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37 results for “Central Sands”
Groundwater level data from 2013 to 2015 in Central Sands area, Wisconsin
38 groundwater wells' water level data in Central Sands area, Wisconsin. The Central Sands is an area of the state with a high density of high-capacity wells for irrigation. The Wisconsin Department of Natural Resources (WDNR), UW Extension, and the counties began monitoring shallow groundwater wells near lakes in 2013. The five counties include: Portage, Waupaca, Adams, Waushara, and Marquette. Volunteers were enlisted to monitor lake levels on 38 lakes in the region. Instead of using staff gauges, the team opted to install shallow groundwater wells near the lake shore. This eliminated the need to reinstall and survey staff gauges each season. It was assumed that shallow groundwater wells would be a good approximation of lake levels because the soils are made up of porous, sand material. On a subset of lakes, WDNR collected water level data from the shallow groundwater wells and from staff gauges at the same time. One season of monitoring showed that changes in water levels over time are similar, but the actual elevation of water in the well might be different than the surface of the lake. This data set can be downloaded from WDNR's SWIMS database: https://dnr.wi.gov/topic/surfacewater/swims/
Text-fig. 3. Geological map and schematic geological section of the discovery site of the Late Upper Palaeolithic skull from Moča (southern Slovakia). I. – Primary position (?), II. – The discovery site (secondary position), A – B – The schematic geological section of the discovery site 1. H – Fluvial clayey to sandy loams (subordinately humolites) – Holocene; secondary discovery site layer, 2. lm-pH – Loam – peat – Holocene, 3. e Wl – Eolian sands – Late Würm (Late glacial of Würm), 4. lm,sWl – Fluvial clayey (to humic) loams or fine sands – Late Würm (Late glas cial of Würm); original discovery site layer, now eroded, 4a. fe Wl – Fluvial – aeolian silty sands (calcareous) – Late Würm (Late glacial s-lm of Würm), 5. lmW3 – Fluvial loams, sandy loams – final Würm (W3), 5a. W3 – Fluvial sands – final (?) Würm (?W3), 6. gW2+3 – Fluvial gravs els, sandy gravels, sands with gravel – Pleniglacial of Würm (W2+3), 7. lW – Aeolian loess and loess loams – Würm (undivided) in A Late Upper Palaeolithic Skull From Moča (The Slovak Republic) In The Context Of Central Europe
Text-fig. 3. Geological map and schematic geological section of the discovery site of the Late Upper Palaeolithic skull from Moča (southern Slovakia). I. – Primary position (?), II. – The discovery site (secondary position), A – B – The schematic geological section of the discovery site 1. H – Fluvial clayey to sandy loams (subordinately humolites) – Holocene; secondary discovery site layer, 2. lm-pH – Loam – peat – Holocene, 3. e Wl – Eolian sands – Late Würm (Late glacial of Würm), 4. lm,sWl – Fluvial clayey (to humic) loams or fine sands – Late Würm (Late glas cial of Würm); original discovery site layer, now eroded, 4a. fe Wl – Fluvial – aeolian silty sands (calcareous) – Late Würm (Late glacial s-lm of Würm), 5. lmW3 – Fluvial loams, sandy loams – final Würm (W3), 5a. W3 – Fluvial sands – final (?) Würm (?W3), 6. gW2+3 – Fluvial gravs els, sandy gravels, sands with gravel – Pleniglacial of Würm (W2+3), 7. lW – Aeolian loess and loess loams – Würm (undivided)
Text-fig. 4. Stratigraphic correlation of the five major fossil-bearing localities in the Mikhailovka quarry near Zheleznogorsk. 1 – loesses and soils, 2 – unlaminated loams, 3 – laminated loams, 4 – clays, 5 – sands, 6 – gravels, 7 – carbonate concretions, 8 – mollusk shells, 9 – small mammal remains, 10 – insect remains, 11 – plant macroremains. in Late Pleistocene (Eemian) Mollusk And Small Mammal Fauna From Mikhailovka-5 (Kursk Oblast, Central Russia)
Text-fig. 4. Stratigraphic correlation of the five major fossil-bearing localities in the Mikhailovka quarry near Zheleznogorsk. 1 – loesses and soils, 2 – unlaminated loams, 3 – laminated loams, 4 – clays, 5 – sands, 6 – gravels, 7 – carbonate concretions, 8 – mollusk shells, 9 – small mammal remains, 10 – insect remains, 11 – plant macroremains.
