Search results for "Glacial period"

showing 6 items of 196 documents

Ice age at the Middle–Late Jurassic transition?

2003

A detailed record of sea surface temperatures in the Northern Hemisphere based on migration of marine invertebrate fauna (ammonites) and isotopic thermometry (δ18O values of shark tooth enamel) indicates a severe cooling at the Middle–Late Jurassic transition (MLJT), about 160 Ma ago. The magnitude of refrigeration (1–3°C for lower middle latitudes) and its coincidence in time with an abrupt global-scale fall of sea level documented through sequence stratigraphy are both suggestive of continental ice formation at this time. Ice sheets may have developed over the high-latitude mountainous regions of Far-East Russia. The drastic cooling just post-dated the Middle–Late Callovian widespread dep…

geographygeography.geographical_feature_categoryδ18OPaleontologyGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyPaleoclimatologyEarth and Planetary Sciences (miscellaneous)Ice ageSequence stratigraphyMesozoicGlacial periodIce sheetGeologySea levelEarth and Planetary Science Letters
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Experimental deformation of deuterated ice in 3D and 2D: identification of grain-scale processes

2015

Major polar ice sheets and ice caps experience cycles of variable flow during different glacial periods and as a response to past warming. The rate and localisation of deformation inside an ice body controls the evolution of ice microstructure and crystallographic fabric. This is critical for interpreting proxy signals for climate change, with deformation overprinting and disrupting stratigraphy deep under ice caps due to the nature of the flow. The final crystallographic fabric in polar ice sheets provides a record of deformation history, which in turn controls the flow properties of ice during further deformation and affects geophysical sensing of ice sheets. For example, identification o…

geography.geographical_feature_categoryEcologyMeteorologyClimate changeGeologyGeophysicsGrain sizeProxy (climate)Physics::GeophysicsIce-sheet modelGeographyAstrophysics::Earth and Planetary AstrophysicsGlacial periodClimate stateLayeringIce sheetPhysics::Atmospheric and Oceanic PhysicsProceedings of the Royal Society of Victoria
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The reconstruction of easterly wind directions for the Eifel region (Central Europe) during the period 40.3–12.9 ka BP

2010

Abstract. A high resolution continuous reconstruction of last glacial wind directions is based on provenance analysis of eolian sediments in a sediment core from the Dehner dry Maar in the Eifel region (Germany). This Maar is suitable to archive easterly wind directions due to its location west of the Devonian carbonate basins of the Eifel-North-South-Zone. Thus, eolian sediments with high clastic carbonate content can be interpreted as an east wind signal. The detection of such east wind sediments is applied by a new module of the RADIUS grain size analyze technique. The investigated time period from 40.3–12.9 ka BP can be subclassified in three units: The first unit covers the periods of …

lcsh:GE1-350Global and Planetary ChangeProvenanceStratigraphylcsh:Environmental protectionPaleontologyStormWind directionDevonianMaarPaleontologylcsh:Environmental pollutionClastic rocklcsh:TD172-193.5lcsh:TD169-171.8StadialGlacial periodGeomorphologyGeologylcsh:Environmental sciencesClimate of the Past
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Bacterial Diversity in a Dynamic and Extreme Sub-Arctic Watercourse (Pasvik River, Norwegian Arctic)

2020

Microbial communities promptly respond to the environmental perturbations, especially in the Arctic and sub-Arctic systems that are highly impacted by climate change, and fluctuations in the diversity level of microbial assemblages could give insights on their expected response. 16S rRNA gene amplicon sequencing was applied to describe the bacterial community composition in water and sediment through the sub-Arctic Pasvik River. Our results showed that river water and sediment harbored distinct communities in terms of diversity and composition at genus level. The distribution of the bacterial communities was mainly affected by both salinity and temperature in sediment samples, and by oxygen…

lcsh:Hydraulic engineeringGeography Planning and DevelopmentClimate changesedimentitAquatic ScienceBiochemistryAlgal bloombakteerit03 medical and health scienceslcsh:Water supply for domestic and industrial purposeslcsh:TC1-978Glacial period030304 developmental biologyWater Science and TechnologyPhylotypearktinen aluelcsh:TD201-5000303 health sciences030306 microbiologyEcologyvesiekosysteemitbacterial diversityriver sediment and waterSedimentmikrobiekologiaSalinitymikrobistoTaxonvirtavedetNGSsub-Arctic systemEnvironmental scienceSurface runoffjoetWater
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STOP 12: Late-glacial and Holocene development of Lake Rāzna as recorded by biostratigraphy

2014

loss on ignitionGeographyKvartāra ģeoloģijapollen analyses:NATURAL SCIENCES::Earth sciences::Exogenous earth sciences::Sedimentology [Research Subject Categories]Glacial periodPhysical geographyBiostratigraphyLoss on ignition:NATURAL SCIENCES::Earth sciences::Exogenous earth sciences::Quaternary geology [Research Subject Categories]HoloceneLate Quaternary Terrestrial Processes, Sediments and History: From Glacial to Postglacial Environments
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Evolution of Seismicity During a Stalled Episode of Reawakening at Cayambe Volcano, Ecuador

2021

Cayambe Volcano is an ice-capped, 5,790 m high, andesitic-dacitic volcanic complex, located on the equator in the Eastern Cordillera of the Ecuadorian Andes. An eruption at Cayambe would pose considerable hazards to surrounding communities and a nationally significant agricultural industry. Although the only historically documented eruption was in 1785, it remains persistently restless and long-period (LP) seismicity has been consistently observed at the volcano for over 10 years. However, the sparse monitoring network, and complex interactions between the magmatic, hydrothermal, glacial, and tectonic systems, make unrest at Cayambe challenging to interpret. In June 2016 a seismic “crisis” …

volcano-tectonic interactionsgeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesScienceEquatorQvolcano-glacier interactionsInduced seismicityFault (geology)010502 geochemistry & geophysics01 natural sciencesTectonicsVolcanoMagmavolcano-seismic swarmsGeneral Earth and Planetary SciencesGlacial periodlong-period seismicityVolcanic coneGeologySeismology0105 earth and related environmental sciencesvolcanic monitoringFrontiers in Earth Science
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