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462 results for “Castle”
Pelagic, epilimnetic production estimates in Sparkling, Trout (Wisconsin), Acton (Ohio), and Castle (California) Lakes (USA) calculated using 14C and free-water O2 metabolism methods, 2007 - 2017
Concurrent daily estimates of pelagic, eplilimnetic production (mmol C m3 d) generated from 14C incubations and diel changes in high frequency dissolved oxygen data (free-water). Original data derived from the North Temperate Lakes Long Term Ecological Research program (Sparkling [2007-2013], Trout [2007-2012] Lakes), Castle Lake Research Station (Castle Lake [2014-2017]), and Center for Aquatic and Watershed Sciences (Acton Lake [2010-2014]). 14C production estimates were generated as part of each research programs core data collection. Free-water production estimates generated using high frequency sensor data provided by research programs and Phillips (2020) time-varying, Bayesian metabolism model.
Mountain Lake Chemistry and Physics Profile Data since 2015 at Castle Lake
This data set contains long-term limnology data from Castle Lake (located 5440 ft above sea level in Northern California). The data contained can be broadly grouped into two different types: chemical and physical data. This data set contains dissolved oxygen saturation, dissolved oxygen concentration, chlorophyll-a concentration, CDOM, phycocyanin concentration, conductivity, specific conductivity, pH, salinity, water temperature, pressure, turbidity, sea pressure, density anomaly, and speed of sound at various depths. Sampling Frequency: Continuous measurements were made and recorded down to milliseconds. Sampling dates vary from year to year, starting as early as February and as late as November. This data collection is part of an ongoing project funded by the US National Science Foundation, private donors, US AID, and the University of Nevada's Global Water Center. This package was updated in February 2023 with data from 2021 and 2022. Dissolved O2 concentration data in the 2020 data file was updated to values in units of mg/L instead of umol/L and specific conductivity units in all files was revised to be in microSiemens per centimeter and not milliSiemens per centimeter.
Mountain Lake Biology, Chemistry, Physics, and Climate Data since 1959 at Castle Lake
This data set contains long-term limnology data from Castle Lake (located 5440 ft above sea level in Northern California) on primary productivity, zooplankton and phytoplankton measurements, dissolved oxygen, nutrient chemistry, lake morphology, and fish measurements. Short-term research projects on benthic invertebrates composition and a bathymetric map can also be found within the data package. Ecological, watershed and climatological measurements taken characterize the limnology of Castle Lake, a pristine glacial cirque that is the largest (by volume) of the 25 alpine and sub-alpine lake within the larger Upper Sacramento River Watershed. Sampling Frequency: Varies depending on survey conducted. During summer months- multiple times during each month. Less frequent during winter months. This data collection part of an ongoing project funded by the US National Science Foundation, private donors, US AID, and the University of Nevada's Global Water Center.
