- EC| MARS
Zhou, Y.; Ma, J.; Zhang, Y.; Qin, B.; Jeppesen, E.; Jeppesen, E.
Harvested from ORCID Public Data FileJeppesen, E. in OpenAIRE Shi, K.; Brookes, J.D.; Spencer, R.G.M.; Zhu, G.; Gao, G.;Brookes, J.D.
Harvested from ORCID Public Data FileBrookes, J.D. in OpenAIREThis study highlights how Chinese economic development detrimentally impacted water quality in recent decades and how this has been improved by enormous investment in environmental remediation funded by the Chinese government. To our knowledge, this study is the first to describe the variability of surface water quality in inland waters in China, the affecting drivers behind the changes, and how the government-financed conservation actions have impacted water quality. Water quality was found to be poorest in the North and the Northeast China Plain where there is greater coverage of developed land (cities + cropland), a higher gross domestic product (GDP), and higher population density. There are significant positive relationships between the concentration of the annual mean chemical oxygen demand (COD) and the percentage of developed land use (cities + cropland), GDP, and population density in the individual watersheds (p < 0.001). During the past decade, following Chinese government-financed investments in environmental restoration and reforestation, the water quality of Chinese inland waters has improved markedly, which is particularly evident from the significant and exponentially decreasing GDP-normalized COD and ammonium (NH4+-N) concentrations. It is evident that the increasing GDP in China over the past decade did not occur at the continued expense of its inland water ecosystems. This offers hope for the future, also for other industrializing countries, that with appropriate environmental investments a high GDP can be reached and maintained, while simultaneously preserving inland aquatic ecosystems, particularly through management of sewage discharge.
161 citations 161 popularity Top 1% influence Top 10% impulse Top 1% 
Powered by BIP!add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.<script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.watres.2017.04.035&type=result"></script>'); --> </script>For further information contact us at helpdesk@openaire.eu - EC| MARS Zhou, Y.; Ma, J.; Zhang, Y.; Qin, B.; Jeppesen, E.;
Jeppesen, E.
Harvested from ORCID Public Data FileJeppesen, E. in OpenAIRE Shi, K.; Brookes, J.D.; Spencer, R.G.M.; Zhu, G.; Gao, G.;Brookes, J.D.
Harvested from ORCID Public Data FileBrookes, J.D. in OpenAIREThis study highlights how Chinese economic development detrimentally impacted water quality in recent decades and how this has been improved by enormous investment in environmental remediation funded by the Chinese government. To our knowledge, this study is the first to describe the variability of surface water quality in inland waters in China, the affecting drivers behind the changes, and how the government-financed conservation actions have impacted water quality. Water quality was found to be poorest in the North and the Northeast China Plain where there is greater coverage of developed land (cities + cropland), a higher gross domestic product (GDP), and higher population density. There are significant positive relationships between the concentration of the annual mean chemical oxygen demand (COD) and the percentage of developed land use (cities + cropland), GDP, and population density in the individual watersheds (p < 0.001). During the past decade, following Chinese government-financed investments in environmental restoration and reforestation, the water quality of Chinese inland waters has improved markedly, which is particularly evident from the significant and exponentially decreasing GDP-normalized COD and ammonium (NH4+-N) concentrations. It is evident that the increasing GDP in China over the past decade did not occur at the continued expense of its inland water ecosystems. This offers hope for the future, also for other industrializing countries, that with appropriate environmental investments a high GDP can be reached and maintained, while simultaneously preserving inland aquatic ecosystems, particularly through management of sewage discharge.
161 citations 161 popularity Top 1% influence Top 10% impulse Top 1% Powered by BIP!add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.<script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.watres.2017.04.035&type=result"></script>'); --> </script>For further information contact us at helpdesk@openaire.eu - EC| SPECS ,EC| EUPORIAS Dave MacLeod;
Dave MacLeod
Harvested from ORCID Public Data FileDave MacLeod in OpenAIRE Verónica Torralba; Melanie Davis; Francisco Doblas‐Reyes;Verónica Torralba
Harvested from ORCID Public Data FileVerónica Torralba in OpenAIREABSTRACTWind power forecasts are useful tools for power load balancing, energy trading and wind farm operations. Long range monthly‐to‐seasonal forecasting allows the prediction of departures from average weather conditions beyond traditional weather forecast timescales, months in advance. However, it has not yet been demonstrated how these forecasts can be optimally transformed to wind power. The predictable part of a seasonal forecast is for longer monthly averages, not daily averages, but to use monthly averages misses information on variability. To investigate, here a model relating average weather conditions to average wind power output was built, based on the relationship between instantaneous wind speed and power production and incorporating fluctuations in air density due to temperature and wind speed variability. Observed monthly average power output from UK stations was used to validate the model and to investigate the optimal temporal resolution for the data used to drive the model. Multiple simulations of wind power were performed based on reanalysis data, making separate simulations based on monthly, daily and sub‐daily averages, using a distribution defined by the mean across the period to incorporate information on variability. Basing the simulation on monthly averages alone is sub‐optimal: using daily average winds gives the highest correlation against observations. No improvement over this is gained by using sub‐daily averages or including temperature variability. This signifies that to transform seasonal forecasts to wind power a compromise must be made between using the daily averages with debatable skill and the more predictable monthly averages, losing information on day‐to‐day variability.
Access RoutesGreen gold Published in a Diamond OA journal add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.<script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1002/met.1660&type=result"></script>'); --> </script>For further information contact us at helpdesk@openaire.eu - EC| SPECS ,EC| EUPORIAS Dave MacLeod;
Dave MacLeod
Harvested from ORCID Public Data FileDave MacLeod in OpenAIRE Verónica Torralba; Melanie Davis; Francisco Doblas‐Reyes;Verónica Torralba
Harvested from ORCID Public Data FileVerónica Torralba in OpenAIREABSTRACTWind power forecasts are useful tools for power load balancing, energy trading and wind farm operations. Long range monthly‐to‐seasonal forecasting allows the prediction of departures from average weather conditions beyond traditional weather forecast timescales, months in advance. However, it has not yet been demonstrated how these forecasts can be optimally transformed to wind power. The predictable part of a seasonal forecast is for longer monthly averages, not daily averages, but to use monthly averages misses information on variability. To investigate, here a model relating average weather conditions to average wind power output was built, based on the relationship between instantaneous wind speed and power production and incorporating fluctuations in air density due to temperature and wind speed variability. Observed monthly average power output from UK stations was used to validate the model and to investigate the optimal temporal resolution for the data used to drive the model. Multiple simulations of wind power were performed based on reanalysis data, making separate simulations based on monthly, daily and sub‐daily averages, using a distribution defined by the mean across the period to incorporate information on variability. Basing the simulation on monthly averages alone is sub‐optimal: using daily average winds gives the highest correlation against observations. No improvement over this is gained by using sub‐daily averages or including temperature variability. This signifies that to transform seasonal forecasts to wind power a compromise must be made between using the daily averages with debatable skill and the more predictable monthly averages, losing information on day‐to‐day variability.
Access RoutesGreen gold Published in a Diamond OA journal add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.<script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1002/met.1660&type=result"></script>'); --> </script>For further information contact us at helpdesk@openaire.eu - Appleby, P. G.; Jones, V. J.; Ellis-Evans, J. C.;
Appleby, P. G.
