1,738 publications from this institution
The mean (±SE) depth‐integrated gross production (P) of 2,600 ± 271 mg O 2 m −2 d −1 derived from a compilation of data from nine cruises conducted between 1991–2000 in the subtropical NE Atlantic was found to be significantly lower (t‐test, P = 0.005, N = 33) than the mean (±SE) community respiration (R) of 3,821 ± 276 mg O 2 m −2 d −1 . Two‐thirds of the stations investigated were heterotrophic, and the P/R ratio of the communities tended to increase as P increased, such that communities where P < 3,000 mg O 2 m −2 d −1 tended to be heterotrophic. The tendency for R to exceed P (P/R , 1.0) was statistically significant (Wilcoxon ranked sign test, P < 0.05) in the upper and deep layers of the photic zone, with an overall balance between P and R at intermediate depths. These results provide evidence that the subtropical NE Atlantic is a heterotrophic ecosystem, where planktonic communities respire more organic carbon than they produce, thereby acting as net sources of CO 2 .
Uniform CO2 during human evolution (180 to 280 ppm) resulted, because of the role of the CO2-bicarbonate buffer in regulating pH, in rather constant pH (7.35 to 7.45) in human fluids, cells and tissues, determining, in turn, the narrow pH range for optimal functioning of the human proteome. Here we hypothesize that chronic exposure to elevated pCO2 with increasing atmospheric CO2 (>400 ppm) and extended time spent in confined, crowded indoor atmospheres (pCO2 up to 5,000 ppm) with urban lifestyles may be a major, largely overlooked, driver of changes in the performance of the human proteome. The reduced pH (downregulated from 0.1 to 0.4 units below the optimum pH) of extant humans chronically exposed to elevated CO2 is likely to lead to proteome malfunction due to protein misfolding, aggregation, charge distribution and altered interaction with other molecules (e.g. nucleic acids, metals, proteins, and drugs). Such alterations would have systemic effects helping explain the prevalence of syndromes (obesity, diabetes, respiratory diseases, osteoporosis, cancer, and neurological disorders) characteristic of the modern lifestyle. The risks chronic exposure to elevated CO2 poses to human health are too profound to be ignored and require testing with fit-for-purpose equipment and protocols along with indoor carbon capture technologies to bring CO2 levels to those (180 to 280 ppm) under which the humans proteome evolved.
During the past several decades, high numbers of gelatinous zooplankton species have been reported in many estuarine and coastal ecosystems. Coupled with media-driven public perception, a paradigm has evolved in which the global ocean ecosystems are thought to be heading toward being dominated by “nuisance” jellyfish. We question this current paradigm by presenting a broad overview of gelatinous zooplankton in a historical context to develop the hypothesis that population changes reflect the human-mediated alteration of global ocean ecosystems. To this end, we synthesize information related to the evolutionary context of contemporary gelatinous zooplankton blooms, the human frame of reference for changes in gelatinous zooplankton populations, and whether sufficient data are available to have established the paradigm. We conclude that the current paradigm in which it is believed that there has been a global increase in gelatinous zooplankton is unsubstantiated, and we develop a strategy for addressing the critical questions about long-term, human-related changes in the sea as they relate to gelatinous zooplankton blooms.
Abstract Climate change impact syntheses, such as those by the Intergovernmental Panel on Climate Change, consistently assert that limiting global warming to 1.5 °C is unlikely to safeguard most of the world’s coral reefs. This prognosis is primarily based on a small subset of available models that apply similar ‘excess heat’ threshold methodologies. Our systematic review of 79 articles projecting coral reef responses to climate change revealed five main methods. ‘Excess heat’ models constituted one third (32%) of all studies but attracted a disproportionate share (68%) of citations in the field. Most methods relied on deterministic cause-and-effect rules rather than probabilistic relationships, impeding the field’s ability to estimate uncertainty. To synthesize the available projections, we aimed to identify models with comparable outputs. However, divergent choices in model outputs and scenarios limited the analysis to a fraction of available studies. We found substantial discrepancies in the projected impacts, indicating that the subset of articles serving as a basis for climate change syntheses may project more severe consequences than other studies and methodologies. Drawing on insights from other fields, we propose methods to incorporate uncertainty into deterministic modeling approaches and propose a multi-model ensemble approach to generating probabilistic projections for coral reef futures.
The Distribution System Operators (DSO) to assure service continuity regularly resource to live working and mobile generators; however, there are specific occasions where it is not feasible to resort to these tools. Temporary shunt cables in MV lines ensure the supply/distribution of electricity to consumers but need to be licensed. This paper focus on as E-REDES, in the pursuit of higher quality assurance and faster response, created a standard project for temporary overhead MV lines with bundled cables, worked with the Directorate-General for Energy and Geology (DGEG) to establish a fast-tracking licencing of temporary lines, assembled and deployed mobile maintenance kits to strategic locations.
Trabajo presentado en Arctic Frontiers 2011, Arctic Tipping Points, celebrado en Tromso (Noruega), del 23 al 28 de enero de 2011. El libro de abstracts se publico como: 2011 Abstracts. Arctic Frontiers. The Arctic in the Earth System Perspective: the role of tiping points. Tromso: [University of Tromso, 2011]