РИС. 1. Раковины ювенильных крымских клауЗиллид (A–C). A. Mentissa gracilicosta, г. КоШка, СимеиЗ, coll. В. Н. Попов, det. С. В. Леонов. B. Mentissa canalifera, окрестности с. Краснолесье, 23.08.2002, сoll.&det. С. В. Леонов. C. Cochlodina laminata, Артек «Дубрава», 27.05.1999, coll.?, det. С.В. Леонов. Раковины половоЗрелых Balea perversa (D–G). D. Между Виклебю и Ресмо, остров Эланд, ШвециЯ, 07.1958 (фото F. Welter-Shultes). Е. Девичий Замок, Палава, ЮжнаЯ МоравиЯ, ЧехиЯ, 26.09.1998 (фото M. Horsák). F. РаЗвалины Замка РейнграфенШтайн блиЗ Бад-Мюнстер-ам-Штайн, Рейнланд-Пфальц, ГерманиЯ (фото А. В. Сысоев). G. Яйла Южной Демерджи, АлуШта, Республика Крым, РоссиЯ, 14.11.2002, сoll. Н. М. Ковблюк, det. С. В. Леонов. Все иЗображениЯ в одном масШтабе. FIG. 1. Shells of juvenile Crimean clausillids (A–C). A. Mentissa gracilicosta, Koshka mountain, Simeiz, coll. V. N. Popov, det. S. V. Leonov. B. Mentissa canalifera, near Krasnolesye village, 23.08.2002, coll.&det. S. V. Leonov. C. Cochlodina laminata, Artek "Dubrava", 27.05.1999, coll.?, det. S.V. Leonov. Adult Balea perversa shells (D–G). D. Sweden, Öland, between Vickleby and Resmo, 07.1958 (photo F. Welter-Shultes). E. Dívčí hrad, South Moravia, Czech Republic, 26.09.1998 (photo by M. Horsák). F. Ruins of the Rheingrafenstein Castle near Bad Munster am Stein, Rheineland-Pfalz, Germany (photo by A.V. Sysoev). G. Yayla Yuzhnaya Demerdzhi, Alushta, Republic of Crimea, Russia, 14.11.2002, coll. N. M. Kovblyuk, det. S. V. Leonov. All images are at the same scale. in О достоверности находок Balea perversa (Gastropoda: Pulmonata: Clausiliidae) в Крыму
РИС. 1. Раковины ювенильных крымских клауЗиллид (A–C). A. Mentissa gracilicosta, г. КоШка, СимеиЗ, coll. В. Н. Попов, det. С. В. Леонов. B. Mentissa canalifera, окрестности с. Краснолесье, 23.08.2002, сoll.&det. С. В. Леонов. C. Cochlodina laminata, Артек «Дубрава», 27.05.1999, coll.?, det. С.В. Леонов. Раковины половоЗрелых Balea perversa (D–G). D. Между Виклебю и Ресмо, остров Эланд, ШвециЯ, 07.1958 (фото F. Welter-Shultes). Е. Девичий Замок, Палава, ЮжнаЯ МоравиЯ, ЧехиЯ, 26.09.1998 (фото M. Horsák). F. РаЗвалины Замка РейнграфенШтайн блиЗ Бад-Мюнстер-ам-Штайн, Рейнланд-Пфальц, ГерманиЯ (фото А. В. Сысоев). G. Яйла Южной Демерджи, АлуШта, Республика Крым, РоссиЯ, 14.11.2002, сoll. Н. М. Ковблюк, det. С. В. Леонов. Все иЗображениЯ в одном масШтабе. FIG. 1. Shells of juvenile Crimean clausillids (A–C). A. Mentissa gracilicosta, Koshka mountain, Simeiz, coll. V. N. Popov, det. S. V. Leonov. B. Mentissa canalifera, near Krasnolesye village, 23.08.2002, coll.&det. S. V. Leonov. C. Cochlodina laminata, Artek "Dubrava", 27.05.1999, coll.?, det. S.V. Leonov. Adult Balea perversa shells (D–G). D. Sweden, Öland, between Vickleby and Resmo, 07.1958 (photo F. Welter-Shultes). E. Dívčí hrad, South Moravia, Czech Republic, 26.09.1998 (photo by M. Horsák). F. Ruins of the Rheingrafenstein Castle near Bad Munster am Stein, Rheineland-Pfalz, Germany (photo by A.V. Sysoev). G. Yayla Yuzhnaya Demerdzhi, Alushta, Republic of Crimea, Russia, 14.11.2002, coll. N. M. Kovblyuk, det. S. V. Leonov. All images are at the same scale.
Fig. 6 in A new thalassematid echiuran worm from the Middle Ordovician Castle Bank Biota of Wales, UK
Fig. 6. Echiura gen. et sp. indet. from the Darriwilian (Middle Ordovician) of Castle Bank, Wales, UK, NMW.2021.3G.102. A1, overall view; A2, proboscis; A3, caudal region; A4, close up showing projections from anal region. A1 in plane-polarised light, A2–A4 in cross-polarised light.
Fig. 5 in A new thalassematid echiuran worm from the Middle Ordovician Castle Bank Biota of Wales, UK
Fig. 5. Reconstruction of Llwygarua suzannae gen. et sp. nov.; observed size range: 5.5 to 7 mm long.
Fig. 1. A in A new thalassematid echiuran worm from the Middle Ordovician Castle Bank Biota of Wales, UK
Fig. 1. A. Location of Castle Bank within Wales (highlighted within UK, inset). B. Stratigraphic position within the sequence of the Builth-Llandrindod Inlier. Asterisk indicates Castle Bank locality.
