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РИС. 1. Личинки мидии Mytilus galloprovincialis на стадиЯх: A – стерробластулы (стрелками обоЗначены три рЯда ресничек) и B – трохофоры (стрелкоЙ обоЗначены реснички апикального султанчика). МасШтаб: 15 мкм. FIG. 1. Larvae of the mussel Mytilus galloprovincialis at two different stages: (A) –sterroblastula (arrows indicate three rows of cilia) and (B) – trochophore (the arrow indicates cilia of the parietal plume). Scale: 15 µm. in Морфометрические особенности личинок мидии Mytilus galloprovincialis (Lamarck, 1819) (Bivalvia: Mytilidae) в онтогенеЗе
РИС. 1. Личинки мидии Mytilus galloprovincialis на стадиЯх: A – стерробластулы (стрелками обоЗначены три рЯда ресничек) и B – трохофоры (стрелкоЙ обоЗначены реснички апикального султанчика). МасШтаб: 15 мкм. FIG. 1. Larvae of the mussel Mytilus galloprovincialis at two different stages: (A) –sterroblastula (arrows indicate three rows of cilia) and (B) – trochophore (the arrow indicates cilia of the parietal plume). Scale: 15 µm.
Fig. 1 in Benthic and Planktic Foraminifera as Indicators of Late Glacial to Holocene Paleoclimatic Changes in a Marginal Environment: An Example from the Southeastern Bay of Biscay
Fig. 1. Study area bathymetry (Liu and Dittert 2010), surface circulation patterns (Koutsikopoulos et al. 1996), and location of the study Site WH (44°33′N, 2°45′W; 2,000 m water depth). The position of Site KS10b (Mojtahid et al. 2013) is marked by a white square. IPC – Iberian Poleward Current, ENACW – Eastern North Atlantic Central Waters.
Fig. 5. a in Benthic and Planktic Foraminifera as Indicators of Late Glacial to Holocene Paleoclimatic Changes in a Marginal Environment: An Example from the Southeastern Bay of Biscay
Fig. 5. a – oxygen stable isotope ratios (δ18O) performed on G. bulloides and G. inflata; b – Δδ 18O between δ18O and δ18O; G. inflata G. bulloides c – carbon stable isotope ratios (δ13C) performed on G. bulloides and G. inflata; d – Δδ 13C between δ13C and δ13C. The grey G. inflata G. bulloides lines represent FC WH and the black colour represents CADIAC WH. The horizontal dotted lines delimitate the major changes (see text for all the details).
Fig. 4. a in Benthic and Planktic Foraminifera as Indicators of Late Glacial to Holocene Paleoclimatic Changes in a Marginal Environment: An Example from the Southeastern Bay of Biscay
Fig. 4. a – time records in Cores CADIAC WH (black color) and FC WH (grey color) of benthic foraminiferal abundances (ind. g–1 of dry sediment), benthic foraminiferal accumulation rates (ind. cm–2 ka–1), relative abundances of the main benthic species present with ≥ 5% in at least one sample (after removing the non-fossilizing taxa), and species richness; b – time records in Cores CADIAC WH (black color) and FC WH (grey color) of planktic foraminiferal abundances (ind. g–1 of dry sediment), same indications as for benthic faunas. The horizontal dotted lines delimitate the major foraminiferal changes (see text for all the details).
Figure. The phylogenetic tree showing the relationship among Brevibacillus parabrevis strains SA2.2 and TJ2.3, Bacillus licheniformis MG4.2, and their phylogenetically closest type strains. The GenBank accession numbers of the type strains and studied strains are shown following species names. Distance matrix was calculated by Kimura's 2-parameter model. The scale bar indicates 0.02 substitutions per nucleotide position. Alicyclobacillus pohliae AJ564766 served as an out-group. in Distribution of extracellular enzyme-producing bacteria in the digestive tracts of 4 brackish water fish species
Figure. The phylogenetic tree showing the relationship among Brevibacillus parabrevis strains SA2.2 and TJ2.3, Bacillus licheniformis MG4.2, and their phylogenetically closest type strains. The GenBank accession numbers of the type strains and studied strains are shown following species names. Distance matrix was calculated by Kimura's 2-parameter model. The scale bar indicates 0.02 substitutions per nucleotide position. Alicyclobacillus pohliae AJ564766 served as an out-group.
