Find research datasets worth reusing

Fig. 6 in On Powellithecidae fam. nov., a new Pliocene to Recent bryozoan family endemic to New Zealand, with the description of Powellitheca gen. nov. (Bryozoa, Cheilostomata)

Fig. 6. Powellitheca waipukurensis (Waters, 1887) comb. nov. Nukumaruan, Pleistocene, Nukumaru Limestone, Waiinu Beach. A–F. NHMUK BZ 7744. A. General view of two colonies encrusting a bivalve shell. B. Fusion of the two colonies shown in A and formation of kenozooids along the encountering edge. C. Group of fertile zooids and autozooids. D. Ancestrula and early ontogeny. E. Close-up of the minimally calcified ancestrula. F. Autozooidal orifice and avicularium. — G–H. NHMUK BZ 7745. G. Internal view of the proximal, convex, orificial rim lacking a lyrula. H. Multiporous septula on the zooidal vertical walls. Scale bars: A = 1 mm; B = 500 µm; C–D = 200 µm; E–F = 100 µm; G–H = 20 µm.

Fig. 3 in On Powellithecidae fam. nov., a new Pliocene to Recent bryozoan family endemic to New Zealand, with the description of Powellitheca gen. nov. (Bryozoa, Cheilostomata)

Fig. 3. Powellitheca labiosa gen. et sp. nov. NIWA 98320 (A–C, E–F), 98229 (D), Recent, Three King Islands, New Zealand. A. Group of fertile zooids and autozooids. B. Tilted view of the primary orifice of an autozooid. Note the lack of a lyrula. C. Close-up of the frontal, multiporous septula on the distolateral corners and the funnel-shaped pseudopores on the frontal shield. D. Lateral, multiporous septula on the zooidal vertical walls. E–F. Tilted view of the orifice of fertile zooids. Scale bars: A = 500 µm; B–C = 100 µm; D = 200 µm; E = 250 µm; F = 150 µm.

Fig. 2 in On Powellithecidae fam. nov., a new Pliocene to Recent bryozoan family endemic to New Zealand, with the description of Powellitheca gen. nov. (Bryozoa, Cheilostomata)

Fig. 2. Powellitheca terranovae gen. et sp. nov. NIWA 98983, Recent, Stephens Hole, NZOI Station Q686, New Zealand. A. Group of fertile zooids and autozooids. B. Close-up of an autozooid showing frontal, multiporous septula on the distolateral corners. C. Lateral, multiporous septula on the vertical walls of a maternal zooid. Note also the prominent, suboral umbo. D. Avicularium. E. Tilted view of an autozooidal orifice to show the anvil-shaped, downwardly directed lyrula. F. Orifice of a maternal zooid and incomplete ooecium. Scale bars: A = 250 µm; B–C = 100 µm; D–E = 50 µm; F = 150 µm.

Fig. 1 in On Powellithecidae fam. nov., a new Pliocene to Recent bryozoan family endemic to New Zealand, with the description of Powellitheca gen. nov. (Bryozoa, Cheilostomata)

Fig. 1. Emballotheca quadrata (MacGillivray, 1880), NHMUK 1897.5.1.830, Recent, Port Phillip Heads, Victoria, Australia. A. General view of the colony. B. Autozooidal orifice and avicularia. C. Close-up of a condyle with scaled tip. D. Fertile zooid and surrounding autozooids. E. Large, spatulate, frontal avicularium and lateral pore-chamber windows in the vertical walls. Scale bars: A = 500 µm; B = 40 µm; C = 10 µm; D = 200 µm; E = 100 µm.

Fig. 5 in On Powellithecidae fam. nov., a new Pliocene to Recent bryozoan family endemic to New Zealand, with the description of Powellitheca gen. nov. (Bryozoa, Cheilostomata)

Fig. 5. Powellitheca waipukurensis (Waters, 1887) comb. nov. Specimen figured by Brown (1952: fig. 203), NHMUK D36986, Mangapanian, Early Pliocene, Hawkes Bay, Waipukurau Gorge. A. General view of the colony. B. Group of autozooids and fertile zooids showing the dimorphic orifices. C. Group of zooids with avicularia. D. Autozooids. Scale bars: A = 500 µm; B–C = 200 µm; D = 100 µm.