Harvested from ORCID Public Data FileAppleby, P. G. in OpenAIRESediment cores from three lakes (Moss, Sombre and Heywood) in the maritime Antarctic (Signy Island, South Orkney Islands) have been successfully dated radiometrically by210Pb and137Cs. The core inventories of both fallout radionuclides are an order of magnitude higher than that which can be supported by the direct atmospheric flux at this latitude. The elevated values may be explained by fallout onto the catchment during the winter being delivered directly to the lakes during the annual thaw. Two of the lakes (Sombre and Heywood) show marked increases in sediment accumulation afterc. 1950. This appears to be associated with a documented rise in temperature in the South Orkney Islands, which has caused extensive deglaciation at Signy Island.
48 citations 48 popularity Top 10% influence Top 10% impulse Top 10% Powered by BIP!add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.<script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/bf00678106&type=result"></script>'); --> </script>For further information contact us at helpdesk@openaire.eu - Appleby, P. G.; Jones, V. J.; Ellis-Evans, J. C.;
Appleby, P. G.
Harvested from ORCID Public Data FileAppleby, P. G. in OpenAIRESediment cores from three lakes (Moss, Sombre and Heywood) in the maritime Antarctic (Signy Island, South Orkney Islands) have been successfully dated radiometrically by210Pb and137Cs. The core inventories of both fallout radionuclides are an order of magnitude higher than that which can be supported by the direct atmospheric flux at this latitude. The elevated values may be explained by fallout onto the catchment during the winter being delivered directly to the lakes during the annual thaw. Two of the lakes (Sombre and Heywood) show marked increases in sediment accumulation afterc. 1950. This appears to be associated with a documented rise in temperature in the South Orkney Islands, which has caused extensive deglaciation at Signy Island.
48 citations 48 popularity Top 10% influence Top 10% impulse Top 10% Powered by BIP!add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.<script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1007/bf00678106&type=result"></script>'); --> </script>For further information contact us at helpdesk@openaire.eu - CO| MAINTENANCE AND RESILIENCE OF FOUNDATIONAL SPECIES TO CLIMATE FLUCTUATIONS: ROLE OF "SUPPORTING" SPECIES INTERACTIONS ,UKRI| Environmentally regulated genes as basis for coral reef resilience ,CO| EVALUATING ECOLOGICAL RESISTANCE AND RESILIENCE TO EXTREME CLIMATE EVENTS: COMPARING CRITICAL BIOENGINEER SPECIES IN TROPICAL EASTER ISLAND AND TEMPERATE CENTRAL CHILE ,EC| INCORALSRiegl, B.; Glynn, P.W.; Wieters, E.; Purkis, S.; +2 Authors
Wieters, E.
Harvested from ORCID Public Data FileWieters, E. in OpenAIRERiegl, B.; Glynn, P.W.; Wieters, E.; Purkis, S.; D'Angelo, C.; Wiedenmann, J.;Wieters, E.
Harvested from ORCID Public Data FileWieters, E. in OpenAIREPredicted increases in seawater temperatures accelerate coral reef decline due to mortality by heat-driven coral bleaching. Alteration of the natural nutrient environment of reef corals reduces tolerance of corals to heat and light stress and thus will exacerbate impacts of global warming on reefs. Still, many reefs demonstrate remarkable regeneration from past stress events. This paper investigates the effects of sea surface temperature (SST) and water column productivity on recovery of coral reefs. In 71 Indo-Pacific sites, coral cover changes over the past 1-3 decades correlated negative-exponentially with mean SST, chlorophyll a, and SST rise. At six monitoring sites (Persian/Arabian Gulf, Red Sea, northern and southern Galápagos, Easter Island, Panama), over half of all corals were <31 years, implying that measured environmental variables indeed shaped populations and community. An Indo-Pacific-wide model suggests reefs in the northwest and central Indian Ocean, as well as the central west Pacific, are at highest risk of degradation, and those at high latitudes the least. The model pinpoints regions where coral reefs presently have the best chances for survival. However, reefs best buffered against temperature and nutrient effects are those that current studies suggest to be most at peril from future ocean acidification.
Access RoutesGreen gold 41 citations 41 popularity Top 10% influence Top 10% impulse Top 10% Powered by BIP!add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.<script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1038/srep08273&type=result"></script>'); --> </script>For further information contact us at helpdesk@openaire.eu - CO| MAINTENANCE AND RESILIENCE OF FOUNDATIONAL SPECIES TO CLIMATE FLUCTUATIONS: ROLE OF "SUPPORTING" SPECIES INTERACTIONS ,UKRI| Environmentally regulated genes as basis for coral reef resilience ,CO| EVALUATING ECOLOGICAL RESISTANCE AND RESILIENCE TO EXTREME CLIMATE EVENTS: COMPARING CRITICAL BIOENGINEER SPECIES IN TROPICAL EASTER ISLAND AND TEMPERATE CENTRAL CHILE ,EC| INCORALSRiegl, B.; Glynn, P.W.; Wieters, E.; Purkis, S.; +2 Authors
Wieters, E.
Harvested from ORCID Public Data FileWieters, E. in OpenAIRERiegl, B.; Glynn, P.W.; Wieters, E.; Purkis, S.; D'Angelo, C.; Wiedenmann, J.;Wieters, E.
Harvested from ORCID Public Data FileWieters, E. in OpenAIREPredicted increases in seawater temperatures accelerate coral reef decline due to mortality by heat-driven coral bleaching. Alteration of the natural nutrient environment of reef corals reduces tolerance of corals to heat and light stress and thus will exacerbate impacts of global warming on reefs. Still, many reefs demonstrate remarkable regeneration from past stress events. This paper investigates the effects of sea surface temperature (SST) and water column productivity on recovery of coral reefs. In 71 Indo-Pacific sites, coral cover changes over the past 1-3 decades correlated negative-exponentially with mean SST, chlorophyll a, and SST rise. At six monitoring sites (Persian/Arabian Gulf, Red Sea, northern and southern Galápagos, Easter Island, Panama), over half of all corals were <31 years, implying that measured environmental variables indeed shaped populations and community. An Indo-Pacific-wide model suggests reefs in the northwest and central Indian Ocean, as well as the central west Pacific, are at highest risk of degradation, and those at high latitudes the least. The model pinpoints regions where coral reefs presently have the best chances for survival. However, reefs best buffered against temperature and nutrient effects are those that current studies suggest to be most at peril from future ocean acidification.
