Individual organisms on land and in the ocean sequester massive amounts of the carbon emitted into the atmosphere by humans. Yet the role of ecosystems as a whole in modulating this uptake of carbon is less clear. Here, we study several different mechanisms by which climate change and ecosystems could interact. We show that climate change could cause changes in ecosystems that reduce their capacity to take up carbon, further accelerating climate change. More research on – and better governance of – interactions between climate change and ecosystems is urgently required.

We examined the prevalence and correlates of Helicobacter pylori (H. pylori) infection according to cytotoxin-associated gene A (CagA) phenotype, a main virulence antigen, among the ethnically diverse population groups of Jerusalem. A cross-sectional study was undertaken in Arab (N = 959) and Jewish (N = 692) adults, randomly selected from Israel's national population registry in age-sex and population strata. Sera were tested for H. pylori immunoglobulin G (IgG) antibodies. Positive samples were tested for virulence IgG antibodies to recombinant CagA protein, by enzyme-linked immunosorbent assay. Multinomial regression models were fitted to examine associations of sociodemographic factors with H. pylori phenotypes. H. pylori IgG antibody sero-prevalence was 83.3% (95% confidence interval (CI) 80.0%–85.5%) and 61.4% (95% CI 57.7%–65.0%) among Arabs and Jews, respectively. Among H. pylori positives, the respective CagA IgG antibody sero-positivity was 42.3% (95% CI 38.9%–45.8%) and 32.5% (95% CI 28.2%–37.1%). Among Jews, being born in the Former Soviet Union, the Middle East and North Africa, vs. Israel and the Americas, was positively associated with CagA sero-positivity. In both populations, sibship size was positively associated with both CagA positive and negative phenotypes; and education was inversely associated. In conclusion, CagA positive and negative infection had similar correlates, suggesting shared sources of these two H. pylori phenotypes.

This paper seeks to contribute to understanding of the dynamics of reference relation and subordination in Tibetan grammar. As a way of shedding light on this complex topic, it examines a translated sūtra, the Ye shes rgyas pa'i mdo, which contains numerous stories relating interactions and conversations between a variety of characters. A close reading of several representative passages of this text reveals some of the systematic structures of subordination. Despite not being outlined as a principle in traditional Tibetan grammars, subordination is seen here to be clearly reinforced by, and at times entirely encoded in, the use of the converb –nas to express coreference, and in the verbal noun and converb structures –pa dang and -pa las to connote cross-reference. The paper thus aims to show how attention to the functioning of subordinating structures serves the reader in the interpretation of complex passages where such structures at times provide the only key to the attribution of agency.

Peatland development and carbon accumulation on the Pacific coast of Canada have received little attention in paleoecological studies, despite wetlands being common landscape features. Here, we present a multi–proxy paleoenvironmental study of an ombrotrophic bog in coastal British Columbia. Following decreases in relative sea level, the wetland was isolated from marine waters by 13,300 cal yr BP. Peat composition, non-pollen palynomorph, and C and N analyses demonstrate terrestrialization from an oligotrophic lake to a marsh by 11,600 cal yr BP, followed by development of a poor fen, and then a drier ombrotrophic bog by 8700 cal yr BP. Maximum carbon accumulation occurred during the early Holocene fen stage, when seasonal differences in insolation were amplified. This highlights the importance of seasonality in constraining peatland carbon sequestration by enhancing productivity during summer and reducing decomposition during winter. Pollen analysis shows that Pinus contorta dominated regional forests by 14,000 cal yr BP. Warm and relatively dry summers in the early Holocene allowed Pseudotsuga menziesii to dominate lowland forests 11,200–7000 cal yr BP. Tsuga heterophylla and P. menziesii formed coniferous forest in the mid- and late Holocene. Tephra matching the mid-Holocene Glacier Peak–Dusty Creek assemblage provides evidence of its most northwesterly occurrence to date.

This paper addresses the process towards the integration of subsurface knowledge into urban planning for three cities – Rotterdam, Glasgow and Oslo – participating in the European Cooperation in Science and Technology (COST) Action TU1206 Sub-Urban. These cities each have unique challenges in managing conflicts and opportunities in the subsurface in the planning process. The COST Sub-Urban Action has enabled a unique interaction between subsurface specialists and urban planners across over 20 European cities, and has laid the foundations for a new understanding between experts who develop subsurface knowledge and those who can benefit most from it – urban planners and decision makers. Common challenges identified include: improving planning policies, enhancing the level of awareness of the subsurface in city development and the modification of legislation to include the subsurface. The paper provides a review of the current status of subsurface planning in the three cities, each of whom are aiming to adapt their urban planning practice and legislation in light of emerging subsurface knowledge, and the current major knowledge gaps. In our opinion, there are two main routes to raise awareness that lead to improved understanding and the use of subsurface information in urban planning processes: (1) the development of a subsurface policy and (2) providing subsurface information. These measures should enable subsurface knowledge to be widely disseminated in order to manage risks and opportunities, and maximise the economic, social and environmental benefits of the urban subsurface and its services on which cities depend.