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77 results for “deposition analysis”
Long term response of arctic tussock tundra to thermal erosion features: A modeling analysis. Tussock tundra regrowth after a thermal erosion event: Simulation F - increased N deposition
The Multiple Element Limitation (MEL) model is used to simulate the recovery of Alaskan arctic tussock tundra to thermal erosion features (TEFs) caused by permafrost thaw and mass wasting. TEFs could be significant to regional carbon (C) and nutrient budgets because permafrost soils contain large stocks of soil organic matter (SOM) and TEFs are expected to become more frequent as climate warms. These simulations deal only with recovery following TEF stabilization and do not address initial losses of C and nutrients during TEF formation. To capture the variability among and within TEFs, we simulate a range of post-stabilization conditions by varying the initial size of SOM pools and nutrient supply rates. This file contains the results for 100 years of tussock tundra recovery after a thermal erosion event. This simulation is of TEF recovery with increased N deposition compared to the base simulation. Data is presented for day 250 of each year.
Long term response of arctic tussock tundra to thermal erosion features: A modeling analysis. Tussock tundra regrowth after a thermal erosion event: Simulation H - increased N and P deposition
The Multiple Element Limitation (MEL) model is used to simulate the recovery of Alaskan arctic tussock tundra to thermal erosion features (TEFs) caused by permafrost thaw and mass wasting. TEFs could be significant to regional carbon (C) and nutrient budgets because permafrost soils contain large stocks of soil organic matter (SOM) and TEFs are expected to become more frequent as climate warms. These simulations deal only with recovery following TEF stabilization and do not address initial losses of C and nutrients during TEF formation. To capture the variability among and within TEFs, we simulate a range of post-stabilization conditions by varying the initial size of SOM pools and nutrient supply rates. This file contains the results for 100 years of tussock tundra recovery after a thermal erosion event. This simulation is of TEF recovery with increased N and P deposition compared to the base simulation. Data is presented for day 250 of each year.
Long term response of arctic tussock tundra to thermal erosion features: A modeling analysis. Tussock tundra regrowth after a thermal erosion event: Simulation G - increased P deposition
The Multiple Element Limitation (MEL) model is used to simulate the recovery of Alaskan arctic tussock tundra to thermal erosion features (TEFs) caused by permafrost thaw and mass wasting. TEFs could be significant to regional carbon (C) and nutrient budgets because permafrost soils contain large stocks of soil organic matter (SOM) and TEFs are expected to become more frequent as climate warms. These simulations deal only with recovery following TEF stabilization and do not address initial losses of C and nutrients during TEF formation. To capture the variability among and within TEFs, we simulate a range of post-stabilization conditions by varying the initial size of SOM pools and nutrient supply rates. This file contains the results for 100 years of tussock tundra recovery after a thermal erosion event. This simulation is of TEF recovery with increased P deposition compared to the base simulation. Data is presented for day 250 of each year.
Don't put all your eggs in one leaf-roll: a network analysis of candy-striped spider leaf preferences for egg deposition
<p>"Enoplognatha leaf choice.R" - R script for all analyses and figures for the manuscript.</p> <p>"Enop_LeafENNR_EnopChoice.csv" - Interaction matrix showing the leaves selected by each individual candy-striped spider.</p> <p>"Enop_LeafENNR_PlantComm.csv" - Proportional plant community composition in each quadrat within which candy-striped spiders were found.</p> <p>"Enop_LeafTSENNR_EnopChoice.csv" - Interaction matrix showing the tropho-species selected by each individual candy-striped spider.</p> <p>"Enop_LeafENNR_PlantComm.csv" - Proportional plant tropho-species community composition in each quadrat within which candy-striped spiders were found.</p> <p>"Enop_SNRENNR_EnopChoice.csv" - Interaction matrix showing the semi-natural habitats selected by each individual candy-striped spider.</p> <p>"Enop_SNRENNR_SNRs.csv" - Matrix equally representing the semi-natural habitats as the number of quadrats surveyed in each.</p> <p>"Leaf traits.csv" - The leaf trait data used to cluster leaves into tropho-species.</p> <p>"leaf.incidence.csv" - The number of candy-striped spiders that interacted with each plant species for assessment of interaction diversity and completeness.</p> <p>"Site Map.csv" - Latitude and longitude of the ten sampling sites used in this study.</p> <p>"TS plotting order.csv" - A file used to set the plotting order of tropho-species in a bipartite plot.</p>