Fig. 7 in On Powellithecidae fam. nov., a new Pliocene to Recent bryozoan family endemic to New Zealand, with the description of Powellitheca gen. nov. (Bryozoa, Cheilostomata)

Fig. 7. Powellitheca terranovae gen. et sp. nov. Underwater photograph taken by Dr. Vincent Zintzen (Department of Conservation, NZ) at the Poor Knights Islands, off the NE coast of North Island, north of Auckland, New Zealand. Note the band of yellow pigment at the colony's growing edges and the 19 yellow tentacles of the autozooids.

opencc-by-4.0May 2017View details →

Sixty-one thousand Recent planktonic foraminifera from the Atlantic Ocean

<p>Here we provide an extensive image library of Recent microfossils (primarily planktonic foraminifera) from the Atlantic Ocean, with accompanying 2D and 3D coordinate data and morphometric measurements.  This data was generated using high-throughput imaging methods (<em>AutoMorph</em>) developed in P.M. Hull's lab at Yale University.</p> <p>The dataset consists of microfossils from 34 sediment samples, mounted on 155- micropaleontological slides, primarily from the North Atlantic Ocean <strong>(metadata_tables.tar.gz</strong>: Table 1). All slides are accessioned to the Yale Peabody Museum of Natural History (YPM) Division of Invertebrate Paleontology with unique YPM catalog numbers (metadata_tables.tar.gz: Table 2). Slides of microfossils were imaged at multiple focal heights (z-planes) using a light microscope with an automated stage and processed with the image processing models of <em>AutoMorph</em> as detailed in Table 2. <em>AutoMorph</em> software and tutorials can be accessed here: https://github.com/HullLab. For an example of a raw slide scan see: Hsiang, Allison Y., Nealson, Kaylea, Elder, Leanne E., Liu, Yusu, & Hull, Pincelli M. (2016). Slide scan example for Automorph. Zenodo. http://doi.org/10.5281/zenodo.167557. </p> <p>124,230 unique objects (primarily microfossils) were identified from the 155 slides of 34 sediment samples, and were classified into 16 object categories (metadata_tables.tar.gz: Table 3).  Object classification is provided in Table 3 and summarized in Table 4 (metadata_tables.tar.gz). Table 5 in metadata_tables.tar.gz  provides a technical validation of the automated 2D morphometric measurements; comparable data validation for the 3D morphometric measurements are provided in Hsiang et al. 2016 (http://dx.doi.org/10.1098/rstb.2015.0227).</p> <p>Images and morphometric data are provided in 12 additional datasets:</p> <p><strong>1) slide_images.tar.gz</strong> contains one image for each slide scanned in this study (155 slides), with a red box around each object extracted using the <em>AutoMorph</em> segment module. Slides are named according to their YPM catalog number and related sample and site information can be found in Tables 1 and 2 (metadata_tables.tar.gz), and in the YPM database (http://collections.peabody.yale.edu/search/) by YPM catalog number. </p> <p><strong>2) edf_images.tar.gz</strong> contains the extended depth of focus images (EDF: a 2D image composite created from multiple z-stacked photographic images) generated by the <em>AutoMorph</em> focus module for each of the 124,230 individual objects identified by segment.</p> <p><strong>3 & 4) obj_zstacks_part1.tar.gz</strong> and <strong>obj_zstacks_part2.tar.gz</strong> contain the original zstack images of each object.  2D outlines and shape measurements for each object are extracted using the<em> AutoMorph</em> module run2dmorph. </p> <p><strong>5) 2d_outline_check.tar.gz</strong> provides an overlay of the extracted 2D outline on the object EDF for quality control purposes for all extracted objects (113,847 objects) and a text file of all objects with failed 2D extractions (10,384 objects).</p> <p><strong>6) 2d_coordinates.tar.gz</strong> provides the 2D coordinates of each object in a single csv (all_coordinates.csv) and by slide (155 csv files named according to YPM catalog number), and a text file of all objects with failed 2D extractions (10,384 objects).</p> <p><strong>7) shape_measurements.csv</strong> contains the complete list of all objects in the dataset (124,230 objects) with the 2D and 3D measurements extracted by the<em> AutoMorph</em> routines run2morph and run3dmorph when available.</p> <p><strong>8 & 9) 3d_pdfs_part1.tar.gz</strong> and <strong>3d_pdfs_part2.tar.gz</strong> provide 3D pdfs of each 3D object extracted (109,207 objects) for quality control purposes and a text file of all objects with failed 3D extractions (15,023 objects). 3D pdfs, meshes and shape measurements were generated by the <em>AutoMorph</em> module run3dmorph. Note that only some pdf viewers are able to display 3d pdfs properly. </p> <p><strong>10-12) 3d_obj_files_part1.tar.gz</strong>, <strong>3d_obj_files_part2.tar.gz</strong>, and <strong>3d_obj_files_part3.tar.gz</strong> provide the 3D mesh coordinates as obj files for each extracted object and a text file of all objects with failed 3D extractions (15,023 objects).</p> <p>This dataset accompanies the manuscript "Sixty-one thousand Recent planktonic foraminifera from the Atlantic Ocean" submitted to <em>Scientific Data</em>. The manuscript describes important details related to data collection and usage and should be consulted before using the data provided here. One key note about this dataset is repeated here as a precaution. We provide image classification for only 4/5<sup>th</sup>s of the complete data set. A random subset (1/5<sup>th</sup> of the classifications) are excluded as a test set, so that this image database can be used in machine learning.</p>