Figure. Provinces situated in the Eastern Anatolia Region, Turkey. Asterisks indicate the sampled provinces in the present study. in Contributions to the knowledge of Agathidinae fauna of the Eastern Anatolia Region of Turkey
Figure. Provinces situated in the Eastern Anatolia Region, Turkey. Asterisks indicate the sampled provinces in the present study.
Text-fig. 3. Rhinoppioides quadrituberculatus MIKO gen. et sp. nov. Above: assumed fragments of legs as seen in body cavity of holotype (Aa – in dorsal view, Ab – in ventral view) and paratype (B, only dorsal view available). Below: speculative reconstruction of legs, assumed segments leg IV in above rows (numbers 1, 3, 5, 7, 12, 13, 14), assumed segments of leg I below (numbers 6, 9, 10). Rest of the segments assumed to belong to legs II and III. Only trochanters III (nr. 8) and IV (nr. 7, 12) undoubtedly belonging to the new species. Bars indicating 50 µm, numbers indicate identity of segments. in Oribatid Mite Fossils From Quaternary And Pre-Quaternary Sediments In Slovenian Caves I.Two New Genera And Two New Species Of The Family Oppiidae From The Early Pleistocene
Text-fig. 3. Rhinoppioides quadrituberculatus MIKO gen. et sp. nov. Above: assumed fragments of legs as seen in body cavity of holotype (Aa – in dorsal view, Ab – in ventral view) and paratype (B, only dorsal view available). Below: speculative reconstruction of legs, assumed segments leg IV in above rows (numbers 1, 3, 5, 7, 12, 13, 14), assumed segments of leg I below (numbers 6, 9, 10). Rest of the segments assumed to belong to legs II and III. Only trochanters III (nr. 8) and IV (nr. 7, 12) undoubtedly belonging to the new species. Bars indicating 50 µm, numbers indicate identity of segments.
Text-fig. 1. Rhinoppioides quadrituberculatus MIKO gen. et sp. nov. A – dorsal view of holotype (prodorsal setae largely missing except right lamellar seta, notogastral setae missing and their insertions not discernable); B – ventral view of holotype (genital and anal valves missing, only insertions of ventral setae visible, gnathosoma missing); C – lateral view of paratype (notogaster missing). Bar indicates 100 µm. For explanation of acronyms see page 31. in Oribatid Mite Fossils From Quaternary And Pre-Quaternary Sediments In Slovenian Caves I.Two New Genera And Two New Species Of The Family Oppiidae From The Early Pleistocene
Text-fig. 1. Rhinoppioides quadrituberculatus MIKO gen. et sp. nov. A – dorsal view of holotype (prodorsal setae largely missing except right lamellar seta, notogastral setae missing and their insertions not discernable); B – ventral view of holotype (genital and anal valves missing, only insertions of ventral setae visible, gnathosoma missing); C – lateral view of paratype (notogaster missing). Bar indicates 100 µm. For explanation of acronyms see page 31.
Text-fig. 1. Geological setting and location of the fossil sites mentioned in this paper. Grey area indicates Cretaceous Basins. in Revision Of Protopteris And Oncopteris Tree Fern Stem Casts From The Late Cretaceous Of Central Europe
Text-fig. 1. Geological setting and location of the fossil sites mentioned in this paper. Grey area indicates Cretaceous Basins.
Text-fig. 2. Stratigraphic ranges of selected porambonitid taxa in West Gondwana (Iberica), Baltica, Perunica and Avalonia. Arrows indicate derivation of early Baltic porambonitids from Gondwanan Poramborthis (1), derivation of Porambonites in Perunica and Avalonia from Baltica (2), and expansion of Porambonites from Baltica and/or Avalonia to West Gondwana (3). in Porambonites Havliceki Sp. Nov., A New Brachiopod From The Šárka Formation (Darriwilian) From Bohemia And Its Contribution To Early History Of The Porambonitidae
Text-fig. 2. Stratigraphic ranges of selected porambonitid taxa in West Gondwana (Iberica), Baltica, Perunica and Avalonia. Arrows indicate derivation of early Baltic porambonitids from Gondwanan Poramborthis (1), derivation of Porambonites in Perunica and Avalonia from Baltica (2), and expansion of Porambonites from Baltica and/or Avalonia to West Gondwana (3).
