Continuous 1.3-million-year record of East African hydroclimate, and implications for patterns of evolution and biodiversity.

The transport of moisture in the tropics is a critical process for the global energy budget and on geologic timescales, has markedly influenced continental landscapes, migratory pathways, and biological evolution. Here we present a continuous, first-of-its-kind 1.3-My record of continental hydroclimate and lake-level variability derived from drill core data from Lake Malawi, East Africa (9-15° S). Over the Quaternary, we observe dramatic shifts in effective moisture, resulting in large-scale changes in one of the world's largest lakes and most diverse freshwater ecosystems. Results show evidence for 24 lake level drops of more than 200 m during the Late Quaternary, including 15 lowstands when water levels were more than 400 m lower than modern. A dramatic shift is observed at the Mid-Pleistocene Transition (MPT), consistent with far-field climate forcing, which separates vastly different hydroclimate regimes before and after ∼800,000 years ago. Before 800 ka, lake levels were lower, indicating a climate drier than today, and water levels changed frequently. Following the MPT high-amplitude lake level variations dominate the record. From 800 to 100 ka, a deep, often overfilled lake occupied the basin, indicating a wetter climate, but these highstands were interrupted by prolonged intervals of extreme drought. Periods of high lake level are observed during times of high eccentricity. The extreme hydroclimate variability exerted a profound influence on the Lake Malawi endemic cichlid fish species flock; the geographically extensive habitat reconfiguration provided novel ecological opportunities, enabling new populations to differentiate rapidly to distinct species.

Chromosome-level reference genomes of two imperiled desert fishes: spikedace (Meda fulgida) and loach minnow (Tiaroga cobitis).

North American minnows (Cypriniformes: Leuciscidae) comprise a diverse taxonomic group, but many members, particularly those inhabiting deserts, face elevated extinction risks. Despite conservation concerns, leuciscids remain under sampled for reference assemblies relative to other groups of freshwater fishes. Here, we present 2 chromosome-scale reference genome assemblies spikedace (Meda fulgida) and loach minnow (Tiaroga cobitis) using PacBio, Illumina and Omni-C technologies. The complete assembly for spikedace was 882.1 Mb in total length comprised of 83 scaffolds with N50 = 34.8 Mb, L50 = 11, N75 = 32.3 Mb, and L75 = 18. The complete assembly for loach minnow was 1.3 Gb in total length comprised of 550 scaffolds with N50 = 48.6 Mb, L50 = 13, N75 = 42.3 Mb, and L75 = 20. Completeness assessed via Benchmarking Universal Single-Copy Orthologues (BUSCO) metrics using the Actinopterygii BUSCO database showed ∼97% for spikedace and ∼98% for loach minnow of complete BUSCO proportions. Annotation revealed approximately 32.58 and 29.04% of spikedace and loach minnow total genome lengths to be comprised of protein-coding genes, respectively. Comparative genomic analyses of these endangered and co-distributed fishes revealed widespread structural variants, gene family expansions, and evidence of positive selection in both genomes.

Ecological consequences of early Late Pleistocene megadroughts in tropical Africa.

Extremely arid conditions in tropical Africa occurred in several discrete episodes between 135 and 90 ka, as demonstrated by lake core and seismic records from multiple basins [Scholz CA, Johnson TC, Cohen AS, King JW, Peck J, Overpeck JT, Talbot MR, Brown ET, Kalindekafe L, Amoako PYO, et al. (2007) Proc Natl Acad Sci USA 104:16416-16421]. This resulted in extraordinarily low lake levels, even in Africa's deepest lakes. On the basis of well dated paleoecological records from Lake Malawi, which reflect both local and regional conditions, we show that this aridity had severe consequences for terrestrial and aquatic ecosystems. During the most arid phase, there was extremely low pollen production and limited charred-particle deposition, indicating insufficient vegetation to maintain substantial fires, and the Lake Malawi watershed experienced cool, semidesert conditions (<400 mm/yr precipitation). Fossil and sedimentological data show that Lake Malawi itself, currently 706 m deep, was reduced to an approximately 125 m deep saline, alkaline, well mixed lake. This episode of aridity was far more extreme than any experienced in the Afrotropics during the Last Glacial Maximum (approximately 35-15 ka). Aridity diminished after 95 ka, lake levels rose erratically, and salinity/alkalinity declined, reaching near-modern conditions after 60 ka. This record of lake levels and changing limnological conditions provides a framework for interpreting the evolution of the Lake Malawi fish and invertebrate species flocks. Moreover, this record, coupled with other regional records of early Late Pleistocene aridity, places new constraints on models of Afrotropical biogeographic refugia and early modern human population expansion into and out of tropical Africa.