Access RoutesGreen gold 41 citations 41 popularity Top 10% influence Top 10% impulse Top 10% Powered by BIP!add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.<script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1038/srep08273&type=result"></script>'); --> </script>For further information contact us at helpdesk@openaire.eu - M. Hoffmann; C. Hilton Taylor; A. Angulo; M. Bohm; +170 Authors
M. Hoffmann
Harvested from ORCID Public Data FileM. Hoffmann in OpenAIRE M. Hoffmann; C. Hilton Taylor; A. Angulo; M. Bohm;M. Hoffmann
Harvested from ORCID Public Data FileM. Hoffmann in OpenAIRE T. M. Brooks; T. M. Brooks
Harvested from ORCID Public Data FileT. M. Brooks in OpenAIRE S. H. M. Butchart; K. E. Carpenter; J. Chanson;S. H. M. Butchart
Harvested from ORCID Public Data FileS. H. M. Butchart in OpenAIRE B. Collen; N. A. Cox; W. R. T. Darwall; N. K. Dulvy; L. R. Harrison; V. Katariya; C. M. Pollock; S. Quader;N. K. Dulvy
Harvested from ORCID Public Data FileN. K. Dulvy in OpenAIRE N. I. Richman; N. I. Richman
Harvested from ORCID Public Data FileN. I. Richman in OpenAIRE A. S. L. Rodrigues; A. S. L. Rodrigues
Harvested from ORCID Public Data FileA. S. L. Rodrigues in OpenAIRE M. F. Tognelli; J. C. Vie; J. M. Aguiar; D. J. Allen; G. R. Allen; G. Amori; N. B. Ananjeva;M. F. Tognelli
Harvested from ORCID Public Data FileM. F. Tognelli in OpenAIRE F. Andreone; P. Andrew; A. L. A. Ortiz; J. E. M. Baillie; R. Baldi; B. D. Bell; S. D. Biju; J. P. Bird; P. Black Decima;F. Andreone
Harvested from ORCID Public Data FileF. Andreone in OpenAIRE J. J. Blanc; F. Bolanos; W. Bolivar G; I. J. Burfield; J. A. Burton; D. R. Capper;J. J. Blanc
Harvested from ORCID Public Data FileJ. J. Blanc in OpenAIRE F. Castro; G. Catullo; R. D. Cavanagh; A. Channing; N. L. Chao; A. M. Chenery; CHIOZZA, Federica; V. Clausnitzer; N. J. Collar; L. C. Collett; B. B. Collette; C. F. C. Fernandez; M. T. Craig; M. J. Crosby; N. Cumberlidge; A. Cuttelod; A. E. Derocher; A. E. Derocher
Harvested from ORCID Public Data FileA. E. Derocher in OpenAIRE A. C. Diesmos; A. C. Diesmos
Harvested from ORCID Public Data FileA. C. Diesmos in OpenAIRE J. S. Donaldson; J. W. Duckworth; G. Dutson; S. K. Dutta; R. H. Emslie; A. Farjon; S. Fowler; J. Freyhof; D. L. Garshelis;J. S. Donaldson
Harvested from ORCID Public Data FileJ. S. Donaldson in OpenAIRE J. Gerlach; D. J. Gower; T. D. Grant; G. A. Hammerson; R. B. Harris; L. R. Heaney; S. B. Hedges; J. M. Hero; B. Hughes; S. A. Hussain; J. Icochea M; R. F. Inger; N. Ishii;J. Gerlach
Harvested from ORCID Public Data FileJ. Gerlach in OpenAIRE D. T. Iskandar; R. K. B. Jenkins; Y. Kaneko; M. Kottelat; K. M. Kovacs; S. L. Kuzmin; E. La Marca; J. F. Lamoreux; M. W. N. Lau;D. T. Iskandar
Harvested from ORCID Public Data FileD. T. Iskandar in OpenAIRE E. O. Lavilla; K. Leus; R. L. Lewison;E. O. Lavilla
Harvested from ORCID Public Data FileE. O. Lavilla in OpenAIRE G. Lichtenstein; S. R. Livingstone;G. Lichtenstein
Harvested from ORCID Public Data FileG. Lichtenstein in OpenAIRE V. Lukoschek; D. P. Mallon; P. J. K. Mcgowan; A. Mcivor; P. D. Moehlman;V. Lukoschek
Harvested from ORCID Public Data FileV. Lukoschek in OpenAIRE S. Molur; A. M. Alonso; J. A. Musick; K. Nowell; R. A. Nussbaum; W. Olech; N. L. Orlov; T. J. Papenfuss; G. Parra Olea; W. F. Perrin; B. A. Polidoro; M. Pourkazemi; P. A. Racey;M. Pourkazemi
Harvested from ORCID Public Data FileM. Pourkazemi in OpenAIRE J. S. Ragle; M. Ram; G. Rathbun; R. P. Reynolds; A. G. J. Rhodin; S. J. Richards;J. S. Ragle
Harvested from ORCID Public Data FileJ. S. Ragle in OpenAIRE L. O. Rodriguez; L. O. Rodriguez
Harvested from ORCID Public Data FileL. O. Rodriguez in OpenAIRE S. R. Ron; RONDININI, CARLO; A. B. Rylands; Y. Sadovy De Mitcheson;RONDININI, CARLO
Harvested from ORCID Public Data FileRONDININI, CARLO in OpenAIRE J. C. Sanciangco; K. L. Sanders; G. Santos Barrera;J. C. Sanciangco
Harvested from ORCID Public Data FileJ. C. Sanciangco in OpenAIRE J. Schipper; J. Schipper
Harvested from ORCID Public Data FileJ. Schipper in OpenAIRE C. Self Sullivan; Y. C. Shi; A. Shoemaker; F. T. Short; C. Sillero Zubiri;C. Self Sullivan
Harvested from ORCID Public Data FileC. Self Sullivan in OpenAIRE D. L. Silvano; K. G. Smith; A. T. Smith; J. Snoeks; A. J. Stattersfield; A. J. Symes; A. B. Taber; B. K. Talukdar; H. J. Temple; R. Timmins;D. L. Silvano
Harvested from ORCID Public Data FileD. L. Silvano in OpenAIRE J. A. Tobias; K. Tsytsulina; D. Tweddle;J. A. Tobias
Harvested from ORCID Public Data FileJ. A. Tobias in OpenAIRE C. Ubeda; S. V. Valenti; P. Paul Van Dijk; L. M. Veiga; A. Veloso; D. C. Wege; M. Wilkinson; E. A. Williamson; F. Xie; B. E. Young; H. R. Akcakaya; L. Bennun; T. M. Blackburn;E. A. Williamson
Harvested from ORCID Public Data FileE. A. Williamson in OpenAIRE
BOITANI, Luigi; H. T. Dublin; G. A. B. Da Fonseca; C. Gascon; T. E. Lacher;BOITANI, Luigi
Derived by OpenAIRE algorithms or harvested from 3rd party repositoriesBOITANI, Luigi in OpenAIRE G. M. Mace; S. A. Mainka; J. A. Mcneely; R. A. Mittermeier; G. M. Reid;G. M. Mace
Harvested from ORCID Public Data FileG. M. Mace in OpenAIRE J. P. Rodriguez; A. A. Rosenberg;J. P. Rodriguez
Harvested from ORCID Public Data FileJ. P. Rodriguez in OpenAIRE M. J. Samways; J. Smart; B. A. Stein; S. N. Stuart;M. J. Samways
Harvested from ORCID Public Data FileM. J. Samways in OpenAIREAssessing Biodiversity Declines Understanding human impact on biodiversity depends on sound quantitative projection. Pereira et al. (p. 1496 , published online 26 October) review quantitative scenarios that have been developed for four main areas of concern: species extinctions, species abundances and community structure, habitat loss and degradation, and shifts in the distribution of species and biomes. Declines in biodiversity are projected for the whole of the 21st century in all scenarios, but with a wide range of variation. Hoffmann et al. (p. 1503 , published online 26 October) draw on the results of five decades' worth of data collection, managed by the International Union for Conservation of Nature Species Survival Commission. A comprehensive synthesis of the conservation status of the world's vertebrates, based on an analysis of 25,780 species (approximately half of total vertebrate diversity), is presented: Approximately 20% of all vertebrate species are at risk of extinction in the wild, and 11% of threatened birds and 17% of threatened mammals have moved closer to extinction over time. Despite these trends, overall declines would have been significantly worse in the absence of conservation actions.