Fig. 3 in A new thalassematid echiuran worm from the Middle Ordovician Castle Bank Biota of Wales, UK
Fig. 3. Thalassematid echiuran Llwygarua suzannae gen. et sp. nov., from the Darriwilian (Middle Ordovician) of Castle Bank, Wales, UK, paratype NMW.2021.3G.100. A1, overall view; A2, close up showing detail of central region of trunk, with muscle arrangement of longitudinal and oblique muscle bundles (arrowed); A3, proboscis with anterior projections arrowed, A5, close up showing reticulate structure; A4, caudal region with irregular structures possibly resulting from damage.
Fig. 4 in A new thalassematid echiuran worm from the Middle Ordovician Castle Bank Biota of Wales, UK
Fig. 4. Thalassematid echiuran Llwygarua suzannae gen. et sp. nov., from the Darriwilian (Middle Ordovician) of Castle Bank, Wales, UK, NMW.2021.3G.101. A1, overall view of worm in probably dorsal view; A2, proboscis and midline structures; A3, detail of apex of proboscis, the anterior projections faintly visible (arrowed); A4, counterpart of A1; A5, close up of A4 showing caudal region.
Fig. 2 in A new thalassematid echiuran worm from the Middle Ordovician Castle Bank Biota of Wales, UK
Fig. 2. Recent thalassematid echiuran (A) and a fossil equivalent (B). A.?Ochetostoma sp., highlighting significant features for comparison with the fossils (photograph courtesy of Arthur Anker), typical length 10–20 cm. B. Holotype of Llwygarua suzannae gen. et sp. nov., from the Darriwilian (Middle Ordovician) of Castle Bank, Wales, UK, NMW.2021.3G.99 showing overall specimen in slightly oblique lateral view (B1); enlargement with anterior ventral part of trunk (B4), showing one anterior seta (white arrow) and probably second seta (black arrow); detail of proboscis in cross-polarised light (B5), showing reticulate structure and anterior projections adjacent to midline; central region of trunk with distinctive wrinkling of cuticle in response to compression (B2), and proboscis in plane-polarised light (B3), with anterior projections arrowed.
Dataset: Castle Biosciences, Inc. (CSTL) Stock Performance
This dataset provides historical stock market performance data for specific companies. It enables users to analyze and understand the past trends and fluctuations in stock prices over time. This information can be utilized for various purposes such as investment analysis, financial research, and market trend forecasting.
Located Earthquakes Loki's Castle 2019-2020 Deployment
<div>The dataset includes information about the 6977 located events from the 2019-2020 Loki ocean bottom seismometer deplyoment (network code: 8M). The events cover the deplyoment period of 11 months and were recorded by 8 ocean bottom seismometers west of Loki's Castle hydrothermal vent field with a station spacing of 5-6 km. Earthquakes were detected using Lassie, automatically picked using PhaseNet, and partially manually re-picked. Events for location were chosen to have at least 7 P phase picks and were located using NonLinLoc with the EDT_OT inversion scheme. Amplitudes were automatically picked with SEISANs automag function. Local magnitudes were calculated using the hypocentral distance. </div>
FIGURE 7 in Teganium (Porifera, Hexactinellida) from the Middle Ordovician Castle Bank fauna of Avalonia (Wales, UK)
FIGURE 7. Palaeogeographic distributions of species of Teganium (all species in B originally assigned to Teganiella). A, Ordovician (Sandbian, 458 Ma). B, Carboniferous (Visean, 340 Ma). Map constructed using GPlates (Müller et al. 2018) using data from Torsvik & Cocks (2016). Does not include unconfirmed taxa listed by Ruedemann (1925b, 1934, 1942).
FIGURE 6 in Teganium (Porifera, Hexactinellida) from the Middle Ordovician Castle Bank fauna of Avalonia (Wales, UK)
FIGURE 6. Teganium sp., from the Middle Ordovician Castle Bank Biota, Wales. A, NMW.2021.3G.76i and ii, overall view, with positions of detail images indicated by boxes (all rotated). B, apex of NMW.2021.3G.76i, apex of sponge showing extensive marginalia; C, detail of body wall showing characteristic texture (boxed area enlarged inset); D, apex of NMW.2021.3G.76ii, with oscular margin and trace of marginalia. Scale bars: A equals 10 mm; B–D equal 1 mm.
