Search results for "Environmental Protection"

showing 10 items of 289 documents

Black shale deposition during Toarcian super-greenhouse driven by sea level

2013

Abstract. One of the most elusive aspects of the Toarcian oceanic anoxic event (T-OAE) is the paradox between carbon isotopes that indicate intense global primary productivity and organic carbon burial at a global scale, and the delayed expression of anoxia in Europe. During the earliest Toarcian, no black shales were deposited in the European epicontinental seaways, and most organic carbon enrichment of the sediments postdated the end of the overarching positive trend in the carbon isotopes that characterises the T-OAE. In the present study, we have attempted to establish a sequence stratigraphic framework for Early Toarcian deposits recovered from a core drilled in the Paris Basin using a…

010504 meteorology & atmospheric sciencesStratigraphylcsh:Environmental protection[SDE.MCG]Environmental Sciences/Global ChangesGeochemistry010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesPaleontologyWater columnlcsh:Environmental pollution[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistrySequence stratigraphylcsh:TD169-171.8Earth ScienceSea levellcsh:Environmental sciences0105 earth and related environmental sciencesTotal organic carbonlcsh:GE1-350Global and Planetary ChangePaleontology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryAnoxic waters[ SDE.MCG ] Environmental Sciences/Global ChangesIsotopes of carbon13. Climate action[SDU]Sciences of the Universe [physics][SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphylcsh:TD172-193.5Enhanced weatheringOil shaleGeology
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Effect of the Ordovician paleogeography on the (in)stability of the climate.

2014

The Ordovician Period (485–443 Ma) is characterized by abundant evidence for continental-sized ice sheets. Modeling studies published so far require a sharp CO2 drawdown to initiate this glaciation. They mostly used non-dynamic slab mixed-layer ocean models. Here, we use a general circulation model with coupled components for ocean, atmosphere, and sea ice to examine the response of Ordovician climate to changes in CO2 and paleogeography. We conduct experiments for a wide range of CO2 (from 16 to 2 times the preindustrial atmospheric CO2 level (PAL)) and for two continental configurations (at 470 and at 450 Ma) mimicking the Middle and the Late Ordovician conditions. We find that the temper…

010504 meteorology & atmospheric scienceslcsh:Environmental protectionStratigraphy010502 geochemistry & geophysics01 natural scienceslcsh:Environmental pollutionSea icelcsh:TD169-171.8Glacial periodlcsh:Environmental sciences0105 earth and related environmental scienceslcsh:GE1-350Global and Planetary Changegeographygeography.geographical_feature_categoryNorthern HemispherePaleontologyRadiative forcingOcean dynamics13. Climate action[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology[SDU]Sciences of the Universe [physics]Climatologylcsh:TD172-193.5OrdovicianIce sheet[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/ClimatologyGlobal coolingGeology[ SDU ] Sciences of the Universe [physics]
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Holocene climate variability in north-eastern Italy: potential influence of the NAO and solar activity recorded by speleothem data

2012

Abstract. Here we present high-resolution stable isotope and lamina thickness profiles as well as radiocarbon data for the Holocene stalagmite ER 76 from Grotta di Ernesto (north-eastern Italy), which was dated by combined U-series dating and lamina counting. ER 76 grew between 8 ka (thousands of years before 2000 AD) and today, with a hiatus from 2.6 to 0.4 ka. Data from nine meteorological stations in Trentino show a significant influence of the North Atlantic Oscillation (NAO) on winter temperature and precipitation in the cave region. Spectral analysis of the stable isotope signals of ER 76 reveals significant peaks at periods of 110, 60–70, 40–50, 32–37 and around 25 a. Except for the …

010504 meteorology & atmospheric scienceslcsh:Environmental protectionStratigraphySpeleothemStalagmite010502 geochemistry & geophysics01 natural scienceslaw.inventionMediterranean sealcsh:Environmental pollutionCavelawlcsh:TD169-171.814. Life underwaterRadiocarbon datinglcsh:Environmental sciencesHolocene0105 earth and related environmental scienceslcsh:GE1-350Global and Planetary Changegeographygeography.geographical_feature_categoryPaleontology13. Climate actionPluvialNorth Atlantic oscillationClimatologylcsh:TD172-193.5GeologyClimate of the Past
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From USSR to EU: 20 years of rural landscape changes in Vidzeme, Latvia