Text-fig. 3. Correlation of geological sections with Pleistocene deposits of the Mikhailovka quarry near Zheleznogorsk. 1 – modern and fossil soils, 2 – loess-like loam, 3 – sandy clay, 4 – aleurites, 5 – horizontally laminated clays, 6 – brown loams, 7 – blue clays and loams, 8 – sands, 9 – gravels, 10 – mollusk shells, 11 – small mammal remains. in Late Pleistocene (Eemian) Mollusk And Small Mammal Fauna From Mikhailovka-5 (Kursk Oblast, Central Russia)
Text-fig. 3. Correlation of geological sections with Pleistocene deposits of the Mikhailovka quarry near Zheleznogorsk. 1 – modern and fossil soils, 2 – loess-like loam, 3 – sandy clay, 4 – aleurites, 5 – horizontally laminated clays, 6 – brown loams, 7 – blue clays and loams, 8 – sands, 9 – gravels, 10 – mollusk shells, 11 – small mammal remains.
Fig. 3 in A remarkable sand-dwelling fish assemblage from central Amazonia, with comments on the evolution of psammophily in South American freshwater fishes
Fig. 3. The sit-and-wait foraging posture of "Imparfinis" pristos in dorsal view. Note translucent body and commashaped pupil.
Fig. 2 in A remarkable sand-dwelling fish assemblage from central Amazonia, with comments on the evolution of psammophily in South American freshwater fishes
Fig. 2. The sit-and-wait foraging posture of Mastiglanis asopos in posterior view. Note very long barbels and filamentous rays of pectoral fins spread in a drift trap-like device, as well as the alignment of mentonian barbels and pectoral filaments.
Fig. 1 in A remarkable sand-dwelling fish assemblage from central Amazonia, with comments on the evolution of psammophily in South American freshwater fishes
Fig. 1. Two species indicative of the morphological and behavioural variation found among the sand-dwelling fish assemblage in an Amazonian streamlet: a, the diurnally active Characidium cf. pteroides in its characteristic sit-and-wait posture while foraging for bottom-dwelling prey; b, the nocturnally active Gymnorhamphichthys rondoni in its typical headdown posture while actively searching for interstitial prey.
SGS-LTER CO2 Elevation Study: Percent sand, silt & clay from each block and treatment of the Open Top Chambers on the Central Plains Experimental Range, Nunn, Colorado, USA 1997 - 2001
This data package was produced by researchers working on the Shortgrass Steppe Long Term Ecological Research (SGS-LTER) Project, administered at Colorado State University. Long-term datasets and background information (proposals, reports, photographs, etc.) on the SGS-LTER project are contained in a comprehensive project collection within the Digital Collections of Colorado (http://digitool.library.colostate.edu/R/?func=collections&collection_id=3429). The data table and associated metadata document, which is generated in Ecological Metadata Language, may be available through other repositories serving the ecological research community and represent components of the larger SGS-LTER project collection. Additional information and referenced materials can be found: http://hdl.handle.net/10217/82454. Soil cores, divided at 7 depths, from the shortgrass steppe Open Top Chamber experiment were analyzed for percent sand, silt and clay. It was found that soils were fairly consistent across treatments. This research was conducted at the Central Plains Experimental Range, near Nunn, CO; lat.40degrees 40 minutes N; long. 104 degrees 45 minutes W in the shortgrass steppe region of NE Colorado, USA and as a collaboration between SGS-LTER and USDA-ARS researchers.
