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Fig. 2 in A New Luperosaurus (Squamata: Gekkonidae) From The Sierra Madre Of Luzon Island, Philippines
Fig. 2. Luperosaurus kubli, holotype (PNM 9156; adult male, SVL = 104.5 mm): A, dorsal view of head, with snout tilted forward 10°); B, lateral view of head; C, ventral view of head; D, palmar surface of right manus.
SNBS:GB-03 - A High Sierra Time-Lapse dataset
<p>These images were collected between 2018 and 2020 using a Wingscapes TimelapseCam Pro. They are used to produce Figure 2 in the drpToolkit software note published in Methods in Ecology and Evolution. </p>
Figure 5 from: Pérez-Luque A, Bonet F, Pérez-Pérez R, Aspizua R, Lorite J, Zamora R (2014) Sinfonevada: Dataset of Floristic diversity in Sierra Nevada forests (SE Spain). PhytoKeys 35: 1-15. https://doi.org/10.3897/phytokeys.35.6363
Figure 5 - Location of the forest-inventory plots. This map shows the location of the forest-inventory plots and the distribution of the ecosystem types present in Sierra Nevada. The vegetation is predominantly high-mountain shrublands and pine plantations, with some natural forests (oaks, Pyrenean oaks, maples, etc.).
Figure 4 from: Pérez-Luque A, Bonet F, Pérez-Pérez R, Aspizua R, Lorite J, Zamora R (2014) Sinfonevada: Dataset of Floristic diversity in Sierra Nevada forests (SE Spain). PhytoKeys 35: 1-15. https://doi.org/10.3897/phytokeys.35.6363
Figure 4 - Diagram of integration of SINFONEVADA within Information System of Sierra Nevada Global Change Observatory. The original database of SINFONEVADA contains two types of information: forest attributes and related information and occurrence data. This information was integrated into the Information System of Sierra Nevada Global Change Observatory. After a validation process (see Quality Control section) the occurrence data were accommodated to Darwin Core Archive to integrate in GBIF.
Figure 3 from: Pérez-Luque A, Bonet F, Pérez-Pérez R, Aspizua R, Lorite J, Zamora R (2014) Sinfonevada: Dataset of Floristic diversity in Sierra Nevada forests (SE Spain). PhytoKeys 35: 1-15. https://doi.org/10.3897/phytokeys.35.6363
Figure 3 - Taxonomic coverage. The figure shows the taxonomic coverage for class, order and family. The circles size are proportional to the number of records in the Sinfonevada database. Numbers indicates the percentage of records. All taxonomic classes included in the database are shown. For order and family rank, only the top 10 are shown. Colour indicates the taxonomic class: green (Liliopsida); black (Magnoliopsida) and blue (Pinopsida).
Figure 2 from: Pérez-Luque A, Bonet F, Pérez-Pérez R, Aspizua R, Lorite J, Zamora R (2014) Sinfonevada: Dataset of Floristic diversity in Sierra Nevada forests (SE Spain). PhytoKeys 35: 1-15. https://doi.org/10.3897/phytokeys.35.6363
Figure 2 - Structure of the Sierra Nevada Global Change Observatory. The four cornerstones of the research project are shown: monitoring program, adaptive management, information systems and dissemination. A monitoring program is needed to identify the impacts of global change over Sierra Nevada. The information compiled needs to be transformed into useful knowledge for the managers to carry out an active and adaptive management of natural resources. To achieve this, it is essential that all data be integrated and analysed in an information system. Finally, the general public should be informed of both the results obtained and methodologies used, through effective outreach activities.
Figure 1 from: Pérez-Luque A, Bonet F, Pérez-Pérez R, Aspizua R, Lorite J, Zamora R (2014) Sinfonevada: Dataset of Floristic diversity in Sierra Nevada forests (SE Spain). PhytoKeys 35: 1-15. https://doi.org/10.3897/phytokeys.35.6363
Figure 1 - Location of Sierra Nevada mountain (southern Spain). The boundaries of the National and Natural Parks are shown. We used a Landsat 5 image (2001) as background.