Fig. 5. Parsimony splits network constructed from a per and ITS2 concatenated sequence data set. Heterozygous specimens are indicated with A and B in Ecological and geographical speciation in Lucilia bufonivora: The evolution of amphibian obligate parasitism
Fig. 5. Parsimony splits network constructed from a per and ITS2 concatenated sequence data set. Heterozygous specimens are indicated with A and B. 'bufonivora_EUROPE_A' represents a consistent haplotype present in all 12 samples from Europe (Table 1), of which just two were heterozygous ('bufonivora_frog' and 'bufonivora_NLWi'). 'bufonivora_CAN' and 'elongata_CAN' are represented by two samples each, none of which were heterozygous. Scale bar represents expected changes per site.
Figure 1 in First report of Drupella cornus Röding, 1798 (Gastropoda: Muricidae), a biological indicator of coral reef habitat of Lakshadweep Archipelago, India
Figure 1. Drupella cornus Röding, 1798, collected at benthic coral reef habitat of Minicoy Island, Lakshadweep.
Text-fig. 4. Platanaceae 1–3. Macginitiea gracilis (LESQUEREUX) J. WOLFE et WEHR leaves and associated reproductive structures 1. Holotype of Aralia gracilis LESQUEREUX from Bridger Pass, Wyoming, USNM 330. 2. Specimen showing the typical configuration of five lobes, Killpecker Creek flora, Wyoming. UF 18126-13242. 3. Silicified M. gracilis leaf from Almont, North Dakota; arrow indicates adjacent Macginicarpa infructescence, UF 15722-29202a. 4. Macginicarpa infructescence from Almont, UF15722-35493. 5. Platananthus sp., Almont, UF 15722-62019. 6. Macginicarpa glabra MANCHESTER infructescence, enlarged from fig. 3, UF 15722-29202b. Specimens in figs 3-6 collected and donated by John Curtis. Scales = 1 cm. Images 3–6 light-dark inverted. in Revisions To Roland Brown'S North American Paleocene Flora
Text-fig. 4. Platanaceae 1–3. Macginitiea gracilis (LESQUEREUX) J. WOLFE et WEHR leaves and associated reproductive structures 1. Holotype of Aralia gracilis LESQUEREUX from Bridger Pass, Wyoming, USNM 330. 2. Specimen showing the typical configuration of five lobes, Killpecker Creek flora, Wyoming. UF 18126-13242. 3. Silicified M. gracilis leaf from Almont, North Dakota; arrow indicates adjacent Macginicarpa infructescence, UF 15722-29202a. 4. Macginicarpa infructescence from Almont, UF15722-35493. 5. Platananthus sp., Almont, UF 15722-62019. 6. Macginicarpa glabra MANCHESTER infructescence, enlarged from fig. 3, UF 15722-29202b. Specimens in figs 3-6 collected and donated by John Curtis. Scales = 1 cm. Images 3–6 light-dark inverted.
Text-fig. 3. CA climate charts for the Monte Tondo and Tossignano floras, showing climatic ranges of the Nearest Living Relatives of the fossil taxa with respect to MAT. Right-hand positoned large bold figures and shaded areas in each case indicate the Coexistence Interval, with the number of overlapping taxa being at a maximum. in Palaeoenvironmental Analysis Of The Messinian Macrofossil Floras Of Tossignano And Monte Tondo (Vena Del Gesso Basin, Romagna Apennines, Northern Italy)
Text-fig. 3. CA climate charts for the Monte Tondo and Tossignano floras, showing climatic ranges of the Nearest Living Relatives of the fossil taxa with respect to MAT. Right-hand positoned large bold figures and shaded areas in each case indicate the Coexistence Interval, with the number of overlapping taxa being at a maximum.
Text–fig. 1. Geographical and geological situation in the James Ross Island region. The locality No. 32 and the position of the Johann Gregor Mendel Czech Antarctic Station (JGM) are indicated. Modified from Sakala and Vodrážka (2014). in Marattiopsis Vodrazkae Sp. Nov. (Marattiaceae) From The Campanian Of The Hidden Lake Formation, James Ross Island, Antarctica.