FIGURE 5 in Teganium (Porifera, Hexactinellida) from the Middle Ordovician Castle Bank fauna of Avalonia (Wales, UK)
FIGURE 5. Cut-away reconstruction of Teganium avalonensis sp. nov., with detail of wall structure on the right; dermal/hypodermal skeleton in lower part, and choanosomal layer with exhalent canals in upper part.
FIGURE 3 in Teganium (Porifera, Hexactinellida) from the Middle Ordovician Castle Bank fauna of Avalonia (Wales, UK)
FIGURE 3. Teganium avalonensis sp. nov. A, paratype NMW.2021.3G.74; apical part with marginalia, imaged with directed light (from right) to highlight texture of body wall; B, paratype NMW.2021.3G.98, with low-angle light to highlight diagnostic texture of body wall (boxed area enlarged inset); C–F, paratype NMW.2021.3G.82, partial specimen with the boxes in C indicating positions of D, E and F; D, lateral detail to show reticulate skeletal grid (plane-polarised light); E, detail showing scale of minute triaxon spicules within the same area; centres of several spicules arrowed; F, detail of central part of specimen in cross-polarised light (contrast enhanced) to highlight the small circular cavities within choanosomal (internal) layer of body wall. Scale bars: A, B, D, F equal 1 mm; C equals 5 mm; E equals 0.1 mm.
FIGURE 2 in Teganium (Porifera, Hexactinellida) from the Middle Ordovician Castle Bank fauna of Avalonia (Wales, UK)
FIGURE 2. Teganium avalonensis sp. nov., from the Middle Ordovician Castle Bank Biota, Wales. A–B: paratype slab NMW.2021.3G.72, with pair of sponges in A, plane-polarised light, and B, cross-polarised; C, E, holotype NMW.2021.3G.71: C, overall view, with box indicating area enlarged in E; E, detail of basal region showing projecting basalia; D, paratype NMW.2021.3G.73, overall view. Scale bars: A–D equal 5 mm; E equals 1 mm.
FIGURE 4 in Teganium (Porifera, Hexactinellida) from the Middle Ordovician Castle Bank fauna of Avalonia (Wales, UK)
FIGURE 4. Paratypes of Teganium avalonensis sp. nov. A, NMW.2021.3G.77; B, NMW.2021.3G.98 in cross-polarised light (boxed area enlarged in Figure 3B); C, NMW.2021.3G.78 with pair of specimens, the right-hand one with marginalia; D, NMW.2021.3G.79; E, NMW.2021.3G.81 with multiple specimens, in cross-polarised light; F, NMW.2021.3G.80. Scale bars equal 1 mm.
FIGURE 1 in Teganium (Porifera, Hexactinellida) from the Middle Ordovician Castle Bank fauna of Avalonia (Wales, UK)
FIGURE 1. Locality map (left) and local stratigraphy of the Castle Bank locality, showing occurrence of Teganium avalonensis sp. nov. within the Castle Bank sequence (mainly siltstone, with shading representing colour of sediment; v: volcanic ash layers). Exact locality information is deposited with the specimens.
Fig.1.Domal bryozoans from the Castle Hayne Formation. A–D in Palaeoecology of free-lying domal bryozoan colonies from the Upper Eocene of southeastern USA
Fig.1.Domal bryozoans from the Castle Hayne Formation. A–D. Parasmittina collum (Canu and Bassler). A.Upper surface with multiple subcolonies vis − ible; NHM BZ4963. B.Undersurface of colony established on Chlamys; NHM BZ4964. C.NHM BZ4965.C 1.Lateral view.C 2.Undersurface, established on bivalve fragment. D.Lateral view of colony with renewed growth indicated by second lateral flange; NHM BZ4966. E, F. Osthimosia glomerata (Gabb and Horn). E.NHM BZ4967.E 1.Upper surface.E 2.Undersurface, established on Lunulites sp.E 3.Lateral view. F.Lateral view of colony with renewed growth indicated by broader flange developed above short basal portion with a curved surface consisting of frontal surfaces of zooids; NHM BZ4968. G. Multispecies dome; NHM BZ4969. G1. Upper surface. G2. Undersurface showing Chlamys substratum. G3. Lateral view. Scale bars 1 cm.
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