Figure 2 in Cicada minimum age tree: Cryptic speciation and exponentially increasing base substitution rates in recent geologic time

Figure 2. Cicada timetree built by BEAST v1.X, applying 1,534 bp COI sequence. OUTs with isolate number: our own analyzed specimens shown in Table 1, and others: from GenBank/DDJB. In outgroup Hemiptera; #: analyzed family by Johnson et al. (2018); % analyzed family by Misof et al. (2014). Inserted figure: Base substitution rate (= rate median shown at each node; substitutions per site per million year; s/s/myr) vs age (= posterior age shown at each node) diagram. Red approximate curve with its formula was drawn by Excel function, with the intersection for the curve = 0.0128 s/s/myr, the rate median shown on Tracer.

Figure 4 in Cicada minimum age tree: Cryptic speciation and exponentially increasing base substitution rates in recent geologic time

Figure 4. Number of base changes of transition and tansversion vs corrected pairwide distance diagram for whole mitochondrial gene.

Figure 1 in Cicada minimum age tree: Cryptic speciation and exponentially increasing base substitution rates in recent geologic time

Figure 1. Simplified cicada timetree built by BEAST v1.X, applying a 1,534 bp in maximum COI sequence. Inserted figure: Base substitution rate (= ratemedian shown at each node; substitutions per siteper millionyear; s/s/ myr) vsage (= posterior age shown at each node) diagram. Red approximate curve with its formula was drawn by an Excel function, with the intersection for the curve = 0.0128 s/s/myr, the rate median shown on Tracer.