Text–fig. 1. Geographical and geological situation in the James Ross Island region. The locality No. 32 and the position of the Johann Gregor Mendel Czech Antarctic Station (JGM) are indicated. Modified from Sakala and Vodrážka (2014).
Text-fig. 6b. Z-score profile for Moča skull. Comparison of Moča skull indices with LUP and recent sample, –1.96 and +1.96: 95% tolerance interval (95% of the LUP and recent variability), 0: LUP and recent sample mean, grey band: 95% confidence interval of mean z-scores. Only those samples having more than n = 5 in the particular group are included. in A Late Upper Palaeolithic Skull From Moča (The Slovak Republic) In The Context Of Central Europe
Text-fig. 6b. Z-score profile for Moča skull. Comparison of Moča skull indices with LUP and recent sample, –1.96 and +1.96: 95% tolerance interval (95% of the LUP and recent variability), 0: LUP and recent sample mean, grey band: 95% confidence interval of mean z-scores. Only those samples having more than n = 5 in the particular group are included.
Text-fig. 6. Most parsimonious tree obtained after addition of Acaciaephyllum to the data set of Doyle (2008), with modifications discussed in the text, and with relationships of other taxa fixed with a backbone constraint tree based on results of Doyle (2008). Relative parsimony of alternative positions of Acaciaephyllum is indicated as in Text-fig. 2. Gnet = Gnetales. in Early Cretaceous Monocots: A Phylogenetic Evaluation
Text-fig. 6. Most parsimonious tree obtained after addition of Acaciaephyllum to the data set of Doyle (2008), with modifications discussed in the text, and with relationships of other taxa fixed with a backbone constraint tree based on results of Doyle (2008). Relative parsimony of alternative positions of Acaciaephyllum is indicated as in Text-fig. 2. Gnet = Gnetales.
Text-fig. 4. Most parsimonious trees obtained after addition of Virginianthus (with "Liliacidites" minutus pollen) to the (A) D&E and (B) J/M trees. Relative parsimony of alternative positions of Virginianthus is indicated as in Text-fig. 2; abbreviations as in Text-fig. 1. in Early Cretaceous Monocots: A Phylogenetic Evaluation
Text-fig. 4. Most parsimonious trees obtained after addition of Virginianthus (with "Liliacidites" minutus pollen) to the (A) D&E and (B) J/M trees. Relative parsimony of alternative positions of Virginianthus is indicated as in Text-fig. 2; abbreviations as in Text-fig. 1.
Text-fig. 2. Representative most parsimonious trees obtained after addition of Liliacidites to (A) the D&E tree (Text-fig. 1) and (B) the J/M tree, with relationships among major clades based on the plastid genome analyses of Jansen et al. (2007) and Moore et al. (2007). Thicker lines indicate all most parsimonious (MP), one step less parsimonious (MP+1), and two step less parsimonious (MP+2) positions for Liliacidites. Abbreviations as in Text-fig. 1. in Early Cretaceous Monocots: A Phylogenetic Evaluation
Text-fig. 2. Representative most parsimonious trees obtained after addition of Liliacidites to (A) the D&E tree (Text-fig. 1) and (B) the J/M tree, with relationships among major clades based on the plastid genome analyses of Jansen et al. (2007) and Moore et al. (2007). Thicker lines indicate all most parsimonious (MP), one step less parsimonious (MP+1), and two step less parsimonious (MP+2) positions for Liliacidites. Abbreviations as in Text-fig. 1.
Text-fig. 3. One of two most parsimonious trees obtained after addition of Anacostia (with Similipollis pollen) to the D&E tree. Relative parsimony of alternative positions of Anacostia is indicated as in Text-fig. 2; abbreviations as in Text-fig. 1. in Early Cretaceous Monocots: A Phylogenetic Evaluation
Text-fig. 3. One of two most parsimonious trees obtained after addition of Anacostia (with Similipollis pollen) to the D&E tree. Relative parsimony of alternative positions of Anacostia is indicated as in Text-fig. 2; abbreviations as in Text-fig. 1.
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Allen Brain Atlas
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ABODe is a University of Edinburgh DataShare dataset for behavior classification in group-housed mice using home-cage video, identities, bounding boxes, ground-plate positions, and annotator labels.
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