QENS spectra of myoglobin in solution to be used with the analysis codes deposited under 10.5281/zenodo.7058345
<p>Quasielastic Neutron Scattering spectra of myoglobin in solution recorded on the IN5 spectrometer at the Institut Laue-Langevin in Grenoble, France. The data sets are to be used with the analysis codes deposited under DOI:10.5281/zenodo.7058345, which are in turn related to the publication A. Hassani, A. M. Stadler, and G.R. Kneller, Quasi-analytical resolution-correction of elastic neutron scattering from proteins, to appear in the Journal of Chemical Physics (DOI:10.1063/5.0103960). </p> <p>The data can be freely used, citing properly the reference concerning the original data, A. M. Stadler, F. Demmel, J. Ollivier, and T. Seydel, Picosecond to Nanosecond Dynamics Provide a Source of Conformational Entropy for Protein Folding. Phys. Chem. Chem. Phys., 18(31):21527–21538, 2016 (DOI: 10.1039/c6cp04146a).</p> <p> </p>
Fig. 12 Supratidal limestones. a in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania
Fig. 12 Supratidal limestones. a Algal-microbial mats; they contain alternations of calcified cyanobacteria and very fine micritic lamine. b Detail from the image a; the cyanobacteria laminae with agglutinated fine peloids and ostracods (indicated by arrows). c, d Fenestral algal/cyanobacterial bindstone; micro-lamination is formed by calcified cyanobacteria filaments; the lower part is composed of rivulariacean-type cyanobacteria; detail at left;
Fig. 5 Pedogenetically altered granular limestones. a, b in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania
Fig. 5 Pedogenetically altered granular limestones. a, b Peloidal-bioclastic grainstone bearing vadoids and black pebbles, micritised intraclasts and meniscus cements. c-d Dissolution features associated with microstalactitic and equigranular cements which are developed arround cavities and grains; cavities are filled with vadose silt in association with large crystals of equigranular calcite.
Fig. 8 a-d in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania
Fig. 8 a-d Normal marine subtidal limestones. Bioturbated bioclastic packstone with dasycladalean algae [Selliporella neocomiensis (Radoičić), Terquemella sp.]; miliolids, ostracods and bivalve fragments.
Fig. 3 in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania
Fig. 3 Intraclastic/bioclastic-dominated shoals. a-f Coarse intraclastic-bioclastic grainstone and rudstone containing intraclasts, oncoids, peloids, normal and incipient ooids. g-h Intraclastic-bioclastic grainstone and rudstone with vadoids. Bioclasts are represented by large benthic foraminifera (a, c-d), coral fragments (b, d-e), rivulariacean-type cyanobacteria (e.g. Diversocalis sp.) (c), bivlave fragments, echinoderm fragments, dasycladalean algae [Clypeina sulcata (Alth)] (a) and gastropods (f); intraclasts and blackened bioclasts (black pebbles) (a, c, d, f, h).
Fig. 15 in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania
Fig. 15 Limestones from the Padina Brașoavei outcrop (Urdărița horst). The arrows indicate the discontinuity surface.
Fig. 4 in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania
Fig. 4 Contact between the intraclastic/bioclastic-dominated shoals (A) and peritidal limestones (B) in the Dâmbovicioara Gorges.
Fig. 11 a in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania
Fig. 11 a Intertidal carbonates (micro-cycles delimitated by firmground type surfaces) (thin section in panorama). Fenestral peloidal-oncoidic grainstone; Millimeter-scale firmgrounds are composed of micritic laminae (arrowed).
Fig. 7 a, b in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania
Fig. 7 a, b Well bedded, decimetre- to meter-thick limestones from the peritidal succession of the Cheile Dâmbovicioarei; c fenestral structures and millimeter to centimeter-thick sets of laminae are present.
Fig. 9 Restricted marine subtidal limestones. a-d in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania
Fig. 9 Restricted marine subtidal limestones. a-d Oncoidal-bioclastic packstone with cyanobacteria nodules.
Fig. 17 Carbonate facies from the breccia levels. a-d in Microfacies Analysis And Depositional Environments Of The Tithonian-Valanginian Limestones From Dâmbovicioara Gorges (Cheile Dâmbovicioarei), Getic Carbonate Platform, Romania
Fig. 17 Carbonate facies from the breccia levels. a-d Peloidal-bioclastic packstone with cyanobacteria, ostracods and foraminifera (d); cavities are filled with vadose silt and gravitational terrigenous material. e-f Breccia with horizontal (e), circumgranular and vertical (f) cracks. Scale-bar = 1 mm.
