Search results for "Geochemistry"

showing 10 items of 2967 documents

Wood as a structural element in the houses of Akrotiri on Thera, Greece. The anthracological evidence

2021

Abstract The highly destructive eruption of the volcano of Santorini during the Late Cycladic I period as a fortunate consequence caused the buildings of the archaeological site of Akrotiri on Thera (Greece) to be remarkably well preserved. The present study deals with wood charcoal macroremains from the construction timbers of two buildings from this site, namely Xeste 3, a semi-public building and the House of the Ladies, a private building. The data suggest the extensive use of Olea europaea for the construction of the wooden floors of the upper storeys, the doors and the infrastructure of the walls. Other taxa systematically used for the beams of the floors of the upper storeys were Pin…

010506 paleontologybiologyTamarixEvergreen010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesArchaeologyPoor qualityPinus <genus>GeographyDeciduousvisual_artvisual_art.visual_art_mediumPeriod (geology)Charcoal0105 earth and related environmental sciencesEarth-Surface ProcessesQuaternary International
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Upper Ovetian trilobites from Spain and their implications for the palaeobiogeography and correlation of the Cambrian Stage 3 in Gondwana

2016

Abstract The upper part of the La Herreria Formation in Los Barrios de Luna (Leon Province, N Spain) has been revised from a palaeontological and biostratigraphical point of view. Two stratigraphic sections have been studied including their trilobite and ichnofossils contents. The ichnofossil assemblages have a high diversity of species characterising the Cruziana ichnofacies, suggesting a shallow sublittoral environment for the upper part of the La Herreria Formation. The trilobites species recognised are Lunagraulos antiquus , Dolerolenus formosus , Dolerolenus longioculatus , Lunolenus lunae , Metadoxides richterorum , Metadoxides armatus and Sardaspis ? sp. from the upper Ovetian (lower…

010506 paleontologybiologyTrace fossilBiostratigraphy010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesCambrian Stage 3TrilobiteGondwanaPaleontologyGeophysicsIchnofaciesCambrian Series 2CruzianaGeology0105 earth and related environmental sciencesEarth-Surface ProcessesTectonophysics
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Turonian marine amniotes from the Opole area in southwest Poland

2018

A few isolated plesiosaurian and mosasauroid squamate teeth were collected from the Opole area in southwest Poland during the late nineteenth century. Calcareous nannofossil analysis of their associated rock matrix indicates an early Turonian age (nannofossil zone UC7; Mytiloides ex gr. labiatus and Inoceramus apicalis inoceramid zones), which is significant because this constitutes a globally enigmatic interval of marine amniote evolution. The Opole plesiosaurian teeth are attributable to polycotylids, but an indeterminate mesopodial was also recovered. They are similar to specimens from the Cenomanian-Turonian in the Saxonian Cretaceous Basin of Germany and the Chalk succession of England…

010506 paleontologybiologyplesiosauriaCentral EuropePaleontologycomparisonsLate Mesozoic010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesCretaceousMosasauroideaPlesiosauriaPaleontologyGeographyComparisonsTaxonomy (biology)CalcareousPlesiosauriaMosasauroideaTaxonomy0105 earth and related environmental sciencesCretaceous Research
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Calcareous nannofossil response to Late Cretaceous climate change in the eastern Tethys (Zagros Basin, Iran)

2020

Abstract Coniacian to Maastrichtian changes in calcareous nannofossil assemblages have been investigated in the eastern Tethyan Shahneshin section (central Zagros Basin, Iran). The nannofossil assemblages are mainly composed of Watznaueria spp. (avg. 54%), Retecapsa spp (avg. 7.9%), Cribrosphaerella ehrenbergii (avg. 7.7%) and Micula spp. (avg. 5.7%). Throughout the late Campanian, there is a trend to lower abundances in Watznaueria spp. together with increasing abundances of C. ehrenbergii and Arkhangelskiella cymbiformis, which are considered in this basin as the main cool-water taxa. Our results reveal that, despite a diagenetic impact on calcareous nannoflora, a number of primary paleoe…

010506 paleontologybiologyδ13CPaleontologyStructural basin010502 geochemistry & geophysicsOceanographybiology.organism_classification01 natural sciencesCretaceousDiagenesisForaminiferaPaleontologyBorealBenthic zoneCalcareousEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Planktonic foraminifera biozones and isotope stratigraphy of the Cenomanian-Turonian boundary in the western part of the Kopet-Dagh Basin, NE Iran

2018

Abstract A biostratigraphic study based on the planktonic foraminifera and isotope stratigraphy of the Cenomanian-Turonian interval has been undertaken in the western part of the Kopet-Dagh Basin (NE Iran). In this research, two stratigraphic sections including: Maraveh Tappeh and Qareh Galdy have been sampled and studied. Based on planktonic foraminifera, three biozones were assigned to this interval. These are the Rotalipora cushmani Zone, Whiteinella archaeocretacea Zone and Helvetoglobotruncana helvetica Zone, These biostratigraphic data confirm a gradual faunal turnover of planktonic foraminifera, at the Cenomanian-Turonian boundary in Whiteinella archaeocretacea Zone characterized by:…

010506 paleontologybiologyδ18OGeologyBiozoneBiostratigraphyStructural basin010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesForaminiferaPaleontologyStratigraphyBiostratigraphy Light isotopes Cenomanian-Turonian boundary Kopet-Dagh basin NE IranCenomanianSiltstoneGeology0105 earth and related environmental sciencesEarth-Surface ProcessesJournal of African Earth Sciences
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Growth-increment characteristics and isotopic (delta O-18) temperature record of sub- thermocline Aequipecten opercularis (Mollusca: Bivalvia): evide…