Access RoutesGreen bronze 1K citations 1,221 popularity Top 0.1% influence Top 0.1% impulse Top 0.1% Powered by BIP!add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.<script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1126/science.1194442&type=result"></script>'); --> </script>For further information contact us at helpdesk@openaire.eu - M. Hoffmann; C. Hilton Taylor; A. Angulo; M. Bohm; +170 Authors
M. Hoffmann
Harvested from ORCID Public Data FileM. Hoffmann in OpenAIRE M. Hoffmann; C. Hilton Taylor; A. Angulo; M. Bohm;M. Hoffmann
Harvested from ORCID Public Data FileM. Hoffmann in OpenAIRE T. M. Brooks; T. M. Brooks
Harvested from ORCID Public Data FileT. M. Brooks in OpenAIRE S. H. M. Butchart; K. E. Carpenter; J. Chanson;S. H. M. Butchart
Harvested from ORCID Public Data FileS. H. M. Butchart in OpenAIRE B. Collen; N. A. Cox; W. R. T. Darwall; N. K. Dulvy; L. R. Harrison; V. Katariya; C. M. Pollock; S. Quader;N. K. Dulvy
Harvested from ORCID Public Data FileN. K. Dulvy in OpenAIRE N. I. Richman; N. I. Richman
Harvested from ORCID Public Data FileN. I. Richman in OpenAIRE A. S. L. Rodrigues; A. S. L. Rodrigues
Harvested from ORCID Public Data FileA. S. L. Rodrigues in OpenAIRE M. F. Tognelli; J. C. Vie; J. M. Aguiar; D. J. Allen; G. R. Allen; G. Amori; N. B. Ananjeva;M. F. Tognelli
Harvested from ORCID Public Data FileM. F. Tognelli in OpenAIRE F. Andreone; P. Andrew; A. L. A. Ortiz; J. E. M. Baillie; R. Baldi; B. D. Bell; S. D. Biju; J. P. Bird; P. Black Decima;F. Andreone
Harvested from ORCID Public Data FileF. Andreone in OpenAIRE J. J. Blanc; F. Bolanos; W. Bolivar G; I. J. Burfield; J. A. Burton; D. R. Capper;J. J. Blanc
Harvested from ORCID Public Data FileJ. J. Blanc in OpenAIRE F. Castro; G. Catullo; R. D. Cavanagh; A. Channing; N. L. Chao; A. M. Chenery; CHIOZZA, Federica; V. Clausnitzer; N. J. Collar; L. C. Collett; B. B. Collette; C. F. C. Fernandez; M. T. Craig; M. J. Crosby; N. Cumberlidge; A. Cuttelod; A. E. Derocher; A. E. Derocher
Harvested from ORCID Public Data FileA. E. Derocher in OpenAIRE A. C. Diesmos; A. C. Diesmos
Harvested from ORCID Public Data FileA. C. Diesmos in OpenAIRE J. S. Donaldson; J. W. Duckworth; G. Dutson; S. K. Dutta; R. H. Emslie; A. Farjon; S. Fowler; J. Freyhof; D. L. Garshelis;J. S. Donaldson
Harvested from ORCID Public Data FileJ. S. Donaldson in OpenAIRE J. Gerlach; D. J. Gower; T. D. Grant; G. A. Hammerson; R. B. Harris; L. R. Heaney; S. B. Hedges; J. M. Hero; B. Hughes; S. A. Hussain; J. Icochea M; R. F. Inger; N. Ishii;J. Gerlach
Harvested from ORCID Public Data FileJ. Gerlach in OpenAIRE D. T. Iskandar; R. K. B. Jenkins; Y. Kaneko; M. Kottelat; K. M. Kovacs; S. L. Kuzmin; E. La Marca; J. F. Lamoreux; M. W. N. Lau;D. T. Iskandar
Harvested from ORCID Public Data FileD. T. Iskandar in OpenAIRE E. O. Lavilla; K. Leus; R. L. Lewison;E. O. Lavilla
Harvested from ORCID Public Data FileE. O. Lavilla in OpenAIRE G. Lichtenstein; S. R. Livingstone;G. Lichtenstein
Harvested from ORCID Public Data FileG. Lichtenstein in OpenAIRE V. Lukoschek; D. P. Mallon; P. J. K. Mcgowan; A. Mcivor; P. D. Moehlman;V. Lukoschek
Harvested from ORCID Public Data FileV. Lukoschek in OpenAIRE S. Molur; A. M. Alonso; J. A. Musick; K. Nowell; R. A. Nussbaum; W. Olech; N. L. Orlov; T. J. Papenfuss; G. Parra Olea; W. F. Perrin; B. A. Polidoro; M. Pourkazemi; P. A. Racey;M. Pourkazemi
Harvested from ORCID Public Data FileM. Pourkazemi in OpenAIRE J. S. Ragle; M. Ram; G. Rathbun; R. P. Reynolds; A. G. J. Rhodin; S. J. Richards;J. S. Ragle
Harvested from ORCID Public Data FileJ. S. Ragle in OpenAIRE L. O. Rodriguez; L. O. Rodriguez
Harvested from ORCID Public Data FileL. O. Rodriguez in OpenAIRE S. R. Ron; RONDININI, CARLO; A. B. Rylands; Y. Sadovy De Mitcheson;RONDININI, CARLO
Harvested from ORCID Public Data FileRONDININI, CARLO in OpenAIRE J. C. Sanciangco; K. L. Sanders; G. Santos Barrera;J. C. Sanciangco
Harvested from ORCID Public Data FileJ. C. Sanciangco in OpenAIRE J. Schipper; J. Schipper
Harvested from ORCID Public Data FileJ. Schipper in OpenAIRE C. Self Sullivan; Y. C. Shi; A. Shoemaker; F. T. Short; C. Sillero Zubiri;C. Self Sullivan
Harvested from ORCID Public Data FileC. Self Sullivan in OpenAIRE D. L. Silvano; K. G. Smith; A. T. Smith; J. Snoeks; A. J. Stattersfield; A. J. Symes; A. B. Taber; B. K. Talukdar; H. J. Temple; R. Timmins;D. L. Silvano
Harvested from ORCID Public Data FileD. L. Silvano in OpenAIRE J. A. Tobias; K. Tsytsulina; D. Tweddle;J. A. Tobias
Harvested from ORCID Public Data FileJ. A. Tobias in OpenAIRE C. Ubeda; S. V. Valenti; P. Paul Van Dijk; L. M. Veiga; A. Veloso; D. C. Wege; M. Wilkinson; E. A. Williamson; F. Xie; B. E. Young; H. R. Akcakaya; L. Bennun; T. M. Blackburn;E. A. Williamson
Harvested from ORCID Public Data FileE. A. Williamson in OpenAIRE BOITANI, Luigi; H. T. Dublin; G. A. B. Da Fonseca; C. Gascon; T. E. Lacher;BOITANI, Luigi
Derived by OpenAIRE algorithms or harvested from 3rd party repositoriesBOITANI, Luigi in OpenAIRE G. M. Mace; S. A. Mainka; J. A. Mcneely; R. A. Mittermeier; G. M. Reid;G. M. Mace
Harvested from ORCID Public Data FileG. M. Mace in OpenAIRE J. P. Rodriguez; A. A. Rosenberg;J. P. Rodriguez
Harvested from ORCID Public Data FileJ. P. Rodriguez in OpenAIRE M. J. Samways; J. Smart; B. A. Stein; S. N. Stuart;M. J. Samways
Harvested from ORCID Public Data FileM. J. Samways in OpenAIREAssessing Biodiversity Declines Understanding human impact on biodiversity depends on sound quantitative projection. Pereira et al. (p. 1496 , published online 26 October) review quantitative scenarios that have been developed for four main areas of concern: species extinctions, species abundances and community structure, habitat loss and degradation, and shifts in the distribution of species and biomes. Declines in biodiversity are projected for the whole of the 21st century in all scenarios, but with a wide range of variation. Hoffmann et al. (p. 1503 , published online 26 October) draw on the results of five decades' worth of data collection, managed by the International Union for Conservation of Nature Species Survival Commission. A comprehensive synthesis of the conservation status of the world's vertebrates, based on an analysis of 25,780 species (approximately half of total vertebrate diversity), is presented: Approximately 20% of all vertebrate species are at risk of extinction in the wild, and 11% of threatened birds and 17% of threatened mammals have moved closer to extinction over time. Despite these trends, overall declines would have been significantly worse in the absence of conservation actions.
