The sedimentary archive of Crater Lake Challa in East Africa contains abundant fossil teeth of cichlid fishes throughout at least the last 25,000 years. Here, we use morphometric analyses of oral teeth from the two extant Oreochromis species inhabiting Lake Challa to explore the feasibility of tracing adaptive modification of the cichlid trophic apparatus in the lake's fossil record. We compared the performance of semi-landmark analysis (SLM) and elliptic Fourier analysis in capturing morphological variation in oral tooth crowns, and found that SLM, supplemented with tooth shaft measurements, ensured consistency with whole-body landmark analyses. Whole-body and tooth morphology data both allowed to discern between the indigenous Oreochromis hunteri and the recently introduced Oreochromis korogwe. Both species have an oral jaw arrangement of outer-row bicuspid and inner-rows tricuspid teeth, but O. hunteri has generally more slender teeth with a proportionally taller major cusp than O. korogwe, suggesting fine-scaled resource partitioning. Exploratory analysis of three fossil samples showed that the major tooth types of modern-day Oreochromis are also represented in the fossil record. Their total morphological variation is largely restricted to the morphospace occupied by contemporary teeth, suggesting a close functional relationship between ancient populations and their likely descendant, O. hunteri

Extensive transfer of tilapia between lakes throughout East Africa has often led to hybridisation with indigenous fish populations. The endemic Oreochromis hunteri of Lake Chala, an isolated crater lake near Mount Kilimanjaro, is potentially susceptible to introgression from a species formerly identified as Oreochromis korogwe, introduced * 30 years ago. We combined whole-body geometric morphometry on 104 specimens of both taxa with molecular phylogenetic analysis of mitochondrial loci from 15 O. hunteri and 9 O. cf. korogwe specimens to assess whether hybridisation has occurred. Using fishes from Lake Jipe and Nyumba ya Mungu reservoir, we expanded our analysis to all four Oreochromis species currently inhabiting the Upper Pangani River system to determine the closest relative of O. hunteri, and hence the possible source population of the ancestral species that colonised Lake Chala. Our results indicate no interbreeding occurs between O. hunteri and O. cf. korogwe, and suggest O. jipe to be the closest living relative of O. hunteri. The introduced O. cf. korogwe is a phenotypically uniform but genetically variable population, the identity of which remains unknown. The high haplotype diversity of O. hunteri is consistent with fossil evidence indicating that its ancestor colonised Lake Chala at least 25,000 years ago.

Climate‐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.

No abstract

Tropical freshwater lakes are well-known for their high biodiversity, and the East African Great Lakes in particular are renowned for their endemic cichlid fish adaptive radiations. While comparative phylogenetic analyses of extant species flocks have revealed patterns and processes of their diversification, evolutionary trajectories within lineages, impacts of environmental drivers, or the scope and nature of now-extinct diversity remain largely unknown. Time-structured paleodata from geologically young fossil records, such as fossil counts and particularly ancient DNA data, would help fill this large knowledge gap. High ambient temperatures can be detrimental to the preservation of DNA, but refined methodology now allows data generation even from very poorly preserved samples. Here, we show for the first time that fish fossils from tropical lake sediments yield endogenous ancient DNA (aDNA). Despite generally low endogenous content and high sample drop-out, high-throughput sequencing and in some cases sequence capture allowed for taxonomic assignment to family or tribe level and phylogenetic placement of individuals. Even skeletal remains weighing less than 1 mg and up to 2700 years of age could be phylogenetically placed. We find that the relationship of degradation of aDNA with the thermal age of samples is similar to that described for terrestrial samples from cold environments adjusted for elevated temperatures. Success rates and aDNA preservation differed between the investigated lakes Chala, Kivu and Victoria, possibly caused by differences in water oxygenation at deposition. Our study demonstrates that sediments of tropical lakes preserve genetic information on rapidly diversifying taxa over time scales of millennia.