Figure 4 from: Espinasa L, D. Bartolo N, E. Newkirk C (2014) DNA sequences of troglobitic nicoletiid insects support Sierra de El Abra and the Sierra de Guatemala as a single biogeographical area: Implications for Astyanax. Subterranean Biology 13: 35-44. https://doi.org/10.3897/subtbiol.13.7256
Figure 4 - The Boquillas River has changed its course throughout time. The Boquillas River currently separates the karstic areas of Sierra de Guatemala from the Sierra the El Abra. In the upper part of the figure, the Boquillas River is seen crossing the sierras through the Servilleta canyon. On the bottom part of the figure, a fossil canyon indicates the river's ancient course. Caves that in the past connected the Sierra de El Abra in the south to the Sierra de Guatemala in the north were only recently geologically truncated by the erosion of the new river course. Limestone is restricted to the green forested hills.
Figure 3 from: Espinasa L, D. Bartolo N, E. Newkirk C (2014) DNA sequences of troglobitic nicoletiid insects support Sierra de El Abra and the Sierra de Guatemala as a single biogeographical area: Implications for Astyanax. Subterranean Biology 13: 35-44. https://doi.org/10.3897/subtbiol.13.7256
Figure 3 - Base pair differences versus estimates of divergence in nicoletiids. Base pair differences in the 16S rRNA fragment is plotted against estimates of divergence times millions of years ago (Mya). Molecular clock calibrating points were extracted from: a populations of Anelpistina musticensis that got separated into different islands when the sea level rose after glacial times 12,000 years ago (Espinasa et al. 2011) b and c species of Prosthecina and d species of Anelpistina from Baja California that got separated from the mainland species when the Gulf of Cortes formed 5 mya (Espinasa et al. 2009) e time when nicoletiids arose from a common ancestor with Lepismatids 302 mya (Regier et al. 2010), and f time when insects arose from a common ancestor with anostraca in the Silurian-Ordovician boundary 427 mya (Gaunt and Miles 2002). The lower arrow indicates the 11–12 bp differences between the Sierra de Guatemala and the Sierra de El Abra Anelpistina populations. Such sequence difference is consistent with a common origin very recently, less than 12,000 years ago, and therefore after the environmental disturbances of the ice age.
Figure 2 from: Espinasa L, D. Bartolo N, E. Newkirk C (2014) DNA sequences of troglobitic nicoletiid insects support Sierra de El Abra and the Sierra de Guatemala as a single biogeographical area: Implications for Astyanax. Subterranean Biology 13: 35-44. https://doi.org/10.3897/subtbiol.13.7256
Figure 2 - Anelpistina quinterensis is one of the most troglomorphic described species of nicoletiids. This relatively large eyeless insect is albino and has extremely elongated appendages. Its habitat is restricted to very humid portions of the caves such as mud banks. It is doubtful that it can survive in an epigean environment. Its habitat probably reflects connectivity within a karstic area throughout geologic times and during the evolutionary history of the species.
Figure 1 from: Espinasa L, D. Bartolo N, E. Newkirk C (2014) DNA sequences of troglobitic nicoletiid insects support Sierra de El Abra and the Sierra de Guatemala as a single biogeographical area: Implications for Astyanax. Subterranean Biology 13: 35-44. https://doi.org/10.3897/subtbiol.13.7256
Figure 1 - The Cañon de la Servilleta of the River Boquillas separates the contiguous Sierra de Guatemala, to the north, from the Sierra de El Abra, in the south. Limestone is restricted to the green forested hills. This study tested if this 100 m high, 100 m wide canyon was an effective biological barrier that prevented underground migration of troglobites between the two karstic areas.
Figure 1 from: Parra-Olea G, Rovito S, Lee D, Wake D (2012) A new species of Bolitoglossa (Amphibia, Caudata) from the Sierra de Juárez, Oaxaca, Mexico. ZooKeys 185: 55-71. https://doi.org/10.3897/zookeys.185.1146
Figure 1 - Map of the localities of Bolitoglossa (Nanotriton) used in the morphological study. Locality numbers correspond to those in Table 1. Green points represent Bolitoglossa chinanteca populations, pink points Bolitoglossa nympha populations, blue points Bolitoglossa occidentalis populations, and red points Bolitoglossa rufescens populations.