Access RoutesGreen bronze 1K citations 1,221 popularity Top 0.1% influence Top 0.1% impulse Top 0.1% Powered by BIP!add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.<script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1126/science.1194442&type=result"></script>'); --> </script>For further information contact us at helpdesk@openaire.eu - Sterken, Mieke; Roberts, Stephen;
Roberts, Stephen
Harvested from ORCID Public Data FileRoberts, Stephen in OpenAIRE Hodgson, Dominic; Vyverman, Wim; +4 AuthorsHodgson, Dominic
Derived by OpenAIRE algorithms or harvested from 3rd party repositoriesHodgson, Dominic in OpenAIRESterken, Mieke; Roberts, Stephen; Roberts, Stephen
Harvested from ORCID Public Data FileRoberts, Stephen in OpenAIRE Hodgson, Dominic; Vyverman, Wim;Hodgson, Dominic
Derived by OpenAIRE algorithms or harvested from 3rd party repositoriesHodgson, Dominic in OpenAIRE Balbo, Andrea L.; Sabbe, Koen;Balbo, Andrea L.
Harvested from ORCID Public Data FileBalbo, Andrea L. in OpenAIRE Moreton, Steven G.; Verleyen, Elie;Moreton, Steven G.
Harvested from ORCID Public Data FileMoreton, Steven G. in OpenAIREThe Antarctic Peninsula is one of the most rapidly warming regions on Earth, as evidenced by a recent increase in the intensity and duration of summer melting, the recession of glaciers and the retreat and collapse of ice shelves. Despite this, only a limited number of well-dated near shore marine and lake sediment based palaeoenvironmental records exist from this region; so our understanding of the longer-term context of this rapid climate change is limited. Here we provide new well-dated constraints on the deglaciation history, and changes in sea ice and climate based on analyses of sedimentological proxies, diatoms and fossil pigments in a sediment core collected from an isolation basin on Beak Island in Prince Gustav Channel, NE Antarctic Peninsula (63°36′S, 57°20′W). Twenty two radiocarbon dates provided a chronology for the core including a minimum modelled age for deglaciation of 10,602 cal yr BP, following the onset of marine sedimentation. Conditions remained cold and perennial sea ice persisted in this part of Prince Gustav Channel until c. 9372 cal yr BP. This was followed by a seasonally open marine environment until at least 6988 cal yr BP, corresponding with the early retreat and disintegration of the ice shelf in southern Prince Gustav Channel. Following isolation of the basin from 6988 cal yr BP a relatively cold climate persisted until 3169 cal yr BP. A Mid-late Holocene climate optimum occurred between 3169 and 2120 cal yr BP, inferred from multiple indicators of increased biological production. This postdates the onset of the Mid-late Holocene climate optimum in the South Shetland Islands (4380 cal yr BP) and the South Orkney Islands (3800 cal yr BP) suggesting that cooler climate systems of the Weddell Sea Gyre to the east of the Peninsula may have buffered the onset of warming. Climate deterioration is inferred from c. 2120 cal yr BP until 543 cal yr BP. This was followed by warming. Superimposed on this warming trend, the instrumental record of recent warming at nearby Hope Bay is mirrored by a recent increase in the lake’s primary production and a shift in the diatom communities in the uppermost 3 cm of sediments, suggesting that this is amongst the first records to show an ecological response to recent rapid temperature increase. These new constraints on glaciological and climate events in Prince Gustav Channel are reviewed in the context of wider changes in the Antarctic region. Peer reviewed
Access RoutesGreen add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.<script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.quascirev.2011.10.017&type=result"></script>'); --> </script>For further information contact us at helpdesk@openaire.eu - Sterken, Mieke; Roberts, Stephen;
Roberts, Stephen
Harvested from ORCID Public Data FileRoberts, Stephen in OpenAIRE Hodgson, Dominic; Vyverman, Wim; +4 AuthorsHodgson, Dominic
Derived by OpenAIRE algorithms or harvested from 3rd party repositoriesHodgson, Dominic in OpenAIRESterken, Mieke; Roberts, Stephen; Roberts, Stephen
Harvested from ORCID Public Data FileRoberts, Stephen in OpenAIRE Hodgson, Dominic; Vyverman, Wim;Hodgson, Dominic
Derived by OpenAIRE algorithms or harvested from 3rd party repositoriesHodgson, Dominic in OpenAIRE Balbo, Andrea L.; Sabbe, Koen;Balbo, Andrea L.
Harvested from ORCID Public Data FileBalbo, Andrea L. in OpenAIRE Moreton, Steven G.; Verleyen, Elie;Moreton, Steven G.