Figure 3 in Cicada minimum age tree: Cryptic speciation and exponentially increasing base substitution rates in recent geologic time

Figure 3. Cicada timetree built by BEAST v1.X, applying 1,534 bp COI and 874 bp 18S rRNA sequences. OUTswith isolate number: our own analyzed specimens shown in Table 1, and others: from GenBank/DDJB. In outgroup Hemiptera; #: analyzed family by Johnson et al. (2018); % analyzed family by Misof et al. (2014). Inserted figure: Base substitution rate (= rate median shown at each node; substitutions per site per million year; s/s/myr) vs age (= posterior age shown at each node) diagram. Red approximatecurve with its formulawas drawn by Excel function, with the intersection for the curve = 0.0114 s/s/myr, the rate median shown on Tracer. Note that this rate is a little slower than thatsolely of COI in Figures 1 and 2, reflecting slowerrate of 18S rRNAthan COI (see Osozawa et al. 2017a).

opencc-by-4.0Nov 2023View details →

Supporting information for "Illuminating the nanostructure of diffuse interfaces: Recent advances and future directions in reflectometry techniques"

<p>This deposition contains the data and analysis (Jupyter notebooks) detailed in Illuminating the nanostructure of diffuse interfaces: Recent advances and future directions in reflectometry techniques. All Jupyter notebooks have also been converted into PDF files for ease of viewing.</p><p> </p><p>All data and code (notebooks) required to reproduce the analysis can be found within the "supporting_data_analysis.zip" archive. This archive contains two sub-directories:</p><ul><li>insituAnalysis<ul><li>Jupyter notebook outlining how to perform the `on-the-fly' analysis.</li><li>Data directory containing all temporally sliced neutron reflectometry data.</li></ul></li><li>MaxEnt<ul><li>Jupyter notebook outlining how to perform the maximum entropy modelling approach for polymer volume fraction profiles.</li><li>Data directory containing relevant neutron reflectometry data and PCHIP spline modelling by Gresham et al. (<a href="www.doi.org/10.1107/S160057672100251X">10.1107/S160057672100251X</a>).</li><li>Code available on the <a href="https://github.com/refnx/refnx-models/tree/master/MaxEntVFP">refnx-models GitHub repo</a>.</li></ul></li></ul><p> </p>

opencc-by-4.0Sep 2021View details →

Fig. 2. A-B in Orbitolinids And Other Larger Benthic Foraminifera From The Aptian-Albian Of Tibet: Critical Discussion Of Some Recently Published Data

Fig. 2. A-B, Praeorbitolina cormyi Schroeder fide BouDagher-Fadel et al. (2017, fig. 9.6 and 9.5), Lower Cretaceous of Tibet. C-D, Paleodictoyconus actinostoma Arnaud-Vanneau & Schroeder, early Aptian of Central Iran. E, Praeorbitolina cf. wienandsi Schroeder fide BouDagher-Fadel et al. (2107, fig. 12.1). F-G, juvenile specimens of Paleodictyoconus sp., (?P. actinostoma Arnaud-Vanneau & Schroeder), early Aptian of Central Iran. H, Pseudochoffatella cuvillieri Deloffre fide Bou-Dagher-Fadel et al. (2017, fig. 12.7). I-K, unknown lituolid, early Aptian Taft Formation of Central Iran. Figures without scale.

opencc-by-4.0Sep 2021View details →

Fig. 1. A in Orbitolinids And Other Larger Benthic Foraminifera From The Aptian-Albian Of Tibet: Critical Discussion Of Some Recently Published Data

Fig. 1. A, Mesorbitolina parva (Douglass) fide BouDagher-Fadel et al. (2017, excerpt of fig. 8), Lower Cretaceous of Tibet. B-E, Praeorbitolina cormyi Schroeder, axial sections perpendicular to the median plane (B-C: excerpt of Bosselini et al., 1999, fig. 5a and 5g, early Aptian of Ethiopia; D-E: early Aptian of Iran). Figures without scale.

opencc-by-4.0Mar 2024View details →

Data from: Distribution, ecology, and natural history of the recently rediscovered and critically endangered Santa Marta Sabrewing

