Search

Climatic and geomorphological changes during the Quaternary period impacted global patterns of speciation and diversification across a wide range of taxa, but few studies have examined these effects on African riverine fish. The lower Congo River is an excellent natural laboratory for understanding complex speciation and population diversification processes, as it is hydrologically extremely dynamic and recognized as a continental hotspot of diversity harboring many narrowly endemic species. A previous study using genome-wide SNP data highlighted the importance of dynamic hydrological regimes to the diversification and speciation in lower Congo River cichlids. However, historical climate and hydrological changes (e.g. reduced river discharge during extended dry periods) have likely also influenced ichthyofaunal diversification processes in this system. The lower Congo River offers a unique opportunity to study climate-driven changes in river discharge, given the massive volume of water from the entire Congo basin flowing through this short stretch of the river. Here, we, for the first time, investigate the impacts of paleoclimatic factors on ichthyofaunal diversification in this system by inferring divergence times and modeling patterns of gene flow in four endemic lamprologine cichlids, including the blind cichlid, Lamprologus lethops. Our results suggest that Quaternary climate changes associated with river discharge fluctuations may have impacted the diversification of species along the system and the emergence of cryptophthalmic phenotype in some endemic species. Our study, using reduced representation sequencing (2RADseq), indicates that the lower Congo River lamprologines emerged during the Early-Middle Pleistocene transition, characterized as one of the earth's major climatic transformation periods. Modeling results suggest that gene flow across populations and between species was not constant but occurred in temporally constrained pulses. We show that these results correlate with glacial–interglacial fluctuations. The current hyper-diverse fish assemblages of the lower Congo River riverscape likely reflect the synergistic effects of multiple drivers fueling complex evolutionary processes through time. [ABSTRACT FROM AUTHOR]

The last decade has seen an explosion of new pedagogical programs, modules, and curricula in undergraduate STEM courses. Despite the importance of effective dissemination in spreading such programs to a broader community of users, relatively little attention is typically given to the needs of potential adopters. In this paper, we build on previous literature on dissemination and examine specific strategies implemented by programs that seek to develop new curricula across several STEM fields. We consider factors that affect likelihood of adoption from the perspectives of both potential disseminators and adopters, reviewing a set of case studies. Finally, we lay out a framework for effective dissemination of research-based STEM curricula, highlighting features that include demonstration of relative advantage over previous pedagogical methods, compatibility with departmental curricula, complexity, and trialability.

The karst aquifer of the Yucatán Peninsula (YP) in southeastern Mexico is a unique ecosystem in which water-filled sinkholes, locally known as cenotes, connect subterranean waters with the surface. This system is home to around 20 species of freshwater fishes, including several that are endemic and/or threatened. Studies on this unique ichthyofauna have been partially hampered by the technical difficulties associated with sampling these habitats, particularly submerged caves. In this proof-of-concept study, we use environmental DNA (eDNA) metabarcoding to survey the diversity of freshwater fishes associated with the YP karst aquifer by sampling six cenotes from across the Ring of Cenotes region in northwestern Yucatán, a 180-km-diameter semicircular band of abundant karst sinkholes. Through a combination of conventional sampling (direct observation, fishing) and eDNA metabarcoding, we detected eight species of freshwater fishes across the six sampled cenotes. Overall, our eDNA metabarcoding approach was effective at detecting the presence of fishes from cenote water samples, including one of the two endemic cave-dwelling fish species restricted to the subterranean section of the aquifer. Although our study was focused on detecting fishes via eDNA, we also recovered DNA from several other vertebrate groups, particularly bats. These results suggest that the eDNA metabarcoding approach represents a promising and largely noninvasive method to assay aquatic biodiversity in these vulnerable habitats, allowing more effective, frequent, and wide-ranging surveys. Our detection of DNA from aerial and terrestrial vertebrate fauna implies that eDNA from cenotes, besides being a means to survey aquatic fauna, may also offer an effective way to quickly survey non-aquatic biodiversity associated with these persistent water bodies. [ABSTRACT FROM AUTHOR]