On following pages: 347. Plains Mouse (Pseudomys australis); 348. Bolam''s Mouse (Pseudomys bolami); 349. Kakadu Pebble Mouse (Pseudomys calabyi); 350. Western Pebble Mouse (Pseudomys chapmani); 351. Desert Mouse (Pseudomys desertor); 352. Shark Bay Mouse (Pseudomys field); 353. Australian Smoky Mouse (Pseudomys fumeus); 354. Eastern Chestnut Mouse (Pseudomys gracilicaudatus); 355. Sandy Inland Mouse (Pseudomys hermannsburgensis); 356. Long-tailed Mouse (Pseudomys higginsi); 357. Central Pebble Mouse (Pseudomys johnson); 358. Western Chestnut Mouse (Pseudomys nanus); 359. New Holland Mouse (Pseudomys novaehollandiae); 360. Western Mouse (Pseudomys occidentalis); 361. Hastings River Mouse (Pseudomys oralis); 362. Eastern Pebble Mouse (Pseudomys patrius); 363. Heath Mouse (Pseudomys shortridgel); 364. Common Australian Rock Rat (Zyzomys argurus); 365. Arnhem Land Rock Rat (Zyzomys maini); 366. Carpentarian Rock Rat (Zyzomys palatalis); 367. Central Australian Rock Rat (Zyzomys pedunculatus); 368. Kimberley Rock Rat (Zyzomys woodward); 369. Malayan Tree Rat (Pithecheir parvus); 370. Red Tree Rat (Pithecheir melanurus); 371. Bornean Tree Rat (Pithecheirops otion); 372. Cutch Rat (Cremnomys cutchicus); 373. Elvira Rat (Cremnomys elvira); 374. Crump's Rat (Diomys crumpi); 375. White-tailed Wood Rat (Madromys blanfordi); 376. Sand-colored Soft-furred Rat (Millardia gleadowi); 377. Kondana Soft-furred Rat (Millardia kondana); 378. Common Soft-furred Rat (Millardia in Muridae
On following pages: 347. Plains Mouse (Pseudomys australis); 348. Bolam''s Mouse (Pseudomys bolami); 349. Kakadu Pebble Mouse (Pseudomys calabyi); 350. Western Pebble Mouse (Pseudomys chapmani); 351. Desert Mouse (Pseudomys desertor); 352. Shark Bay Mouse (Pseudomys field); 353. Australian Smoky Mouse (Pseudomys fumeus); 354. Eastern Chestnut Mouse (Pseudomys gracilicaudatus); 355. Sandy Inland Mouse (Pseudomys hermannsburgensis); 356. Long-tailed Mouse (Pseudomys higginsi); 357. Central Pebble Mouse (Pseudomys johnson); 358. Western Chestnut Mouse (Pseudomys nanus); 359. New Holland Mouse (Pseudomys novaehollandiae); 360. Western Mouse (Pseudomys occidentalis); 361. Hastings River Mouse (Pseudomys oralis); 362. Eastern Pebble Mouse (Pseudomys patrius); 363. Heath Mouse (Pseudomys shortridgel); 364. Common Australian Rock Rat (Zyzomys argurus); 365. Arnhem Land Rock Rat (Zyzomys maini); 366. Carpentarian Rock Rat (Zyzomys palatalis); 367. Central Australian Rock Rat (Zyzomys pedunculatus); 368. Kimberley Rock Rat (Zyzomys woodward); 369. Malayan Tree Rat (Pithecheir parvus); 370. Red Tree Rat (Pithecheir melanurus); 371. Bornean Tree Rat (Pithecheirops otion); 372. Cutch Rat (Cremnomys cutchicus); 373. Elvira Rat (Cremnomys elvira); 374. Crump's Rat (Diomys crumpi); 375. White-tailed Wood Rat (Madromys blanfordi); 376. Sand-colored Soft-furred Rat (Millardia gleadowi); 377. Kondana Soft-furred Rat (Millardia kondana); 378. Common Soft-furred Rat (Millardia
FIGURE 7. WAMR136122 in Taxonomy of the Sand Sliders of Western Australia's central coast (genus Lerista, Squamata: Scincidae): recognition of Lerista miopus (Günther, 1867)
FIGURE 7. WAMR136122, neotype of Lerista miopus (Günther, 1867). A. Whole specimen; B. Lateral head view; C. Dorsal head view. Photo by P. Waddington.
FIGURE 8 in Taxonomy of the Sand Sliders of Western Australia's central coast (genus Lerista, Squamata: Scincidae): recognition of Lerista miopus (Günther, 1867)
FIGURE 8. Lerista miopus in life. Specimen from Tamala Stn, Western Australia, not vouchered, identified using Storr et al. (1981). Photo by S. Wilson.
FIGURE 4. MNHP1246 in Taxonomy of the Sand Sliders of Western Australia's central coast (genus Lerista, Squamata: Scincidae): recognition of Lerista miopus (Günther, 1867)
FIGURE 4. MNHP1246, holotype of Brachystopus lineopunctulatus Duméril and Bibron, 1839. Photo by H. G. Cogger.