<div><strong>Description for "RawData&media_Cphainopeplus" dataset.</strong></div> <div> </div> <div>Data from: Distribution, ecology, and natural history of the recently rediscovered and critically endangered Santa Marta Sabrewing</div> <div>MS bioRxiv ID: </div> <div>Article DOI:</div> <div> </div> <div>Please address questions to:</div> <div> </div> <div>Esteban Botero D., Dr.Sc.</div> <div>Director of Conservation Science</div> <div>SELVA: Research for Conservation in the Neotropics</div> <div>http://www.selva.org.co</div> <div>https://www.selva.org.co/integrantes/esteban-botero-delgadillo/</div> <div>e-mail: eboterod@gmail.com; esteban.botero@selva.org.co</div> <div> </div> <div>=====================================================================================</div> <div>=====================================================================================</div> <div> </div> <div> </div> <div><strong>General information:</strong></div> <div> </div> <div>The whole dataset contains information on Santa Marta Sabrewing, a critically endangered (CR) hummingbird species endemic to the Sierra Nevada de Santa Marta, northern Colombia. Part of the data are of public access and consist of historical geographic records, while another part contains data collected from a focal study population of Santa Marta Sabrewing inhabiting along the La Macana stream, in the Guatapurí River Basin, Cesar Department. No exact coordinates from the focal population were included in this dataset or related documents/materials to protect these locations.</div> <div> </div> <div>The data set is comprised by an Excel file (four spreadsheets) and two short video files that are explained below.</div> <div> </div> <div>*************************************************************************************</div> <div> </div> <div><strong>Excel file "RawData_Cphainopeplus.xlsx" (created 12-02-2024)</strong></div> <div> </div> <div> </div> <div>********** Spreadsheet "1. ConfirmedLoc" **********</div> <div>This spreadsheet contains metadata for the only five records of Santa Marta Sabrewing with confirmatory evidence.</div> <div> </div> <div>The matrix contains the following variables:</div> <div> </div> <div>VARIABLE DESCRIPTION</div> <div> </div> <div>Locality: Name of the locality as described in museums or public databases.</div> <div>Department: Name of department where the locality is found.</div> <div>Latitude: Latitude in decimal degrees.</div> <div>Longitude: Longitude in decimal degrees.</div> <div>Record status: Confirmed (with confirmatory evidence) or unconfirmed (without or needing further examination).</div> <div>Evidence: Evidence available to confirm the record.</div> <div>Source: Source of the record.</div> <div>Observations: Additional information for each row.</div> <div> </div> <div> </div> <div>********** Spreadsheet "2. PointCountDat" **********</div> <div>This spreadsheet contains information from bird counts aimed at detecting Santa Marta Sabrewing.</div> <div> </div> <div>The matrix contains the following variables:</div> <div> </div> <div>VARIABLE DESCRIPTION</div> <div> </div> <div>ID: Point-count station ID.</div> <div>Elevation: Elevation in m.</div> <div>Native: Proportion (0–1) of native vegetation 100 m around the point coordinates.</div> <div>Transformed: Proportion (0–1) of transformed vegetation 100 m around the point coordinates.</div> <div>R1: First point-count replicate, with 0 = absence and 1 = presence.</div> <div>R2: Second point-count replicate, with 0 = absence and 1 = presence.</div> <div>R3: Third point-count replicate, with 0 = absence and 1 = presence.</div> <div>R4: Fourth point-count replicate, with 0 = absence and 1 = presence.</div> <div> </div> <div> </div> <div>********** Spreadsheet "3. Behav" **********</div> <div>This spreadsheet contains information from ad libitum observations to characterize habitat associations and general behaviour of Santa Marta Sabrewing.</div> <div> </div> <div>The matrix contains the following variables:</div> <div> </div> <div>VARIABLE DESCRIPTION</div> <div> </div> <div>Date: Date (day/month/year).</div> <div>Hour: Hour in 24h format.</div> <div>Elevation: Elevation in m.</div> <div>No. Indiv.: No. of individuals of Santa Marta Sabrewing recorded.</div> <div>Behaviour: Simple categories describing sabrewing behaviour.</div> <div>Habitat: Simple categories describing habitat type where sabrewing was recorded.</div> <div> </div> <div> </div> <div>********** Spreadsheet "4. HabitatNeu" **********</div> <div>This spreadsheet contains estimated quantities for estimating Neu´s habitat proportions for Santa Marta Sabrewing. </div> <div> </div> <div>The matrix contains the following variables:</div> <div> </div> <div>VARIABLE DESCRIPTION</div> <div> </div> <div>Habitat: Simple categories describing habitat type where sabrewing was recorded.</div> <div>Obs. Count: No. of Santa Marta Sabrewing records in each habitat type.</div> <div>Hab. Prop.: Proportional area (0–1) of each habitat type in study area.</div> <div>Expected Use: Expected No. of records based on each habitat's proportional area.</div> <div>Sel. Ratio: Ratio between observed count and expected use.</div> <div>Standard. Ratio: Standardized selection ratio (0–1).