on the drivers of evolution for decades. This eventually led to the refutation of Moore’s controversial hypothesis [61,62,63] of the lake being once directly connected to the ocean [see e.g. in 64–68]

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