Figure 3 from: Parra-Olea G, Rovito S, Lee D, Wake D (2012) A new species of Bolitoglossa (Amphibia, Caudata) from the Sierra de Juárez, Oaxaca, Mexico. ZooKeys 185: 55-71. https://doi.org/10.3897/zookeys.185.1146
Figure 3 - Photographs of the live and preserved holotype. A Holotype of Bolitoglossa chinanteca B Holotype of Bolitoglossa chinanteca with a sympatric individual of Bolitoglossa rufescens C Dorsum and D venter of preserved holotype E Ventral view of holotype before preservation, showing color in life F Right hand, G right foot H gular region and I side view of head of preserved holotype. J Photograph of the type locality of Bolitoglossa chinanteca, including banana plants where the type series was collected. All photographs by S. M. Rovito.
Figure 2 from: Parra-Olea G, Rovito S, Lee D, Wake D (2012) A new species of Bolitoglossa (Amphibia, Caudata) from the Sierra de Juárez, Oaxaca, Mexico. ZooKeys 185: 55-71. https://doi.org/10.3897/zookeys.185.1146
Figure 2 - Maximum likelihood gene tree of 16S+cytb genes. Numbers above branches represent support values from 1000 bootstrap replicates.
Figure 2 from: Riera R, Escanez A, González Á, Sierra Á (2012) On the occurrence of egg masses of the diamond-shaped squid Thysanoteuthis rhombus Troschel, 1857 in the subtropical eastern Atlantic (Canary Islands). A potential commercial species? ZooKeys 222: 69-76. https://doi.org/10.3897/zookeys.222.2835
Figure 2 - Some Thysanoteuthis rhombus egg masses recorded (numbers refer to descriptions in Table 1 and Figure 1).
Figure 1 from: Riera R, Escanez A, González Á, Sierra Á (2012) On the occurrence of egg masses of the diamond-shaped squid Thysanoteuthis rhombus Troschel, 1857 in the subtropical eastern Atlantic (Canary Islands). A potential commercial species? ZooKeys 222: 69-76. https://doi.org/10.3897/zookeys.222.2835
Figure 1 - Distribution of egg masses of Thysanoteuthis rhombus in Canary Islands. Triangles: literature records. Circles: new data (numbers refer to descriptions in Table 1).
Figure 98 from: Siler C, Brown R, Oliveros C, Welton L, Rock A, Swab J, Van Weerd M, van Beijnen J, Rodriguez D, Jose E, Diesmos A (2013) The amphibians and reptiles of Luzon Island, Philippines, VIII: the herpetofauna of Cagayan and Isabela Provinces, northern Sierra Madre Mountain Range. ZooKeys 266: 1-120. https://doi.org/10.3897/zookeys.266.3982
Figure 98 - Trimeresurus flavomaculatus (KU 330049)from mid-elevation, Mt. Cagua, Location 1b. Photo: RMB.
Figure 99 from: Siler C, Brown R, Oliveros C, Welton L, Rock A, Swab J, Van Weerd M, van Beijnen J, Rodriguez D, Jose E, Diesmos A (2013) The amphibians and reptiles of Luzon Island, Philippines, VIII: the herpetofauna of Cagayan and Isabela Provinces, northern Sierra Madre Mountain Range. ZooKeys 266: 1-120. https://doi.org/10.3897/zookeys.266.3982
Figure 99 - Cuora amboinensis amboinensis (ACD 3229, deposited in PNM) from Barangay Binatug (Location 22). Photo: K. M. Hesed.
Figure 94 from: Siler C, Brown R, Oliveros C, Welton L, Rock A, Swab J, Van Weerd M, van Beijnen J, Rodriguez D, Jose E, Diesmos A (2013) The amphibians and reptiles of Luzon Island, Philippines, VIII: the herpetofauna of Cagayan and Isabela Provinces, northern Sierra Madre Mountain Range. ZooKeys 266: 1-120. https://doi.org/10.3897/zookeys.266.3982
Figure 94 - Tropidonophis dendrophiops (KU 330031) from mid-elevation, Mt. Cagua, Location 1b. Photo: RMB.
Figure 97 from: Siler C, Brown R, Oliveros C, Welton L, Rock A, Swab J, Van Weerd M, van Beijnen J, Rodriguez D, Jose E, Diesmos A (2013) The amphibians and reptiles of Luzon Island, Philippines, VIII: the herpetofauna of Cagayan and Isabela Provinces, northern Sierra Madre Mountain Range. ZooKeys 266: 1-120. https://doi.org/10.3897/zookeys.266.3982
Figure 97 - Oxyrhabdium leporinum leporinum(KU 330079)from mid-elevation, Mt. Cagua, Location 1b. Photo: RMB.
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