</div> <div> </div> <div>*************************************************************************************</div> <div> </div> <div><strong>Video file "Campylopterus_threat.mp4" (modified 09-02-2024)</strong></div> <div> </div> <div>A slow-motion (~0.1 x) video showing a perching male Santa Marta Sabrewing involved in a persecution flight with a conspecific male aggressor. <span>Footage was taken along the course of La Macana stream, near Chemesquemena village (Cesar Department, northern Colombia). </span>Video: Elquin Toro © (reproduced with permission).</div> <div> </div> <div>*************************************************************************************</div> <div> </div> <div><strong>Video file "Campylopterus_fight.mp4" (modified 09-02-2024)</strong></div> <div> </div> <div>A lek-attending male Santa Marta Sabrewing vocalizing in a perch and subsequently adopting a threatening body posture with wing and tail feathers extended towards a conspecific male intruder. <span>Footage was taken along the course of La Macana stream, near Chemesquemena village (Cesar Department, northern Colombia). </span>Video: Elquin Toro © (reproduced with permission).</div> <div> </div> <div> </div> <div>=====================================================================================</div> <div> </div> <div> </div> <div><strong>Methodological information (for more details, please see the related manuscript):</strong></div> <div> </div> <div>We conducted a thorough revision of scientific literature, international public databases, digital collections, and museum international/national bird collections in search of geographical records of Santa Marta Sabrewing.</div> <div> </div> <div>Aside from the locality where the focal population was found (along the La Macana stream, near the Chemesquemena village, Cesar department), we also conducted three 4–7-day field expeditions to three other localities where Santa Marta Sabrewing could stably occur: San Lorenzo ridge (Magdalena Department); the upper Rioancho River basin, in Dibulla (La Guajira Department); Aracataca (Magdalena Department).</div> <div> </div> <div>We projected Santa Marta Sabrewing's extent of occurrence (EOO) and area of occupancy (AOO). Our EOO and AOO projections were compared with the threshold values given under the IUCN’s criteria B1 and B2 (IUCN 2022). To this end, we delimited suitable habitat in ArcGIS Desktop 10 (ESRI 2011) using a vegetation layer from the CORINE Land Cover Methodology from Colombia, 2018, at 1:100,000 scale (IDEAM 2021), and a layer of biomes compiled in the public-access portal of the Land-use Planning Geographic Information System (SIG-OT) of the “Agustín Codazzi” Geographic Institute of Colombia (https://geoportal.igac.gov.co).</div> <div> </div> <div>We conducted bird counts from September to December 2022 to estimate local abundance along the course of La Macana stream, near Chemesquemena village. Bird surveys were carried out using 20 georeferenced point-count stations (30 m radius), in which one observer searched for Santa Marta Sabrewing for 15 min. One count per station was conducted every month between 07:00 to 11:00s. Detection histories were analysed using the <em>occu</em> function in the <em>unmarked</em> package (Fiske and Chandler 2011) in R 4.0.2 (R Core Team 2020).</div> <div> </div> <div>In the same locality, we also conducted ad libitum observations from July 2022 to October 2023 to describe different aspects of the species’ natural history. We conducted 2–3-day monthly visits to monitor individuals and territories year-round. We described feeding habits and aspects of social or breeding behaviour, including territorial and lekking displays, vocal activity, and lek conformation.</div> <div> </div> <div>Lastly, we performed acoustic analysis focused on a description of Santa Marta Sabrewing territorial calls based on three males. We selected and analyzed a single high-quality recording per male of 20 seconds each. We used a Zoom H6 recorder coupled with a Rode NTG4 phantom-powered shotgun microphone. We visualized and analyzed the recordings using the Seewave package (Sueur et al. 2008) in R.</div> <div> </div> <div> </div> <div><strong>References:</strong></div> <div> </div> <div>ESRI (2011). ArcGIS Desktop: Release 10. Redlands, CA, USA: Environmental Systems Research Institute.</div> <div> </div> <div>Fiske, I., and Chandler, R. (2011). “unmarked”: an R package for Fitting Hierarchical Models of Wildlife Occurrence and Abundance. J. Stat. Soft. 43: 1–23.</div> <div> </div> <div>IDEAM (2021). Leyenda nacional de coberturas de la tierra. Metodología CORINE Land Cover adaptada para Colombia escala 1:100.000 (período 2018). Bogotá, Colombia: Instituto de Hidrología, Meteorología y Estudios Ambientales (IDEAM).</div> <div> </div> <div>IUCN Standards and Petitions Committee (2022). Guidelines for using the IUCN Red List Categories and Criteria. Version 15. Prepared by the Standards and Petitions Committee. https://www.iucnredlist.org/documents/RedListGuidelines.pdf</div> <div> </div> <div>R Core Team. (2020). R: a language and environment for statistical computing, version 4.0.2. R Foundation for Statistical Computing, Vienna, Austria, http://www.R.project.org</div> <div> </div> <div>Sueur, J., Aubin, T., and Simonis, C. (2008). Seewave: a free modular tool for sound analysis and synthesis. Bioacoustics 18: 213–226.</div> <div> </div> <div>=====================================================================================</div> <div>=====================================================================================</div> <p> </p>

