Inferring the evolutionary history of divergence despite gene flow in a lizard species,Scincella lateralis (Scincidae), composed of cryptic lineages

Although recent radiations are fruitful for studying the process of speciation, they are difficult to characterize and require the use of multiple loci and analytical methods that account for processes such as gene flow and genetic drift. Using multilocus sequence data, we combine hierarchical cluster analysis, coalescent species tree inference, and isolation‐with‐migration analysis to investigate evolutionary relationships among cryptic lineages of North American ground skinks. We also estimate the extent that gene flow has accompanied or followed diversification, and also attempt to account for and minimize the influence of gene flow when reconstructing relationships. The data best support seven largely parapatric populations that are broadly concordant with mitochondrial (mt)DNA phylogeography throughout most of the species range, although they fail to fully represent extensive mtDNA divergence along the Gulf Coast. Relationships within and among three broad geographical groups are well supported, despite evidence of gene flow among them. Rejection of an allopatric divergence model partially depends on the inclusion of samples from near parapatric boundaries in the analyses, suggesting that allopatric divergence followed by recent migration may best explain migration rate estimates. Accounting for geographical variation in patterns of gene flow can improve estimates of migration–divergence parameters and minimize the influence of contemporary gene flow on phylogenetic inference. © 2012 The Linnean Society of London, Biological Journal of the Linnean Society, 2012, ?? , ??–??.     

Horizon annealing: a collection‐based approach to automated sequencing of the fossil record

Sheets, H.D., Mitchell, C.E., Izard, Z.T., Willis, J.M., Melchin, M.J. & Holmden, C. 2012: Horizon annealing: a collection‐based approach to automated sequencing of the fossil record. Lethaia, Vol. 45, pp. 532–547. A number of different approaches to quantitative biochronology have been proposed and used to construct high‐resolution time‐scales for a range of uses. We present a new approach, horizon annealing, which uses simulated annealing to optimize the sequencing of collection horizons. Temporal sequences of events produced by this method are compared with those produced by graphic correlation, CONOP and RASC for a series of previously studied exemplar data sets. Horizon annealing produces results similar to other methods, but it does have properties (the ordination of collections and the avoidance of some local minima) that make it useful for high‐resolution studies, particularly those based on capture‐mark‐recapture methods requiring detailed presence–absence data for individual collections and taxa. □ Chronostratigraphy, graphic correlation, graptolite, rate of evolution, CONOP9.     

Algal biochar: effects and applications

Algae represent a promising target for the generation of bioenergy through slow pyrolysis, leading to the production of biochar. This study reports experiments conducted on the production of freshwater and saltwater macroalgal biochar in pilot‐scale quantities, the physical and chemical characteristics of the biochars, and their impact on plant growth. The biochars are low in carbon (C) content, surface area and cation exchange capacity, while being high in ash and nutrients. Trace element analysis demonstrates that macroalgal biochar produced from unpolluted water does not contain toxic trace elements in excess of levels mandated for unrestricted use as a biosolids amendment to soils. Pot trials conducted using a C and nutrient‐poor soil, without and with additional fertilizer, demonstrate dramatic increases between 15 and 32 times, respectively, in plant growth rate for biochar treatments compared with the no biochar controls, with additional smaller increases when fertilizer was added. Pot trials conducted using a relatively fertile agricultural soil showed smaller but significant impacts of biochar amendment over the controls.     

Markedly discordant mitochondrial DNA and allozyme phylogenies of tube-nosed fruit bats, Nyctimene, at the Australian–Oriental biogeographical interface

Australo-Papuan tube-nosed fruit bats of the genus Nyctimene reach their most westerly distribution on the island archipelagos of eastern Indonesia. A recent morphological examination indicates three species occur on Moluccan islands. Both allozyme electrophoresis and mitochondrial DNA (mtDNA) sequencing reveal there are only two species present, Nyctimene cephalotes and Nyctimene albiventer , but there is considerable disparity between the results obtained from the two genetic data sets. Allozyme data indicate N. albiventer occurs on Wokam, which sits on the Australian continental shelf and was joined to Australo-Papua during the last glacial maximum, and N. cephalotes on the other Moluccan islands, all of which are off the continental shelf. Divergence of these two species is dated at approximately 1.5 Mya. By contrast, the mtDNA gene tree shows two deep clades, one containing all specimens from Wokam and Yamdena, and the second all the specimens from the other islands. This especially marked incongruence between the two genetic data sets is ascribed to either a single introgression event of N. albiventer mtDNA into N. cephalotes on Yamdena at around 100 000 ya or lineage sorting of very old mtDNA lineages that coalesce a rather long time before the speciation event. These results highlight that caution should be exercised when relying on mtDNA as barcodes in species taxonomy. The continental-associated N. albiventer on Wokam has higher levels of allozyme heterozygosity and mtDNA nucleotide diversity than the N. cephalotes populations occurring on the more remote islands, indicating that this colonizing species has experienced bottlenecks and/or a low effective population size since speciation.  © 2008 The Linnean Society of London, Biological Journal of the Linnean Society , 2008, 93 , 589–602.     

Global assessment of coral bleaching and required rates of adaptation under climate change

Elevated ocean temperatures can cause coral bleaching, the loss of colour from reef‐building corals because of a breakdown of the symbiosis with the dinoflagellate Symbiodinium. Recent studies have warned that global climate change could increase the frequency of coral bleaching and threaten the long‐term viability of coral reefs. These assertions are based on projecting the coarse output from atmosphere–ocean general circulation models (GCMs) to the local conditions around representative coral reefs. Here, we conduct the first comprehensive global assessment of coral bleaching under climate change by adapting the NOAA Coral Reef Watch bleaching prediction method to the output of a low‐ and high‐climate sensitivity GCM. First, we develop and test algorithms for predicting mass coral bleaching with GCM‐resolution sea surface temperatures for thousands of coral reefs, using a global coral reef map and 1985–2002 bleaching prediction data. We then use the algorithms to determine the frequency of coral bleaching and required thermal adaptation by corals and their endosymbionts under two different emissions scenarios. The results indicate that bleaching could become an annual or biannual event for the vast majority of the world's coral reefs in the next 30–50 years without an increase in thermal tolerance of 0.2–1.0°C per decade. The geographic variability in required thermal adaptation found in each model and emissions scenario suggests that coral reefs in some regions, like Micronesia and western Polynesia, may be particularly vulnerable to climate change. Advances in modelling and monitoring will refine the forecast for individual reefs, but this assessment concludes that the global prognosis is unlikely to change without an accelerated effort to stabilize atmospheric greenhouse gas concentrations.     

The Bioarchaeology of Identity in Spanish Colonial Florida: Social and Evolutionary Transformation before, during, and after Demographic Collapse

In this article, I consider the effects of Spanish missionization on indigenous identity and biological interaction patterns. Odontometric data were recorded for 26 skeletal samples dating to three time periods: precontact (C.E. 1200–1400), early mission (C.E. 1600–1650), and late mission (C.E. 1650–1700). Population genetic analyses generated estimates of regional genetic variation (F_ST) and intersample genetic distances. Genetic variation during the precontact period was limited despite documented linguistic and cultural variation. Variation increased during the early mission period, indicating a decline in between-group interaction despite inclusion within a single colonial sociopolitical framework. During the late mission period, variation declined significantly, indicating a dramatic reduction in between-group variability consistent with genetic drift and gene flow between communities. I discuss these results in terms of archaeological and historical models of postcolonial transformation and suggest an emerging polyethnic community was resident in La Florida preceding the subsequent diaspora caused by burgeoning European military conflict in eastern North America.