Search results for "Palaeolimnology"

showing 6 items of 6 documents

Variability in δ13C values between individual Daphnia ephippia: Implications for palaeo-studies

2018

The stable carbon isotope ratio (δ13 C value) of Daphnia spp. resting egg shells (ephippia) provides information on past changes in Daphnia diet. Measurements are typically performed on samples of _20 ephippia, which obscures the range of values associated with individual ephippia. Using a recently developed laser ablation-based technique, we perform multiple δ13 C analyses on individual ephippia, which show a high degree of reproducibility (standard deviations 0.1e0.5‰). We further measured δ13 C values of 13 ephippia from surface sediments of three Swiss lakes. In the well-oxygenated lake with low methane concentrations, δ13 C values are close to values typical for algae (_31.4‰) and the …

0106 biological sciencesArcheology010504 meteorology & atmospheric sciencesEvolutionhiilita1171Daphnia [water flea]01 natural sciencesDaphniaCarbon cycleStable carbon isotopesAlgaeBehavior and SystematicsPalaeolimnologyTavernemedicineEphippiaEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesStable isotopesPresentisotoopitGlobal and Planetary Changebiologyδ13CEcologyStable isotope ratio010604 marine biology & hydrobiologykausivaihtelutGeologySeasonalitySeasonalitybiology.organism_classificationmedicine.diseasepaleolimnologiaLaser ablationEuropeLakesArchaeology13. Climate actionIsotopes of carbonvesikirputta1181Daphnia ephippiaPhysical geographyQuaternary Science Reviews
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A 2000-year record of lake ontogeny and climate variability from the north-eastern European Russian Arctic

2016

A lake sediment record from the north-eastern European Russian Arctic was examined using palaeolimnological methods, including subfossil chironomid and diatom analysis. The objective of this study is to disentangle environmental history of the lake and climate variability during the past 2000 years. The sediment profile was divided into two main sections following changes in the lithology, separating the limno-telmatic phase between ~2000 and 1200 cal. yr BP and the lacustrine phase between ~1200 cal. yr BP and the present. Owing to the large proportion of semi-terrestrial chironomids and poor modern analogues, a reliable chironomid-based temperature reconstruction for the limno-telmatic p…

010506 paleontologyArcheology010504 meteorology & atmospheric sciencesta1171chironomidsClimate change01 natural sciencesdiatomsPrecipitation0105 earth and related environmental sciencesEarth-Surface ProcessesGlobal and Planetary ChangeSubfossilEcologybiologyPaleontologySedimentpalaeolimnologybiology.organism_classificationArctic RussiaEastern europeanclimate changequantitative reconstructionDiatomArctic13. Climate actionClimatologyPeriod (geology)ta1181Physical geographyGeologyThe Holocene
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Climate change and human impact in central Spain during Roman times: High-resolution multi-proxy analysis of a tufa lake record (Somolinos, 1280m asl)

2012

The Roman Period is considered a crucial phase in the evolution of Holocene landscapes, due to the coincidence of major climatic, environmental, economic and cultural changes. However, there is still debate as to the regional expression of these changes, and to the mechanisms involved, particularly in the topographically and climatically complex region of the Mediterranean. In order to improve our understanding of the synergies between societal and environmental change during this period in central Spain, we present a comprehensive case study based on the integration of multi-proxy palaeoenvironmental, archaeological and historical data. High-resolution, interdisciplinary research has been …

Mediterranean climateEnvironmental changeLand-use changePalaeoenvironmentClimate changeCentral SpainAridGeographyRoman Warm PeriodPalaeolimnologyAridificationLand use land-use change and forestryMarl lakePhysical geographyRoman Warm PeriodGeomorphologyHoloceneEarth-Surface ProcessesCATENA
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Variability in δ13C values between individual Daphnia ephippia: Implications for palaeo-studies

2018

The stable carbon isotope ratio (δ13C value) of Daphnia spp. resting egg shells (ephippia) provides information on past changes in Daphnia diet. Measurements are typically performed on samples of ≥20 ephippia, which obscures the range of values associated with individual ephippia. Using a recently developed laser ablation-based technique, we perform multiple δ13C analyses on individual ephippia, which show a high degree of reproducibility (standard deviations 0.1–0.5‰). We further measured δ13C values of 13 ephippia from surface sediments of three Swiss lakes. In the well-oxygenated lake with low methane concentrations, δ13C values are close to values typical for algae (−31.4‰) and the rang…

PresentisotoopitGlobal and Planetary ChangehiilikausivaihtelutGeologySeasonalityjärvetpaleolimnologiaLaser ablationEuropeLakesStable carbon isotopesArchaeologyPalaeolimnologyTavernevesikirputDaphnia ephippiaEcology Evolution Behavior and SystematicsStable isotopes
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Lacustrine sedimentation in the diapir-controlled Miocene Bicorb Basin, Eastern Spain

1998

The Miocene Bicorb Basin is a small elongated basin developed by normal faulting of a thick Jurassic–Cretaceous carbonate succession and subsequent diapirism of Upper Triassic mudstones and evaporites. The basin fill comprises a sequence over 650 m thick formed by two units. The lower, alluvial unit consists of a complex alternation of conglomerates, sandstones, mudstones, and minor lacustrine limestones. The upper unit comprises marginal alluvial and lacustrine deposits in which seven lacustrine facies associations have been distinguished. The inner lacustrine deposits comprise mudstones and carbonates with minor evaporitic deposits. At the northeast and southwest basin edges, alluvial inp…

EvaporiteRhythmitelacustrine depositsPaleontologyMioceneStructural basinDiapirpalaeolimnologyOceanographyConglomeratePaleontologyBrecciaFaciesdiapirCyclical sequencesAlluviumEcology Evolution Behavior and SystematicsGeologyEarth-Surface Processesrhythmites
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Role of terrestrial carbon in aquatic UV exposure and photoprotective pigmentation of meiofauna in subarctic lakes

2015

Summary Aquatic organisms are adversely influenced by ultraviolet radiation (UV) and utilise photoprotective strategies, including pigmentation. We examined UV-protective melanin pigmentation of aquatic meiofauna (Cladocera) in relation to the UV exposure across 25 tree line lakes in Finland to address the potential effects of increased UV and altered input of UV-screening terrestrial dissolved organic carbon (DOC) on aquatic organisms. Bio-optical parameters, including concentration of DOC, the coloured dissolved organic matter (CDOM) fraction, a suite of carbon quality indices and chlorophyll a, were analysed from lake water, and their role in controlling underwater UV environment (measur…

Total organic carbonChlorophyll abiologyChemistryEcologyMeiobenthosLimnologyta117115. Life on landAquatic Sciencebiology.organism_classificationCladoceraUV radiationAbsorbanceColored dissolved organic matterchemistry.chemical_compoundCladocera13. Climate actionPalaeolimnologyDissolved organic carbonMelaninta118114. Life underwaterDissolved organic carbonFreshwater Biology
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