Harvested from ORCID Public Data FileMoreton, Steven G. in OpenAIREThe Antarctic Peninsula is one of the most rapidly warming regions on Earth, as evidenced by a recent increase in the intensity and duration of summer melting, the recession of glaciers and the retreat and collapse of ice shelves. Despite this, only a limited number of well-dated near shore marine and lake sediment based palaeoenvironmental records exist from this region; so our understanding of the longer-term context of this rapid climate change is limited. Here we provide new well-dated constraints on the deglaciation history, and changes in sea ice and climate based on analyses of sedimentological proxies, diatoms and fossil pigments in a sediment core collected from an isolation basin on Beak Island in Prince Gustav Channel, NE Antarctic Peninsula (63°36′S, 57°20′W). Twenty two radiocarbon dates provided a chronology for the core including a minimum modelled age for deglaciation of 10,602 cal yr BP, following the onset of marine sedimentation. Conditions remained cold and perennial sea ice persisted in this part of Prince Gustav Channel until c. 9372 cal yr BP. This was followed by a seasonally open marine environment until at least 6988 cal yr BP, corresponding with the early retreat and disintegration of the ice shelf in southern Prince Gustav Channel. Following isolation of the basin from 6988 cal yr BP a relatively cold climate persisted until 3169 cal yr BP. A Mid-late Holocene climate optimum occurred between 3169 and 2120 cal yr BP, inferred from multiple indicators of increased biological production. This postdates the onset of the Mid-late Holocene climate optimum in the South Shetland Islands (4380 cal yr BP) and the South Orkney Islands (3800 cal yr BP) suggesting that cooler climate systems of the Weddell Sea Gyre to the east of the Peninsula may have buffered the onset of warming. Climate deterioration is inferred from c. 2120 cal yr BP until 543 cal yr BP. This was followed by warming. Superimposed on this warming trend, the instrumental record of recent warming at nearby Hope Bay is mirrored by a recent increase in the lake’s primary production and a shift in the diatom communities in the uppermost 3 cm of sediments, suggesting that this is amongst the first records to show an ecological response to recent rapid temperature increase. These new constraints on glaciological and climate events in Prince Gustav Channel are reviewed in the context of wider changes in the Antarctic region. Peer reviewed
Access RoutesGreen add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.<script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.quascirev.2011.10.017&type=result"></script>'); --> </script>For further information contact us at helpdesk@openaire.eu - EC| MARINA PLATFORM Erwan Garel; Cibran Camba Rey;
Erwan Garel
Harvested from ORCID Public Data FileErwan Garel in OpenAIRE Óscar Ferreira; Óscar Ferreira
Harvested from ORCID Public Data FileÓscar Ferreira in OpenAIRE Mark van Koningsveld; Mark van Koningsveld
Harvested from ORCID Public Data FileMark van Koningsveld in OpenAIREThis paper assesses the applicability of the Frame of Reference (FoR) approach for the environmental monitoring of large-scale offshore Marine Renewable Energy (MRE) projects. The focus is on projects harvesting energy from winds, waves and currents. Environmental concerns induced by MRE projects are reported based on a classification scheme identifying stressors, receptors, effects and impacts. Although the potential effects of stressors on most receptors are identified, there are large knowledge gaps regarding the corresponding (positive and negative) impacts. In that context, the development of offshore MRE requires the implementation of fit-for-purpose monitoring activities aimed at environmental protection and knowledge development. Taking European legislation as an example, it is suggested to adopt standardized monitoring protocols for the enhanced usage and utility of environmental indicators. Towards this objective, the use of the FoR approach is advocated since it provides guidance for the definition and use of coherent set of environmental state indicators. After a description of this framework, various examples of applications are provided considering a virtual MRE project located in European waters. Finally, some conclusions and recommendations are provided for the successful implementation of the FoR approach and for future studies.
Access RoutesGreen hybrid add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.<script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.jenvman.2014.02.037&type=result"></script>'); --> </script>For further information contact us at helpdesk@openaire.eu - EC| MARINA PLATFORM Erwan Garel; Cibran Camba Rey;
Erwan Garel
Harvested from ORCID Public Data FileErwan Garel in OpenAIRE Óscar Ferreira; Óscar Ferreira
Harvested from ORCID Public Data FileÓscar Ferreira in OpenAIRE Mark van Koningsveld; Mark van Koningsveld
Harvested from ORCID Public Data FileMark van Koningsveld in OpenAIREThis paper assesses the applicability of the Frame of Reference (FoR) approach for the environmental monitoring of large-scale offshore Marine Renewable Energy (MRE) projects. The focus is on projects harvesting energy from winds, waves and currents. Environmental concerns induced by MRE projects are reported based on a classification scheme identifying stressors, receptors, effects and impacts. Although the potential effects of stressors on most receptors are identified, there are large knowledge gaps regarding the corresponding (positive and negative) impacts. In that context, the development of offshore MRE requires the implementation of fit-for-purpose monitoring activities aimed at environmental protection and knowledge development. Taking European legislation as an example, it is suggested to adopt standardized monitoring protocols for the enhanced usage and utility of environmental indicators. Towards this objective, the use of the FoR approach is advocated since it provides guidance for the definition and use of coherent set of environmental state indicators. After a description of this framework, various examples of applications are provided considering a virtual MRE project located in European waters. Finally, some conclusions and recommendations are provided for the successful implementation of the FoR approach and for future studies.
Access RoutesGreen hybrid add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.<script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.jenvman.2014.02.037&type=result"></script>'); --> </script>For further information contact us at helpdesk@openaire.eu - Dal Corso J.[1; 2; 3; 4]; +17 Authors
Dal Corso J.[1
Harvested from ORCID Public Data FileDal Corso J.[1 in OpenAIRE Dal Corso J.[1; 2; 3; 4];Dal Corso J.[1
Harvested from ORCID Public Data FileDal Corso J.[1 in OpenAIRE Gianolla P. [2]; Gianolla P. [2]
Harvested from ORCID Public Data FileGianolla P. [2] in OpenAIRE Rigo M.[3; 5]; Franceschi M.[3]; Franceschi M.[3]
Harvested from ORCID Public Data FileFranceschi M.[3] in OpenAIRE Roghi G.[5]; Mietto P.[3]; Manfrin S.[3];Roghi G.[5]
Harvested from ORCID Public Data FileRoghi G.[5] in OpenAIRE Raucsik B.[6]; Budai T.[7];Raucsik B.[6]
Harvested from ORCID Public Data FileRaucsik B.[6] in OpenAIRE Jenkyns H.[8]; Jenkyns H.[8]
Derived by OpenAIRE algorithms or harvested from 3rd party repositoriesJenkyns H.[8] in OpenAIRE Reymond C.[4]; Reymond C.[4]
Harvested from ORCID Public Data FileReymond C.[4] in OpenAIRE Caggiati M.[2]; Gattolin G.[9];Caggiati M.[2]
Harvested from ORCID Public Data FileCaggiati M.[2] in OpenAIRE Breda A.[3]; Breda A.[3]
Harvested from ORCID Public Data FileBreda A.[3] in OpenAIRE Merico A.[4; 10];Merico A.[4
Harvested from ORCID Public Data FileMerico A.[4 in OpenAIRE Preto N. [3]; Preto N. [3]
Derived by OpenAIRE algorithms or harvested from 3rd party repositoriesPreto N. [3] in OpenAIREThe Carnian Pluvial Episode was a phase of global climatic change and biotic turnover that occurred during the early Late Triassic. In marine sedimentary basins, the arrival of huge amounts of siliciclastic sediments, the establishment of anoxic conditions, and a sudden change of the carbonate factory on platforms marked the Carnian Pluvial Episode. The sedimentary changes are closely associated with abrupt biological turnover among marine and terrestrial groups as, for example, an extinction among ammonoids and conodonts in the ocean, and a turnover of the vertebrate fauna and the flora on land. Multiple negative carbon-isotope excursions were recorded during the Carnian Pluvial Episode in both organic matter and marine carbonates, suggesting repeated injection of 13C-depleted CO2 into the ocean-atmosphere system, but their temporal and causal links with the sedimentological and palaeontological changes are poorly understood. We here review the existing carbon-isotope records and present new data on the carbon-isotope composition of organic carbon in selected sections of the western Tethys realm that record the entire Carnian Pluvial Episode. New ammonoid, conodont and sporomorph biostratigraphic data were collected and coupled to an extensive review of the existing biostratigraphy to constrain the age of the sampled sections. The results provide biostratigraphically constrained composite organic carbon-isotope curves for the Carnian, which sheds light on the temporal and causal links between the main carbon-isotope perturbations, and the distinct environmental and biotic changes that mark the Carnian Pluvial Episode. The carbon-isotope records suggest that a series of carbon-cycle perturbations, possibly recording multiple phases of volcanic activity during the emplacement of the Wrangellia Large Igneous Province, disrupted Carnian environments and ecosystems repeatedly over a remarkably long time interval of about 1 million years.