Text-fig. 2. Taphonomic and pathological phenomena of bear bones from Middle Pleistocene deposits from Vykopaná chodba in Za Hájovnou Cave (Moravia, the Czech Republic). a – fragment of left mandibula with pathological condylar process; b – thoracic vertebra with pathological rib facet; c – Mc III dext. with exostoses; d – fragment of juvenile right ulna with bite marks; e – gnawed right tibia with bite marks on proximal part; f – gnawed left calcaneus with bite marks. in Basic Population And Taphonomic Analysis Of Bear Assemblages From Za Hájovnou Cave (Moravia, The Czech Republic): A Fossil Record From 1987-2007
Text-fig. 2. Taphonomic and pathological phenomena of bear bones from Middle Pleistocene deposits from Vykopaná chodba in Za Hájovnou Cave (Moravia, the Czech Republic). a – fragment of left mandibula with pathological condylar process; b – thoracic vertebra with pathological rib facet; c – Mc III dext. with exostoses; d – fragment of juvenile right ulna with bite marks; e – gnawed right tibia with bite marks on proximal part; f – gnawed left calcaneus with bite marks.
Text-fig. 5. Distribution of age classes of deningeri bears from Middle Pleistocene deposits from Za Hájovnou Cave (Moravia, the Czech Republic) based on wear stage of M2 dext. and m2 dext. (I–III: juveniles, IV–VII: prime adults, VIII–IX: senile adults; according to Stiner 1998). Juveniles distinctly outnumber adults. in Basic Population And Taphonomic Analysis Of Bear Assemblages From Za Hájovnou Cave (Moravia, The Czech Republic): A Fossil Record From 1987-2007
Text-fig. 5. Distribution of age classes of deningeri bears from Middle Pleistocene deposits from Za Hájovnou Cave (Moravia, the Czech Republic) based on wear stage of M2 dext. and m2 dext. (I–III: juveniles, IV–VII: prime adults, VIII–IX: senile adults; according to Stiner 1998). Juveniles distinctly outnumber adults.
Text-fig. 4. Taphonomic and pathological phenomena of bear bones from Middle Pleistocene deposits from Spojovací chodba – Narozeninová chodba in Za Hájovnou Cave (Moravia, the Czech Republic). a – Mc V sin. with a pathological phenomenon on the metapodial distal part (tuberosity/exostosis?); b – gnawed juvenile ulna; c – right tibia gnawed by a large rodent (porcupine?) with detail. in Basic Population And Taphonomic Analysis Of Bear Assemblages From Za Hájovnou Cave (Moravia, The Czech Republic): A Fossil Record From 1987-2007
Text-fig. 4. Taphonomic and pathological phenomena of bear bones from Middle Pleistocene deposits from Spojovací chodba – Narozeninová chodba in Za Hájovnou Cave (Moravia, the Czech Republic). a – Mc V sin. with a pathological phenomenon on the metapodial distal part (tuberosity/exostosis?); b – gnawed juvenile ulna; c – right tibia gnawed by a large rodent (porcupine?) with detail.
Text-fig. 3. Taphonomic and pathological phenomena of bear bones from Middle Pleistocene deposits from Chodba naděje in Za Hájovnou Cave (Moravia, the Czech Republic). a – gnawed lumbar vertebra with a bite mark on the body head; b – fragment of pelvis with a bite mark; c – femur head with a bite mark; d – Mc II dext. with a pathological phenomenon on the metapodial proximal part (tuberosity/exostosis?). in Basic Population And Taphonomic Analysis Of Bear Assemblages From Za Hájovnou Cave (Moravia, The Czech Republic): A Fossil Record From 1987-2007
Text-fig. 3. Taphonomic and pathological phenomena of bear bones from Middle Pleistocene deposits from Chodba naděje in Za Hájovnou Cave (Moravia, the Czech Republic). a – gnawed lumbar vertebra with a bite mark on the body head; b – fragment of pelvis with a bite mark; c – femur head with a bite mark; d – Mc II dext. with a pathological phenomenon on the metapodial proximal part (tuberosity/exostosis?).
FIGURE 7. 1, Strict consensus tree for parsimony analysis including Marada arcanum. 2 in New genus of primitive wombat (Vombatidae, Marsupialia) from Miocene deposits in the Riversleigh World Heritage Area (Queensland, Australia)
FIGURE 7. 1, Strict consensus tree for parsimony analysis including Marada arcanum. 2, Bootstrap support for single most parsimonious tree from analysis excluding Marada arcanum (see text for details). Vombatidae indicated in purple.
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Allen Brain Atlas
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Annotated Behaviour and Observability Dataset (ABODe)
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DANDI Archive for NWB datasets
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The International Brain Laboratory public data releases expose standardized mouse decision-making experiments, including Neuropixels recordings, widefield calcium imaging, behavior, and session metadata accessed through the ONE API.
OpenNeuro
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