Description: Coral recruitment was assessed in highly diverse and economically important Spermonde Archipelago, a reef system subjected to land-based sources of siltation/pollution and destructive fishing, over a period of 2 years. Recruitment on settlement tiles reached up to 705 spat m�2 yr�1 and was strongest in the dry season (July–October), except off-shore, where larvae settled earlier. Pocilloporidae dominated nearshore, while a more diverse community of Acroporidae, Poritidae and others settled in the less polluted mid-shelf and off-shore reefs. Non-coral fouling community appeared to hardly influence initial coral settlement on the tiles, although, this does not necessarily infer low coral post-settlement mortality, which may be enhanced at the near- and off-shore reefs as indicated by increased abundances of potential space competitors on natural substrate. Blast fishing showed no local reduction in coral recruitment and live hard coral cover increased in oligotrophic reefs, indicating potential for coral recovery, if managed effectively.

Description: Publication date: September 2013 Source: Journal of Environmental Economics and Management, Volume 66, Issue 2 Author(s): Michael Finus , Christos Kotsogiannis , Steve McCorriston Given the current trend in global emissions, the latest round of climate change negotiations at the Durban meeting of December 2011 (for the adoption of a comprehensive global treaty on climate change mitigation as soon as possible—and no later than 2015—and to come into force in 2020) has hardly shown the results one would have hoped for. Even for the most optimistic, it remains unclear whether one can expect a successful negotiating outcome by 2015. There are inherent difficulties associated with climate change negotiations, ranging from which countries should bear most responsibility for a given emission reduction target to the assessment of a globally efficient time path for pricing harmful greenhouse gas emissions (GHGs). These difficulties become even more complex and challenging under the pervasive uncertainty of climate science and the uncertainty about the feedback loop between climate change damages and economic growth. During the past decades, the environmental economics literature has provided important insights regarding the design of environmental fiscal policies and treaties but there is a host of issues that remain relatively unexplored. For instance, we know little about the cooperative solution for carbon and trade policies when climate change affects the productive possibilities of countries. In this context, it is also not obvious whether observed policies could be improved upon in such a way that all countries gain in welfare. It remains also unclear what the carbon extraction path should be in the absence of a comprehensive treaty (such as, for example, if environmental policy is unilaterally chosen subject to an agreed ‘ceiling’ in global temperature). Though carbon pricing instruments like carbon taxes, cap-and-trade and hybrids have been well studied, not much is known about their properties in the presence of ‘offset’ schemes such as the Clean Development Mechanism. More work is also required to understand the strategic implications of the uncertainty surrounding climate change and how this affects, for example, the choice of climate change strategy (‘precautionary’ or ‘wait and see’), how uncertainty impacts the propensity of countries to sign a climate treaty, and the extent to which the possibility of a climate catastrophe fosters or hinders cooperation. Understanding political economy issues is also vital in tackling climate change because efficient climate policies stand little chance of being successfully negotiated and implemented if they do not receive the support of the electorate. The papers in the special issue of the Journal of Environmental Economics and Management are precisely devoted to this broad research agenda.

Description: This paper argues that a focus on values, trust and context is vital to build a fuller understanding of public perceptions of carbon dioxide capture and storage (CCS). Empirical data from interviews conducted in the UK and Italy as part of the EU FP7-funded ECO2 project is presented to illustrate how publics and stakeholders often evaluate the geological storage of carbon dioxide in terms of its relation to their broader world views, rather than purely in terms of the perceived techno-scientific risks of the technology.

Description: Chemical (Sr, Mg) and isotopic (δ18O, 87Sr/86Sr) compositions of calcium carbonate veins (CCV) in the oceanic basement were determined to reconstruct changes in Sr/Ca and Mg/Ca of seawater in the Cenozoic. We examined CCV from 10 basement drill sites in the Atlantic and Pacific, ranging in age between 165 and 2.3 Ma. Six of these sites are from cold ridge flanks in basement 〈46 Ma, which provide direct information about seawater composition. CCV of these young sites were dated, using the Sr isotopic evolution of seawater. For the other sites, temperature-corrections were applied to correct for seawater–basement exchange processes. The combined data show that a period of constant/low Sr/Ca (4.46–6.22 mmol/mol) and Mg/Ca (1.12–2.03 mol/mol) between 165 and 30 Ma was followed by a steady increase in Mg/Ca ratios by a factor of three to modern ocean composition. Mg/Ca–Sr/Ca relations suggest that variations in hydrothermal fluxes and riverine input are likely causes driving the seawater compositional changes. However, additional forcing may be involved in explaining the timing and magnitude of changes. A plausible scenario is intensified carbonate production due to increased alkalinity input to the oceans from silicate weathering, which in turn is a result of subduction-zone recycling of CO2 from pelagic carbonate formed after the Cretaceous slow-down in ocean crust production rate.

Description: Present global warming is amplified in the Arctic and accompanied by unprecedented sea ice decline. Located along the main pathway of Atlantic Water entering the Arctic, the Barents Sea is the site of coupled feedback processes that are important for creating variability in the entire Arctic air-ice-ocean system. As warm Atlantic Water flows through the Barents Sea, it loses heat to the Arctic atmosphere. Warm periods, like today, are associated with high northward heat transport, reduced Arctic sea ice cover, and high surface air temperatures. The cooling of the Atlantic inflow creates dense water sinking to great depths in the Arctic Basins, and ~60% of the Arctic Ocean carbon uptake is removed from the carbon-saturated surface this way. Recently, anomalously large ocean heat transport has reduced sea ice formation in the Barents Sea during winter. The missing Barents Sea winter ice makes up a large part of observed winter Arctic sea ice loss, and in 2050, the Barents Sea is projected to be largely ice free throughout the year, with 4°C summer warming in the formerly ice-covered areas. The heating of the Barents atmosphere plays an important role both in “Arctic amplification” and the Arctic heat budget. The heating also perturbs the large-scale circulation through expansion of the Siberian High northward, with a possible link to recent continental wintertime cooling. Large air-ice-ocean variability is evident in proxy records of past climate conditions, suggesting that the Barents Sea has had an important role in Northern Hemisphere climate for, at least, the last 2500 years.

Description: This contribution examines studies on CCS public perception which have investigated the introduction of CCS information to the public. Studies published between 2007 and 2011 are considered and analysed with regard to research methods and tools and the construction of information. The relationship within which the communication of information takes place and content characteristics of the information emerge as two key aspects to be developed both from a methodological and an operational point of view.