Access RoutesGreen hybrid 93 citations 93 popularity Top 1% influence Top 10% impulse Top 1% Powered by BIP!add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.<script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.earscirev.2018.07.004&type=result"></script>'); --> </script>For further information contact us at helpdesk@openaire.eu - Dal Corso J.[1; 2; 3; 4]; +17 Authors
Dal Corso J.[1
Harvested from ORCID Public Data FileDal Corso J.[1 in OpenAIRE Dal Corso J.[1; 2; 3; 4];Dal Corso J.[1
Harvested from ORCID Public Data FileDal Corso J.[1 in OpenAIRE Gianolla P. [2]; Gianolla P. [2]
Harvested from ORCID Public Data FileGianolla P. [2] in OpenAIRE Rigo M.[3; 5]; Franceschi M.[3]; Franceschi M.[3]
Harvested from ORCID Public Data FileFranceschi M.[3] in OpenAIRE Roghi G.[5]; Mietto P.[3]; Manfrin S.[3];Roghi G.[5]
Harvested from ORCID Public Data FileRoghi G.[5] in OpenAIRE Raucsik B.[6]; Budai T.[7];Raucsik B.[6]
Harvested from ORCID Public Data FileRaucsik B.[6] in OpenAIRE Jenkyns H.[8]; Jenkyns H.[8]
Derived by OpenAIRE algorithms or harvested from 3rd party repositoriesJenkyns H.[8] in OpenAIRE Reymond C.[4]; Reymond C.[4]
Harvested from ORCID Public Data FileReymond C.[4] in OpenAIRE Caggiati M.[2]; Gattolin G.[9];Caggiati M.[2]
Harvested from ORCID Public Data FileCaggiati M.[2] in OpenAIRE Breda A.[3]; Breda A.[3]
Harvested from ORCID Public Data FileBreda A.[3] in OpenAIRE Merico A.[4; 10];Merico A.[4
Harvested from ORCID Public Data FileMerico A.[4 in OpenAIRE Preto N. [3]; Preto N. [3]
Derived by OpenAIRE algorithms or harvested from 3rd party repositoriesPreto N. [3] in OpenAIREThe Carnian Pluvial Episode was a phase of global climatic change and biotic turnover that occurred during the early Late Triassic. In marine sedimentary basins, the arrival of huge amounts of siliciclastic sediments, the establishment of anoxic conditions, and a sudden change of the carbonate factory on platforms marked the Carnian Pluvial Episode. The sedimentary changes are closely associated with abrupt biological turnover among marine and terrestrial groups as, for example, an extinction among ammonoids and conodonts in the ocean, and a turnover of the vertebrate fauna and the flora on land. Multiple negative carbon-isotope excursions were recorded during the Carnian Pluvial Episode in both organic matter and marine carbonates, suggesting repeated injection of 13C-depleted CO2 into the ocean-atmosphere system, but their temporal and causal links with the sedimentological and palaeontological changes are poorly understood. We here review the existing carbon-isotope records and present new data on the carbon-isotope composition of organic carbon in selected sections of the western Tethys realm that record the entire Carnian Pluvial Episode. New ammonoid, conodont and sporomorph biostratigraphic data were collected and coupled to an extensive review of the existing biostratigraphy to constrain the age of the sampled sections. The results provide biostratigraphically constrained composite organic carbon-isotope curves for the Carnian, which sheds light on the temporal and causal links between the main carbon-isotope perturbations, and the distinct environmental and biotic changes that mark the Carnian Pluvial Episode. The carbon-isotope records suggest that a series of carbon-cycle perturbations, possibly recording multiple phases of volcanic activity during the emplacement of the Wrangellia Large Igneous Province, disrupted Carnian environments and ecosystems repeatedly over a remarkably long time interval of about 1 million years.
Access RoutesGreen hybrid 93 citations 93 popularity Top 1% influence Top 10% impulse Top 1% Powered by BIP!add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.<script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1016/j.earscirev.2018.07.004&type=result"></script>'); --> </script>For further information contact us at helpdesk@openaire.eu - DFG Bahlburg, Dominik;
Bahlburg, Dominik
Harvested from ORCID Public Data FileBahlburg, Dominik in OpenAIRE Thorpe, Sally E.; Meyer, Bettina;Thorpe, Sally E.
Derived by OpenAIRE algorithms or harvested from 3rd party repositoriesThorpe, Sally E. in OpenAIRE Berger, Uta; +1 AuthorsBerger, Uta
Harvested from ORCID Public Data FileBerger, Uta in OpenAIRE Bahlburg, Dominik; Bahlburg, Dominik
Harvested from ORCID Public Data FileBahlburg, Dominik in OpenAIRE Thorpe, Sally E.; Meyer, Bettina;Thorpe, Sally E.
Derived by OpenAIRE algorithms or harvested from 3rd party repositoriesThorpe, Sally E. in OpenAIRE Berger, Uta; Berger, Uta
Harvested from ORCID Public Data FileBerger, Uta in OpenAIRE Murphy, Eugene J.; Murphy, Eugene J.
Derived by OpenAIRE algorithms or harvested from 3rd party repositoriesMurphy, Eugene J. in OpenAIREAntarctic krill (Euphausia superba) is a key species of the Southern Ocean, impacted by climate change and human exploitation. Understanding how these changes affect the distribution and abundance of krill is crucial for generating projections of change for Southern Ocean ecosystems. Krill growth is an important indicator of habitat suitability and a series of models have been developed and used to examine krill growth potential at different spatial and temporal scales. The available models have been developed using a range of empirical and mechanistic approaches, providing alternative perspectives and comparative analyses of the key processes influencing krill growth. Here we undertake an intercomparison of a suite of the available models to understand their sensitivities to major driving variables. This illustrates that the results are strongly determined by the model structure and technical characteristics, and the data on which they were developed and validated. Our results emphasize the importance of assessing the constraints and requirements of individual krill growth models to ensure their appropriate application. The study also demonstrates the value of the development of alternative modelling approaches to identify key processes affecting the dynamics of krill. Of critical importance for modelling the growth of krill is appropriately assessing and accounting for differences in estimates of food availability resulting from alternative methods of observation. We suggest that an intercomparison approach is particularly valuable in the development and application of models for the assessment of krill growth potential at circumpolar scales and for future projections. As another result of the intercomparison, the implementations of the models used in this study are now publicly available for future use and analyses.