opencc-by-4.0Feb 2023View details →

Figure 1 in Aeshna affinis Vander Linden, 1820 (Odonata: Aeshnidae) in the Iberian Peninsula: A review of past and recent records, and a larval biometric study

Figure 1. Body length (A), prementum (B), supracoxal armature of prothorax (C), lateral spines on segments 6 to 9 of the abdomen and ovipositor (D), extremity of abdomen: cerci, paraprocts, and epiproct (E). / Longitud corporal (A), prementón (B), armadura supracoxal del protórax (c), espinas laterales de los segmentos abdominals 6 a 9 y ovipositor (D), extremo final del abdomen: cercos, paraproctos y epiprocto (E).

Figure 10 in Recent Benthic foraminiferal biofacies in the Bakkhali region, West Bengal, India

Figure 10. (a)Variation of Total Foraminiferal Number with depth (C2); (b) Variation of living foraminifera with depth (C2).

Figure 9 in Recent Benthic foraminiferal biofacies in the Bakkhali region, West Bengal, India

Figure 9. (a) Variation of Total Foraminiferal Number with depth (C1); (b) Variation of living foraminifera with depth (C1).

Plate 3.1 7 in Recent Benthic foraminiferal biofacies in the Bakkhali region, West Bengal, India

Plate 3.1 7 – Asterorotalia pulchella (S); 18 - Asterorotalia pulchella (U); 19 – Cribroelphidium hispidulum (U); 20 – Cribroelphidium poeynum (U); Legends: S – Spiral view; U – Umbilical view; Si – Side view.

Figure 6 in Recent Benthic foraminiferal biofacies in the Bakkhali region, West Bengal, India

Figure 6. Biofacies map of the study area based on the living population of foraminifera (yellow representing Ammonia tepida – Ammonia beccarii biofacies, green representing Haynesina germanica – Ammonia tepida biofacies and red representing Ammonia tepida – Haynesina germanica biofacies).