Abstract

AbstractClimate‐induced habitat change has often been invoked as an important driver of speciation and evolutionary radiation in cichlid fishes, yet studies linking morphological change directly to long‐term environmental fluctuations are scarce. Here, we track changes through time in the oral dentition of Oreochromis hunteri, the endemic and only indigenous fish species inhabiting the East African crater Lake Chala (Kenya/Tanzania), in relation to climate‐driven lake‐level fluctuations during the last 25,000 yr. Fossil teeth were recovered from six periods representing alternating high and low lake‐level stands associated with late‐Pleistocene and Holocene trends in rainfall and drought. To construct a reference framework for morphological variation in fossil assemblages, we first analyzed the variability in oral tooth morphology within the modern‐day fish population. These analyses established that, like other cichlids, O. hunteri gradually replace their bicuspid/tricuspid oral dentition with more unicuspid teeth as they grow. In the fossil assemblages, we found systematic and recurrent changes in the relative abundance of these oral tooth types, with a higher proportion of unicuspids during low‐stands. Moreover, O. hunteri living during low‐stands systematically developed unicuspid dentition at a smaller body size, compared with conspecifics living during high‐stands. Considering that low‐stand conditions created a sizable area of oxygenated soft‐bottom habitat that is lacking during high‐stands, we propose that the associated change in oral dentition reflects the fishes’ exploitation of this new habitat either for feeding or for reproduction. The recurrent nature of the observed shifts provides evidence for the ability of O. hunteri to systematically adapt to local habitat change, and strongly suggests that morphological change in oral dentition promoted its long‐term population persistence in an aquatic ecosystem presenting the dual challenge of being both sensitive to climate change (creating constantly shifting selective pressures) and isolated from surrounding populations (limiting gene flow). In Lake Chala, ancient climate‐driven lake‐level fluctuations did not directly promote speciation in O. hunteri, but the population bottlenecks they may have caused potentially contributed to its divergence from sister species Oreochromis jipe.

Highlights

  • The ability of species to adapt their ecology and behavior to changing environments is a driving force of speciation (Thompson et al 2018)

  • Modern-day reference framework The standard length (SL) of the 88 O. hunteri specimens collected in Lake Chala ranged from 16 to 30 cm, with 81% of all specimens measuring between 23 and 29 cm (Fig. 2c)

  • We can use EW in fossils as a proxy of tooth length, and the EW distributions of fossil fish assemblages as an estimate of median body size

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Summary

Introduction

The ability of species to adapt their ecology and behavior to changing environments is a driving force of speciation (Thompson et al 2018). Adaptation provides ample opportunities for populations to diverge into separate species (Schluter 2000). Such ecological speciation is prominent in the cichlid fishes (Cichlidae) of the African Great Lakes, where it has rapidly produced highly diverse species flocks (Fryer and Iles 1972). In these lakes, lake-level fluctuations induced by Quaternary climate change have caused phases of extreme contraction (Lake Malawi), fragmentation (Lake Tanganyika), or even complete desiccation (Lake Victoria; reviewed by Salzburger et al 2014). Subtle differences in jaw and tooth morphology still permit them to specialize in certain ecological niches, especially during periods of food scarcity

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