The Yucatán Peninsula (YP) contains one of the most spectacular and developed karstic aquifers in the world, which connects to the surface through water‐filled sinkholes locally known as cenotes. Cenotes and their associated submerged caves are home to a remarkable diversity of aquatic fauna, yet very little is known about spatial patterns of intraspecific genetic and morphological variation across the aquifer. The strong affinity to cenotes (vs. submerged caves) exhibited by most fishes inhabiting the YP aquifer raises a fundamental question about the ecology and evolutionary history of its ichthyofauna: how genetically structured and morphologically divergent are fish populations from different cenotes across the YP? To shed light on this question, we investigated phylogeographic structure in the Neotropical catfish Rhamdia guatemalensis, arguably the most ubiquitous representative of the YP aquifer ichthyofauna.Geographic patterns of genetic variation were determined through phylogeographic and population genetics analyses of mitochondrial (mt)DNA sequence data. Body shape variation was investigated using both traditional and geometric morphometrics. Dense sampling across the previously overlooked YP region, coupled with the inclusion of samples from basins unrepresented in past studies, allowed for revision of previous estimates of phylogeographic structuring across the species' range.Our results reveal a striking spatial correspondence between major mtDNA lineages and physiographic regions defined on the basis of broad‐scale patterns of groundwater flow. Morphological variation in populations from the YP, although considerable, neither reflects the observed spatial signal of genetic differentiation nor displays any other discernible geographic pattern. The resulting range‐wide phylogeographic pattern is largely consistent with a latitudinal, isolation‐by‐distance gradient, and the expectations from catchment hydrology, while revealing an unexpectedly close relationship between YP aquifer and epigean populations (both inside and outside the YP).Although the inferred range‐wide phylogeographic history is consistent with a single aquifer colonisation event followed by multiple instances of dispersal out of the aquifer and into neighbouring epigean basins, hypotheses regarding the colonisation and exodus of the YP by R. guatemalensis require further investigation. Within the YP aquifer, regional‐scale hydrogeological differences might impose limits to underground dispersal, potentially driving genetic divergence in populations of R. guatemalensis, and possibly in other cenote‐dwelling fishes as well. Future research focused on other YP aquifer species, however, is needed to test the generality of our findings.Phylogeographic research on the stygofauna of the YP aquifer is a relatively nascent field of inquiry. Besides shedding novel light into the patterns and drivers of genetic differentiation in fish populations from across the aquifer, this study sets the stage for future research aimed at unravelling the evolutionary history of the stygofauna that inhabits the cenotes and submerged caves of the YP. The remarkable and hitherto undocumented phylogeographic pattern revealed herein (i.e. correspondence of major mtDNA lineages with physiographic regions defined by regional‐scale fracture zones) adds to a growing body of evidence in support of the notion that the architecture of freshwater aquifers may include physical barriers that can act as regional‐scale drivers of groundwater faunal distributions and genetic structuring. [ABSTRACT FROM AUTHOR]

The Danakil Depression in northeastern Africa represents one of the harshest arid environments on Earth, yet two genera of fishes, Danakilia (Cichlidae) and Aphanius (Cyprinodontidae), share its sparse aquatic habitats. The evolutionary history of these fishes is investigated here in the context of genetic, geological and paleoenvironmental information. We collected samples from seven sites and assessed phylogeographic relationships using concatenated COI and cytb mtDNA genes. Danakilia morphospecies show low differentiation at mitochondrial markers, but variation is partitioned between a northern cluster containing D. dinicolai plus three undescribed riverine populations, and a southern cluster including two creek populations of D. franchettii separated by the hypersaline waters of Lake Afrera. Aphanius displayed four genetically distinct clades (A. stiassnyae in Lake Afrera; one distributed across the entire area; one in Lake Abaeded; and one in the Shukoray River), but without clear large-scale geographic structure. However, Danakil Aphanius are clearly differentiated from A. dispar sensu stricto from the Sinai Peninsula. Geological evidence suggests that after the Late Pleistocene closure of the Danakil-Red Sea connection, increased post-glacial groundwater availability caused the formation of a brackish paleo-lake flooding the entire region below the -50 m contour. Fish populations previously isolated in coastal oases during glaciation were able to mix in the paleo-lake. Subsequently, in a more arid phase starting ∼7300 BP, paleo-lake regression isolated fishes in separate drainages, triggering their still ongoing diversification. [ABSTRACT FROM AUTHOR]

Accelerated loss of sea ice in the Arctic is opening routes connecting the Atlantic and Pacific Oceans for longer periods each year. These changes may increase the ease and frequency with which marine birds and mammals move between the Pacific and Atlantic Ocean basins. Indeed, recent observations of birds and mammals suggest these movements have intensified in recent decades. Reconnection of the Pacific and Atlantic Ocean basins will present both challenges to marine ecosystem conservation and an unprecedented opportunity to examine the ecological and evolutionary consequences of interoceanic faunal exchange in real time. To understand these changes and implement effective conservation of marine ecosystems, we need to further develop modeling efforts to predict the rate of dispersal and consequences of faunal exchange. These predictions can be tested by closely monitoring wildlife dispersal through the Arctic Ocean and using modern methods to explore the ecological and evolutionary consequences of these movements. [ABSTRACT FROM AUTHOR]