FIGURE 1. Map showing collection localities for Lerista lineopunctulata, L. miopus, L. connivens and L in Taxonomy of the Sand Sliders of Western Australia's central coast (genus Lerista, Squamata: Scincidae): recognition of Lerista miopus (Günther, 1867)
FIGURE 1. Map showing collection localities for Lerista lineopunctulata, L. miopus, L. connivens and L. varia.
FIGURE 6 in Taxonomy of the Sand Sliders of Western Australia's central coast (genus Lerista, Squamata: Scincidae): recognition of Lerista miopus (Günther, 1867)
FIGURE 6. Lerista lineopunctulata sensu stricto in life. Specimen from Lancelin, Western Australia, not vouchered, identified using Storr et al. (1981). Photo by S. Wilson.
FIGURE 2 in Taxonomy of the Sand Sliders of Western Australia's central coast (genus Lerista, Squamata: Scincidae): recognition of Lerista miopus (Günther, 1867)
FIGURE 2. Bayesian phylogenetic tree inferred from concatenated, partitioned analysis of four mitochondrial DNA genes showing the paraphyly of L. lineopunctulata and the relationships between these clades and closely related Lerista species. Posterior probabilities for each node is shown if above 0.50.
FIGURE 3 in Taxonomy of the Sand Sliders of Western Australia's central coast (genus Lerista, Squamata: Scincidae): recognition of Lerista miopus (Günther, 1867)
FIGURE 3. Species tree analysis of L. lineopunctulata clades shows the paraphyly of this species with respect to closely related Lerista species. Posterior probability support for each node is shown only if above 0.50.
Supplementary material 1 from: Martins BdaC, Tamanini Mônico A, Mendonça C, Dantas SP, Souza JRD, Hanken J, Lima AP, Ferrão M (2024) A new species of terrestrial foam-nesting frog of the Adenomera simonstuarti complex (Anura, Leptodactylidae) from white-sand forests of central Amazonia, Brazil. Zoosystematics and Evolution 100(1): 233-253. https://doi.org/10.3897/zse.100.110133
Additional information
Figure 9 from: Martins BdaC, Tamanini Mônico A, Mendonça C, Dantas SP, Souza JRD, Hanken J, Lima AP, Ferrão M (2024) A new species of terrestrial foam-nesting frog of the Adenomera simonstuarti complex (Anura, Leptodactylidae) from white-sand forests of central Amazonia, Brazil. Zoosystematics and Evolution 100(1): 233-253. https://doi.org/10.3897/zse.100.110133
Figure 9 Preserved tadpole of Adenomera albarena, Gosner stage 35. Dorsal (A), lateral (B) and ventral views of the body (C) and ventral view of the oral disc (D). E. Detailed view of the spiracle, with its shape and aperture highlighted by dotted lines. Scale bar: 2 mm (A–D); 1 mm (E).
Figure 6 from: Martins BdaC, Tamanini Mônico A, Mendonça C, Dantas SP, Souza JRD, Hanken J, Lima AP, Ferrão M (2024) A new species of terrestrial foam-nesting frog of the Adenomera simonstuarti complex (Anura, Leptodactylidae) from white-sand forests of central Amazonia, Brazil. Zoosystematics and Evolution 100(1): 233-253. https://doi.org/10.3897/zse.100.110133
Figure 6 Three dorsal colour patterns of Adenomera albarena in life. A. Dark blotches few or absent; B. Many dark blotches; and C. Dorsolateral stripe. Unvouchered specimens.
Figure 5 from: Martins BdaC, Tamanini Mônico A, Mendonça C, Dantas SP, Souza JRD, Hanken J, Lima AP, Ferrão M (2024) A new species of terrestrial foam-nesting frog of the Adenomera simonstuarti complex (Anura, Leptodactylidae) from white-sand forests of central Amazonia, Brazil. Zoosystematics and Evolution 100(1): 233-253. https://doi.org/10.3897/zse.100.110133
Figure 5 Ventral views of the hands and feet of Adenomera albarena. A, C. Male holotype INPA-H 44867; B, D. Female paratype, INPA-H 44875. Scale bars: 5 mm.
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Allen Brain Atlas
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