Ocean acidification limits temperature-induced poleward expansion of coral habitats around Japan

Using results from four coupled global carbon cycle-climate models combined with in situ observations, we estimate the effects of future global warming and ocean acidification on potential habitats for tropical/subtropical and temperate coral communities in the seas around Japan. The suitability of coral habitats is classified on the basis of the currently observed regional ranges for temperature and saturation states with regard to aragonite (Ωarag). We find that, under the "business as usual" SRES A2 scenario, coral habitats are projected to expand northward by several hundred kilometers by the end of this century. At the same time, coral habitats are projected to become sandwiched between regions where the frequency of coral bleaching will increase, and regions where Ωarag will become too low to support sufficiently high calcification rates. As a result, the habitat suitable for tropical/subtropical corals around Japan may be reduced by half by the 2020s to 2030s, and is projected to disappear by the 2030s to 2040s. The habitat suitable for the temperate coral communities is also projected to decrease, although at a less pronounced rate, due to the higher tolerance of temperate corals for low Ωarag. Our study has two important caveats: first, it does not consider the potential adaptation of the coral communities, which would permit them to colonize habitats that are outside their current range. Second, it also does not consider whether or not coral communities can migrate quickly enough to actually occupy newly emerging habitats. As such, our results serve as a baseline for the assessment of the future evolution of coral habitats, but the consideration of important biological and ecological factors and feedbacks will be required to make more accurate projections.

Induction of apoptosis and enhancement of chemosensitivity in human prostate cancer LNCaP cells using bispecific antisense oligonucleotide targeting Bcl-2 and Bcl-xL genes

OBJECTIVE: To determine whether a specifically designed bispecific (Bcl-2/Bcl-xL) antisense oligonucleotide (ASO) induces apoptosis and enhances chemosensitivity in human prostate cancer LNCaP cells, as Bcl-2 and Bcl-xL are both anti-apoptotic genes associated with treatment resistance and tumour progression in many malignancies, including prostate cancer. MATERIALS AND METHODS: Inhibition of Bcl-2 and Bcl-xL expression by the bispecific ASO was evaluated using real-time reverse transcription-polymerase chain reaction and Western blotting, while growth inhibition and induction of apoptosis were analysed by a crystal violet assay, flow cytometry and Western blotting of apoptosis-relevant proteins. The effect of combined treatment with bispecific ASO and chemotherapy or small-interference RNA (siRNA) targeting the clusterin gene was also investigated. RESULTS: Bispecific ASO reduced Bcl-2 and Bcl-xL expression in LNCaP cells in a dose-dependent manner. There was cell growth inhibition, increases in the sub-G0-G1 fraction, and cleavage of caspase-3 and poly(ADP-Ribose) polymerase proteins in LNCaP cells after bispecific ASO treatment. Interestingly, Bcl-2/Bcl-xL bispecific ASO treatment also resulted in the down-regulation of Mcl-1 and up-regulation of Bax. The sensitivity of LNCaP cells to mitoxantrone, docetaxel or paclitaxel was significantly increased, reducing the 50% inhibitory concentration by 45%, 80% or 90%, respectively. Furthermore, the apoptotic induction by Bcl-2/Bcl-xL bispecific ASO was synergistically enhanced by siRNA-mediated inhibition of clusterin, a cytoprotective chaperone that interacts with and inhibits activated Bax. CONCLUSIONS: These findings support the concept of the targeted suppression of Bcl-2 anti-apoptotic family members using multitarget inhibition strategies for prostate cancer, through the effective induction of apoptosis.

The role of ocean transport in the uptake of anthropogenic CO2

We compare modeled oceanic carbon uptake in response to pulse CO2 emissions using a suite of global ocean models and Earth system models. In response to a CO2 pulse emission of 590 Pg C (corresponding to an instantaneous doubling of atmospheric CO2 from 278 to 556 ppm), the fraction of CO2 emitted that is absorbed by the ocean is: 37±8%, 56±10%, and 81±4% (model mean ±2σ ) in year 30, 100, and 1000 after the emission pulse, respectively. Modeled oceanic uptake of pulse CO2 on timescales from decades to about a century is strongly correlated with simulated present-day uptake of chlorofluorocarbons (CFCs) and CO2 across all models, while the amount of pulse CO2 absorbed by the ocean from a century to a millennium is strongly correlated with modeled radiocarbon in the deep Southern and Pacific Ocean. However, restricting the analysis to models that are capable of reproducing observations within uncertainty, the correlation is generally much weaker. The rates of surface-to-deep ocean transport are determined for individual models from the instantaneous doubling CO2 simulations, and they are used to calculate oceanic CO2 uptake in response to pulse CO2 emissions of different sizes pulses of 1000 and 5000 Pg C. These results are compared with simulated oceanic uptake of CO2 by a number of models simulations with the coupling of climate-ocean carbon cycle and without it. This comparison demonstrates that the impact of different ocean transport rates across models on oceanic uptake of anthropogenic CO2 is of similar magnitude as that of climate-carbon cycle feedbacks in a single model, emphasizing the important role of ocean transport in the uptake of anthropogenic CO2.

Potential Future Coral Habitats Around Japan Depend Strongly on Anthropogenic CO2 Emissions

Using the results from the NCAR CSM1.4-coupled global carbon cycle– climate model under the Intergovernmental Panel on Climate Change (IPCC) emission scenarios SRES A2 and B1, we estimated the effects of both global warming and ocean acidification on the future habitats of corals in the seas around Japan during this century. As shown by Yara et al. (Biogeosciences 9:4955–4968,2012), under the high-CO₂-emission scenario (SRES A2), coral habitats will be sandwiched and narrowed between the northern region, where the saturation state of the carbonate mineral aragonite (Ωarag) decreases, and the southern region, where coral bleaching occurs. We found that under the low-emission scenario SRES B1, the coral habitats will also shrink in the northern region by the reduced Ωarag but to a lesser extent than under SRES A2, and in contrast to SRES A2, no bleaching will occur in the southern region. Therefore, coral habitats in the southern region are expected to be largely unaffected by ocean acidification or surface warming under the low-emission scenario. Our results show that potential future coral habitats depend strongly on CO₂ emissions and emphasize the importance of reducing CO₂ emissions to prevent negative impacts on coral habitats.