2012

Landscape changes have been observed throughout rural Europe over the past decades in relation to intensifying agriculture and land marginalisation. This is particularly true for Central and Eastern Europe as drastic political and socio-economic changes have taken place over the past century, as is the case for Latvia. Using a detailed time series of high-resolution remotely sensed images spanning from 1988 to 2007, the landscape structure (composition and configuration) in Vidzeme, central Latvia, is examined and compared between periods. Major recent events for the country, such as independence and entry into the European Union are covered. The effect on landscape structure of various soc…

010504 meteorology & atmospheric sciencesmedia_common.quotation_subjectForest management0211 other engineering and technologies02 engineering and technologyManagement Monitoring Policy and Law01 natural sciencesPoliticsEnvironmental protectionmedia_common.cataloged_instanceEuropean union0105 earth and related environmental sciencesNature and Landscape Conservationmedia_commonGovernmentEcologybusiness.industry021107 urban & regional planningSubsidy15. Life on landIndependenceUrban StudiesGeographyEconomyAgriculturePeriod (geology)businessLandscape and Urban Planning
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Climate indices in historical climate reconstructions: a global state of the art

2021

Narrative evidence contained within historical documents and inscriptions provides an important record of climate variability for periods prior to the onset of systematic meteorological data collection. A common approach used by historical climatologists to convert such qualitative information into continuous quantitative proxy data is through the generation of ordinal-scale climate indices. There is, however, considerable variability in the types of phenomena reconstructed using an index approach and the practice of index development in different parts of the world. This review, written by members of the PAGES (Past Global Changes) CRIAS working group – a collective of climate historians a…

010506 paleontologyGlobal and Planetary ChangeIndex (economics)Data collection010504 meteorology & atmospheric sciencesStratigraphymedia_common.quotation_subjectPaleontology01 natural sciencesEnvironmental protectionEnvironmental pollutionEnvironmental sciencesDocumentary evidenceState (polity)TD172-193.5Multidisciplinary approachTD169-171.8GE1-350Physical geography0105 earth and related environmental sciencesmedia_commonClimate of the Past
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Coarsely crystalline cryogenic cave carbonate – a new archive to estimate the Last Glacial minimum permafrost depth in Central Europe

2012

Abstract. Cryogenic cave carbonate (CCC) represents a specific type of speleothem whose precipitation is triggered by freezing of mineralized karst water. Coarsely crystalline CCC, which formed during slow freezing of water in cave pools, has been reported from 20 Central European caves located in Germany, the Czech Republic, Slovakia and Poland. All these caves are situated in an area which was glacier-free during the Weichselian. Whereas the formation of usual types of speleothems in caves of this region usually ceased during the glacials, coarsely crystalline CCC precipitation was restricted to glacial periods. Since this carbonate type represents a novel, useful paleoclimate proxy, data…

010506 paleontologyGroundwater flowStratigraphylcsh:Environmental protectionGeochemistryAquifer010502 geochemistry & geophysicsPermafrost01 natural scienceslcsh:Environmental pollutionLatent heatlcsh:TD169-171.8Glacial periodGeomorphologylcsh:Environmental sciences0105 earth and related environmental scienceslcsh:GE1-350Global and Planetary ChangegeographyHydrogeologygeography.geographical_feature_categoryPaleontology13. Climate actionlcsh:TD172-193.5QuaternaryGroundwaterGeologyClimate of the Past
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Reevaluating the Role of Organic Matter Sources for Coastal Eutrophication, Oligotrophication, and Ecosystem Health

2019

Organic matter (OM) in aquatic systems is either produced internally (autochthonous OM) or delivered from the terrestrial environment (ter-OM). For eutrophication (or the reverse – oligotrophication), the amount of autochthonous OM plays a key role for coastal ecosystem health. However, the influence of ter-OM on eutrophication or oligotrophication processes of coastal ecosystems is largely unclear. Therefore, ter-OM, or ter-OM proxies are currently not included in most policies or monitoring programs on eutrophication. Nevertheless, ter-OM is increasingly recognized as a strong driver of aquatic productivity: By influencing underwater light conditions and nutrient- and carbon availability,…

