Reef Fishes in Biodiversity Hotspots Are at Greatest Risk from Loss of Coral Species

Coral reef ecosystems are under a variety of threats from global change and anthropogenic disturbances that are reducing the number and type of coral species on reefs. Coral reefs support upwards of one third of all marine species of fish, so the loss of coral habitat may have substantial consequences to local fish diversity. We posit that the effects of habitat degradation will be most severe in coral regions with highest biodiversity of fishes due to greater specialization by fishes for particular coral habitats. Our novel approach to this important but untested hypothesis was to conduct the same field experiment at three geographic locations across the Indo-Pacific biodiversity gradient (Papua New Guinea; Great Barrier Reef, Australia; French Polynesia). Specifically, we experimentally explored whether the response of local fish communities to identical changes in diversity of habitat-providing corals was independent of the size of the regional species pool of fishes. We found that the proportional reduction (sensitivity) in fish biodiversity to loss of coral diversity was greater for regions with larger background species pools, reflecting variation in the degree of habitat specialization of fishes across the Indo-Pacific diversity gradient. This result implies that habitat-associated fish in diversity hotspots are at greater risk of local extinction to a given loss of habitat diversity compared to regions with lower species richness. This mechanism, related to the positive relationship between habitat specialization and regional biodiversity, and the elevated extinction risk this poses for biodiversity hotspots, may apply to species in other types of ecosystems.     

A consensus map of QTLs controlling the root length of maize

Despite their low carbon (C) content, most subsoil horizons contribute to more than half of the total soil C stocks, and therefore need to be considered in the global C cycle. Until recently, the properties and dynamics of C in deep soils was largely ignored. The aim of this review is to synthesize literature concerning the sources, composition, mechanisms of stabilisation and destabilization of soil organic matter (SOM) stored in subsoil horizons. Organic C input into subsoils occurs in dissolved form (DOC) following preferential flow pathways, as aboveground or root litter and exudates along root channels and/or through bioturbation. The relative importance of these inputs for subsoil C distribution and dynamics still needs to be evaluated. Generally, C in deep soil horizons is characterized by high mean residence times of up to several thousand years. With few exceptions, the carbon-to-nitrogen (C/N) ratio is decreasing with soil depth, while the stable C and N isotope ratios of SOM are increasing, indicating that organic matter (OM) in deep soil horizons is highly processed. Several studies suggest that SOM in subsoils is enriched in microbial-derived C compounds and depleted in energy-rich plant material compared to topsoil SOM. However, the chemical composition of SOM in subsoils is soil-type specific and greatly influenced by pedological processes. Interaction with the mineral phase, in particular amorphous iron (Fe) and aluminum (Al) oxides was reported to be the main stabilization mechanism in acid and near neutral soils. In addition, occlusion within soil aggregates has been identified to account for a great proportion of SOM preserved in subsoils. Laboratory studies have shown that the decomposition of subsoil C with high residence times could be stimulated by addition of labile C. Other mechanisms leading to destabilisation of SOM in subsoils include disruption of the physical structure and nutrient supply to soil microorganisms. One of the most important factors leading to protection of SOM in subsoils may be the spatial separation of SOM, microorganisms and extracellular enzyme activity possibly related to the heterogeneity of C input. As a result of the different processes, stabilized SOM in subsoils is horizontally stratified. In order to better understand deep SOM dynamics and to include them into soil C models, quantitative information about C fluxes resulting from C input, stabilization and destabilization processes at the field scale are necessary.     

Diet influences the intake target and mitochondrial functions of Drosophila melanogaster males

In this study, we examine the dietary protein to carbohydrate ratio (P:C) on the mitochondrial functions of two Drosophila melanogaster mtDNA haplotypes. We investigated multiple physiological parameters on flies fed with either 1:12 P:C or 1:3 P:C diets. Our results provide experimental evidence that a specific haplotype has a reduction of complex I activity when the flies are fed with the 1:12 P:C diet. This study is of particular importance to understand the influence of diet on mitochondrial evolution in invasive and broadly distributed species including humans.     

A comparison of the interaction of Chinese hamster fibroblasts with human and bovine transferrins, and conalbumin (chick-egg transferrin)

The iron requirement of a cell line of Chinese hamster fibroblasts is met more efficiently by human transferrin than by bovine transferrin or conalbumin. One possible explanation is that the binding of these transferrins to the Chinese hamster V79 cells may differ. Binding studies now show that the affinity of V79 cells for human transferrin is about 40 times greater than for bovine transferrin. Conalbumin has no detectable affinity for the human transferrin binding sites. Human apotransferrin has approximately one-sixth the affinity for the transferrin binding sites. The binding constant for the relation of human transferrin with the V79 cell is about 2.3·10⁶1· mole⁻¹, and the approximate number of binding sites per cell is 9 · 10⁵.     

Incidence and severity of injuries among juvenile crown-of-thorns starfish on Australia’s Great Barrier Reef

Coral Reefs - Outbreaks of crown-of-thorns starfish (Acanthaster spp.) represent a major threat to coral reef ecosystems throughout the Indo-Pacific, and there is significant interest in whether...     

Basic fibroblast growth factor and insulin-like growth factor I are strong mitogens for cultured mouse keratinocytes

Basic fibroblast growth factor (bFGF), but not acidic fibroblast growth factor (aFGF), was found to be mitogenic for cultured mouse keratinocytes. A six-to-nine fold increase in 3H-thymidine (3H-dT) incorporation into the acid insoluble pool and a similar increase of the labeling index can be measured when bFGF, at a concentration between 1 and 10 ng/ml, is added to keratinocytes arrested in serum-free and growth factor-free medium with a Ca++-concentration below 0.1 mM. The half-maximal response is observed between 0.2 and 0.7 ng/ml. In the same culture system, insulin-like growth factor I/somatomedin C (IGF-I) and insulin act as mitogens. IGF-I shows half-maximal stimulation with 2-3 ng/ml, insulin with 100-500 ng/ml. Basic FGF, IGF-I and insulin can be classified as strong stimulators of DNA synthesis in mouse keratinocytes. In this regard they are comparable to epidermal growth factor, which shows a half-maximal stimulation at a concentration between 1.5-2 ng/ml. These results show that in addition to mesenchymal cells, FGF is a growth factor not only for neuroectodermal cells, but ectodermal cells in general. They further support the idea that the growth promoting effect of insulin on keratinocytes may be mediated by the IGF-I receptor.