Access RoutesGreen gold 10 citations 10 popularity Top 10% influence Average impulse Top 10% Powered by BIP!add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.<script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1371/journal.pone.0286036&type=result"></script>'); --> </script>For further information contact us at helpdesk@openaire.eu - DFG Bahlburg, Dominik;
Bahlburg, Dominik
Harvested from ORCID Public Data FileBahlburg, Dominik in OpenAIRE Thorpe, Sally E.; Meyer, Bettina;Thorpe, Sally E.
Derived by OpenAIRE algorithms or harvested from 3rd party repositoriesThorpe, Sally E. in OpenAIRE Berger, Uta; +1 AuthorsBerger, Uta
Harvested from ORCID Public Data FileBerger, Uta in OpenAIRE Bahlburg, Dominik; Bahlburg, Dominik
Harvested from ORCID Public Data FileBahlburg, Dominik in OpenAIRE Thorpe, Sally E.; Meyer, Bettina;Thorpe, Sally E.
Derived by OpenAIRE algorithms or harvested from 3rd party repositoriesThorpe, Sally E. in OpenAIRE Berger, Uta; Berger, Uta
Harvested from ORCID Public Data FileBerger, Uta in OpenAIRE Murphy, Eugene J.; Murphy, Eugene J.
Derived by OpenAIRE algorithms or harvested from 3rd party repositoriesMurphy, Eugene J. in OpenAIREAntarctic krill (Euphausia superba) is a key species of the Southern Ocean, impacted by climate change and human exploitation. Understanding how these changes affect the distribution and abundance of krill is crucial for generating projections of change for Southern Ocean ecosystems. Krill growth is an important indicator of habitat suitability and a series of models have been developed and used to examine krill growth potential at different spatial and temporal scales. The available models have been developed using a range of empirical and mechanistic approaches, providing alternative perspectives and comparative analyses of the key processes influencing krill growth. Here we undertake an intercomparison of a suite of the available models to understand their sensitivities to major driving variables. This illustrates that the results are strongly determined by the model structure and technical characteristics, and the data on which they were developed and validated. Our results emphasize the importance of assessing the constraints and requirements of individual krill growth models to ensure their appropriate application. The study also demonstrates the value of the development of alternative modelling approaches to identify key processes affecting the dynamics of krill. Of critical importance for modelling the growth of krill is appropriately assessing and accounting for differences in estimates of food availability resulting from alternative methods of observation. We suggest that an intercomparison approach is particularly valuable in the development and application of models for the assessment of krill growth potential at circumpolar scales and for future projections. As another result of the intercomparison, the implementations of the models used in this study are now publicly available for future use and analyses.
Access RoutesGreen gold 10 citations 10 popularity Top 10% influence Average impulse Top 10% Powered by BIP!add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.<script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.1371/journal.pone.0286036&type=result"></script>'); --> </script>For further information contact us at helpdesk@openaire.eu - Hatje, Vanessa; Sarin, Manmohan; Sander, Sylvia G;
Sander, Sylvia G
Harvested from ORCID Public Data FileSander, Sylvia G in OpenAIRE Omanović, Dario; +4 AuthorsOmanović, Dario
Harvested from ORCID Public Data FileOmanović, Dario in OpenAIREHatje, Vanessa; Sarin, Manmohan; Sander, Sylvia G; Sander, Sylvia G
Harvested from ORCID Public Data FileSander, Sylvia G in OpenAIRE Omanović, Dario; Ramachandran, Purvaja; Völker, Christoph; Barra, Ricardo O; Tagliabue, Alessandro;Omanović, Dario
Harvested from ORCID Public Data FileOmanović, Dario in OpenAIREThe effects of climate change (CC) on contaminants and their potential consequences to marine ecosystem services and human wellbeing are of paramount importance, as they pose overlapping risks. Here, we discuss how the interaction between CC and contaminants leads to poorly constrained impacts that affects the sensitivity of organisms to contamination leading to impaired ecosystem function, services and risk assessment evaluations. Climate drivers, such as ocean warming, ocean deoxygenation, changes in circulation, ocean acidification, and extreme events interact with trace metals, organic pollutants, excess nutrients, and radionuclides in a complex manner. Overall, the holistic consideration of the pollutants-climate change nexus has significant knowledge gaps, but will be important in understanding the fate, transport, speciation, bioavailability, toxicity, and inventories of contaminants. Greater focus on these uncertainties would facilitate improved predictions of future changes in the global biogeochemical cycling of contaminants and both human health and marine ecosystems.
Access RoutesGreen gold 18 citations 18 popularity Top 10% influence Average impulse Top 10% Powered by BIP!add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.<script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.3389/fmars.2022.936109&type=result"></script>'); --> </script>For further information contact us at helpdesk@openaire.eu - Hatje, Vanessa; Sarin, Manmohan; Sander, Sylvia G;
Sander, Sylvia G
Harvested from ORCID Public Data FileSander, Sylvia G in OpenAIRE Omanović, Dario; +4 AuthorsOmanović, Dario
Harvested from ORCID Public Data FileOmanović, Dario in OpenAIREHatje, Vanessa; Sarin, Manmohan; Sander, Sylvia G; Sander, Sylvia G
Harvested from ORCID Public Data FileSander, Sylvia G in OpenAIRE Omanović, Dario; Ramachandran, Purvaja; Völker, Christoph; Barra, Ricardo O; Tagliabue, Alessandro;Omanović, Dario
Harvested from ORCID Public Data FileOmanović, Dario in OpenAIREThe effects of climate change (CC) on contaminants and their potential consequences to marine ecosystem services and human wellbeing are of paramount importance, as they pose overlapping risks. Here, we discuss how the interaction between CC and contaminants leads to poorly constrained impacts that affects the sensitivity of organisms to contamination leading to impaired ecosystem function, services and risk assessment evaluations. Climate drivers, such as ocean warming, ocean deoxygenation, changes in circulation, ocean acidification, and extreme events interact with trace metals, organic pollutants, excess nutrients, and radionuclides in a complex manner. Overall, the holistic consideration of the pollutants-climate change nexus has significant knowledge gaps, but will be important in understanding the fate, transport, speciation, bioavailability, toxicity, and inventories of contaminants. Greater focus on these uncertainties would facilitate improved predictions of future changes in the global biogeochemical cycling of contaminants and both human health and marine ecosystems.
Access RoutesGreen gold 18 citations 18 popularity Top 10% influence Average impulse Top 10% Powered by BIP!add ClaimPlease grant OpenAIRE to access and update your ORCID works.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.This Research product is the result of merged Research products in OpenAIRE.
You have already added works in your ORCID record related to the merged Research product.<script type="text/javascript"> <!-- document.write('<div id="oa_widget"></div>'); document.write('<script type="text/javascript" src="https://beta.openaire.eu/index.php?option=com_openaire&view=widget&format=raw&projectId=10.3389/fmars.2022.936109&type=result"></script>'); --> </script>For further information contact us at helpdesk@openaire.eu
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