0106 biological sciences010504 meteorology & atmospheric scienceslcsh:QH1-199.5Ocean EngineeringVDP::Landbruks- og Fiskerifag: 900::Fiskerifag: 920::Akvakultur: 922Aquatic Sciencelcsh:General. Including nature conservation geographical distributionOceanography01 natural sciencesEnvironmental protectionnutrientsEcosystemlcsh:Science0105 earth and related environmental sciencesWater Science and TechnologybrowningGlobal and Planetary ChangeEcosystem health010604 marine biology & hydrobiologyAquatic ecosystemorganic carbondissolved organic carbonCoastal erosioncoastal darkeningeutrophicationProductivity (ecology)Benthic zoneEnvironmental scienceTerrestrial ecosystemlcsh:QEutrophicationFrontiers in Marine Science
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Coping with Difficult Weather and Snow Conditions : Reindeer herders’ views on climate change impacts and coping strategies

2016

Winter is a critical season for reindeer herding, with the amount and quality of snow being among the most important factors determining the condition of reindeer and the annual success of the livelihood. Our first aim was to model the future (2035–2064) snow conditions in northern Finland, especially the quantities related to ground ice and/or ice layers within the snow pack, exceptionally deep snow and late snow melt. Secondly, we studied the strategies by which herders cope with the impacts of difficult weather and snow conditions on herding by interviewing 21 herders. SNOWPACK simulations indicate that snow cover formation will be delayed by an average of 19 days and snow will melt 16 d…

0106 biological sciencesAtmospheric Science010504 meteorology & atmospheric sciencesta1172educationGeography Planning and Developmentta1171Climate changeSnow modelinglcsh:QC851-999Management Monitoring Policy and Law114 Physical sciences010603 evolutionary biology01 natural sciencesReindeer herdingEnvironmental protectiontalviClimate changeHerding1172 Environmental sciences0105 earth and related environmental sciencesTraditional knowledge (TK)2. Zero hungerGlobal and Planetary ChangeLand useEcologyselviytyminenWinter15. Life on landSnowpackLivelihoodSnowreindeer herdingclimate change13. Climate actionSnowmeltSustainabilityEnvironmental sciencelcsh:Meteorology. Climatologytraditional knowledgeCopingsnow modelling
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Biotope Determinants of EPT Assamblages Structure – Târnava Watershed (Transylvania, Romania) Case Study

2015

Abstract This study aims to analyze the biotopic factors affecting the EPT assemblage diversity in the rivers of the Târnava Watershed. Our research revealed that the high diversity of the Plecoptera communities is associated with river reaches with boulder and cobble lithological substrate, accentuated slope and natural bank dynamics, and also it is directly correlated with dissolved oxygen and inversely correlated with chemical and biochemical oxygen demand, total hardness, nitrates and total nitrogen in the water. The high diversity of the Trichoptera communities is associated with water which presents moderate quantities of nutrients (total phosphorus, phosphates) and with river reaches…

0106 biological sciencesBiotopemayfly communitiesWatershedEcologytârnava mare rivertârnava mică river010501 environmental sciences01 natural sciences010602 entomologyGeographyEnvironmental protectionstonefly communitiestârnava riverWater resource managementcaddisfly communitieshuman activitiesQH540-549.50105 earth and related environmental sciencesTransylvanian Review of Systematical and Ecological Research
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Challenges of ecological restoration: Lessons from forests in northern Europe

2013

The alarming rate of ecosystem degradation has raised the need for ecological restoration throughout different biomes and continents. North European forests may appear as one of the least vulnerable ecosystems from a global perspective, since forest cover is not rapidly decreasing and many ecosystem services remain at high level. However, extensive areas of northern forests are heavily exploited and have lost a major part of their biodiversity value. There is a strong requirement to restore these areas towards a more natural condition in order to meet the targets of the Convention on Biological Diversity. Several northern countries are now taking up this challenge by restoring forest biodiv…

0106 biological sciencesConvention on Biological Diversity010504 meteorology & atmospheric sciencesbusiness.industryEnvironmental resource managementBiodiversityEnvironmental restoration15. Life on land010603 evolutionary biology01 natural sciencesForest restorationEcosystem servicesGeography13. Climate actionEnvironmental protectionForest ecologyta1181Ecosystem diversitybusinessRestoration ecologyEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesNature and Landscape ConservationBiological Conservation
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