2021

Abstract The shell δ18O of young modern Aequipecten opercularis from the southern North Sea provides an essentially faithful record of seasonal variation in seafloor temperature. In this well-mixed setting, A. opercularis shell δ18O also serves as a proxy for seasonal variation in surface temperature. Individuals from less agitated (e.g. deeper) settings in a warm climate would not be expected to record the full seasonal range in surface temperature because of thermal stratification in summer. Such circumstances have been invoked to explain cool isotopic summer temperatures from early Pliocene A. opercularis of eastern England. Support for a sub-thermocline setting derives from high-amplitu…

010506 paleontologybiologyδ18OPaleontologyOceanic climateSeasonality010502 geochemistry & geophysicsOceanographybiology.organism_classificationmedicine.disease01 natural sciencesAequipectenOceanographyMediterranean seaBivalve ; Hydrography ; Marine climate ; Pliocene ; SclerochronologySclerochronologymedicineThermoclineEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesTemperature record
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Biostratigraphy, Chronostratigraphy and Paleonvironmental Reconstruction of the Palermo Historical Centre Quaternary succession

2016

Marine deposits from the Palermo Plain were historically relevant for the Quaternary Period definition. Here we show lithostratigraphic, biostratigraphic and chronostratigraphic data collected on three boreholes in the Palermo historical centre that recovered 36.8, 42.0 and 52.0 metres of sediments overlaying the Numidian Flysch. Marine sedimentary sequences span from the Calabrian Stage (calcareous nannofossil Zone MNN 19d) to the Middle Pleistocene (dominance of medium-sized gephyrocapsids within the MNN 19f Zone) and also include a short Holocene depositional event. Calcareous nannofossil, benthic and planktonic foraminifera assemblages point to a shallow coastal environment, possibly < …

010506 paleontologycalcareous nannofossilsFlyschPleistocenebiologyGeologyBiostratigraphy010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesForaminiferaSedimentary depositional environmentPaleontologyStage (stratigraphy)Quaternary.General Earth and Planetary SciencesbiostratigraphyChronostratigraphyQuaternaryPalermo historical centre calcareous nannofossils biostratigraphy Quaternary.Palermo historical centreGeology0105 earth and related environmental sciences
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Advances of sclerochronology research in the last decade

2021

Over the past decade, sclerochronological research has continued to develop rapidly and is diversifying with respect to methods, taxa, geographic coverage as well as temporal depth. Chonologically aligned environmental records from bivalves, gastropods, coralline algae, corals, and many other periodically formed biogenic hard parts are integrated to build networks across broad spatial domains and trophic levels. Replication and exact dating ensure that environmental signals are fully preserved and facilitate the integration among chronologies as well as observational records of climatic and biological phenomena. The proliferation of chronologies promises to usher in a new era of synthesis t…

010506 paleontologyeducation.field_of_studyEarth scienceEcology (disciplines)PopulationPaleontologyClimate change010502 geochemistry & geophysicsOceanography01 natural sciencesField (geography)Natural (archaeology)SclerochronologyPaleoclimatologygrowth pattern ; increment ; shell geochemistry ; environmental proxyeducationEcology Evolution Behavior and SystematicsGeologyDeep time0105 earth and related environmental sciencesEarth-Surface Processes
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Fire–vegetation relationships during the last glacial cycle in a low mountain range (Eifel, Germany)

2021

Abstract Lake sediments can provide useful archives to reconstruct past vegetation changes or fire history. To comprehend how vegetation and fire history have correlated during the last 130,000 years, we used two lake sediment records with known patterns of pollen and botanical macro remains and supplemented this data by analyses of lignin-derived phenols as markers for local vegetation inputs and by benzene polycarboxylic acids (BPCAs) as markers for total fire residue inputs (black carbon, BC). The two sediment archives originated from two maar lakes in the Eifel, which is part of the low mountain ranges in central Germany. A lignin-derived phenol index showed woody angiosperms and gymnos…

010506 paleontologygeographyEemiangeography.geographical_feature_categoryPaleontologySedimentVegetation010502 geochemistry & geophysicsOceanographymedicine.disease_cause01 natural sciencesMaarPollenInterglacialmedicineGlacial periodPhysical geographyEcology Evolution Behavior and SystematicsMountain rangeGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Carbonate slope re‐sedimentation in a tectonically‐active setting (Western Sicily Cretaceous Escarpment, Italy)

2020

Tectonic processes are widely considered as a mechanism causing carbonate platform margin instabilities leading to the emplacement of mass transport deposits and calciturbidites. However, only few examples establishing a clear link between tectonics and re-sedimentation processes are known from the lit- erature. The two-dimensional and three-dimensional wire-cut walls of hun- dreds of quarries extracting ornamental limestones (for example, Perlato di Sicilia) from the Western Sicily Cretaceous Escarpment in Italy expose a series of mass transport deposits. The depositional architecture, spatial facies distri- bution and sedimentary features of these deposits were studied in detail. Thin sec…

010506 paleontologygeographyPillow lavageography.geographical_feature_categoryCarbonate platformStratigraphyGeochemistryGeologyEscarpment010502 geochemistry & geophysics01 natural sciencesCretaceousSedimentary depositional environmentTectonicsFaciesGeneral Earth and Planetary SciencesSedimentary rockGeologyCarbonate slope Cretaceous mass transport deposits re-deposited facies tectonics0105 earth and related environmental sciencesGeneral Environmental ScienceSedimentology
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