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Figure 1 in Use of homeophathic preparations for red spider mite, Tetranychus urticae (Acari: Tetranychidae) control in strawberry plants
Figure 1. Degree of a) Incidence, and b) severity caused by T. urticae in strawberry plants 30 and 60 days after applying the treatments: Distilled water (Ctl); 6 and 30 CH Strawberry leaves homeopathic (Agroh); 6 and 30 CH Bovista (Bov); 6 and 30 CH Belladonna (Bellad); 6 and 30 CH Arnica (Árni) and 6 and 30 CH Ferrum sulphuricum (FS). Treatments with the same letter are not significantly different between them (p <0.05) (n = 8).
Figure 2 in Sublethal effects of cyflumetofen and spirodiclofen on biological parameters of citrus red mite, Panonychus citri McGregor (Acari: Tetranychidae)
Figure 2. Age-stage specific survival rate (Sxj) of offspring from P. citri females treated with LC20 sublethal concentration of cyflumetofen and spirodiclofen compared with untreated females.
Figure 1. A in The Caspian red deer, Cervus elaphus maral (Mammalia: Cervidae): a new host record for Rhipicephalus (Boophilus) annulatus (Acari: Ixodidae) in northern Iran
Figure 1. A combined phylogenetic tree constructed using Bayesian Inference method based on ITS2/16S rRNA sequence data of Rhipicephalus (Boophilus) species in this study with sequences originated from various part of world retrieved from GenBank database. The main R. (B.) annulatus clade separated by a vertical double headed line. The taxa were defined with a name of species, country, GenBank accession number (taxon of the present study is bold). Posterior probability values inserted in the place of nodes. Branch lengths are proportional to the evolutionary changes. Rhipicephalus sanguineus assigned as outgroup taxon.
Figure 3 in Sublethal effects of cyflumetofen and spirodiclofen on biological parameters of citrus red mite, Panonychus citri McGregor (Acari: Tetranychidae)
Figure 3. Age-stage life expectancy (exj) of offspring from P. citri females treated with LC20 sublethal concentration of cyflumetofen and spirodiclofen compared with untreated females.
Text-fig. 1. a: Po Plain and foothills of the Northern Apennine in Northern Italy (inset) with the location of Oriolo (black star) and other Early and Middle Pleistocene plant localities, Enza and Stirone. Red lines indicate the frontal thrust arcs (modified from Martinetto et al. 2015). b: The "La Salita" section, Oriolo and chronology of the two "Sabbie gialle" cycles based on large mammals and palaeomagnetic correlation (modified from Toniato et al. 2017; IMMS 2020* [Italian Mediterranean Marine Stages] updated from Cohen and Gibbars 2020; GTS 2021* [Global Time Scale] updated from Head et al. 2021). c: Quarry "La Salita", Oriolo, in 1987. Main unconformities (U) separating the two "Sabbie gialle" cycles and terrestrial deposits on top are shown. Leaf symbols indicate the positions of some of the layers rich in fossil leaves (photo by G. B. Vai, modified). d: Surroundings of Faenza with the location of Oriolo and adjacent coeval sites yielding plant macrofossils. in The Late Early Pleistocene Flora Of Oriolo, Faenza (Italy): Assembly Of The Modern Forest Biome
Text-fig. 1. a: Po Plain and foothills of the Northern Apennine in Northern Italy (inset) with the location of Oriolo (black star) and other Early and Middle Pleistocene plant localities, Enza and Stirone. Red lines indicate the frontal thrust arcs (modified from Martinetto et al. 2015). b: The "La Salita" section, Oriolo and chronology of the two "Sabbie gialle" cycles based on large mammals and palaeomagnetic correlation (modified from Toniato et al. 2017; IMMS 2020* [Italian Mediterranean Marine Stages] updated from Cohen and Gibbars 2020; GTS 2021* [Global Time Scale] updated from Head et al. 2021). c: Quarry "La Salita", Oriolo, in 1987. Main unconformities (U) separating the two "Sabbie gialle" cycles and terrestrial deposits on top are shown. Leaf symbols indicate the positions of some of the layers rich in fossil leaves (photo by G. B. Vai, modified). d: Surroundings of Faenza with the location of Oriolo and adjacent coeval sites yielding plant macrofossils.
Text-fig. 3. "Rzehakia beds" at Líšeň-Neklež locality. 1 – topsoil, 2 – greenish-gray clay, locally yellow-brown, 3 – ochre-brown coarse sand, 4 – conglomerate with clasts of granodiorite, 5 – grey-brown medium-grained sand, 6 – light yellowish fine sand, 7 – re-sedimented red-brown eluvium of granodiorite, 8 – re-sedimented red-brown granodiorite debris, 9 – granodiorite, 10 – fossil macroflora. in A New Early Miocene (Ottnangian) Flora Of The "Rzehakia Beds" From Brno-Líšeň
Text-fig. 3. "Rzehakia beds" at Líšeň-Neklež locality. 1 – topsoil, 2 – greenish-gray clay, locally yellow-brown, 3 – ochre-brown coarse sand, 4 – conglomerate with clasts of granodiorite, 5 – grey-brown medium-grained sand, 6 – light yellowish fine sand, 7 – re-sedimented red-brown eluvium of granodiorite, 8 – re-sedimented red-brown granodiorite debris, 9 – granodiorite, 10 – fossil macroflora.
Fig. 7 in Red Sea Leucothoidae (Crustacea: Amphipoda) including new and re-described species
Fig. 7. Leucothoe minoculis sp. nov., holotype, ♂, 5.0 mm (MVRCr 7729); paratype, ♀, 3.5 mm (MVRCr-7729).
Fig. 12. Leucothoe squalidens Ledoyer, 1984 in Red Sea Leucothoidae (Crustacea: Amphipoda) including new and re-described species
Fig. 12. Leucothoe squalidens Ledoyer, 1984, juv., length 1.6 mm (MVRCr 7732); ♂, length 2.0 mm (MVRCr 7733).
Fig. 3. A. Leucothoe acutilobata Ledoyer, 1978 in Red Sea Leucothoidae (Crustacea: Amphipoda) including new and re-described species
Fig. 3. A. Leucothoe acutilobata Ledoyer, 1978, ♀, length 6.0 mm. B. Leucothoe predenticulata Ledoyer, 1978, length 4.5 mm.
Fig. 10 in Red Sea Leucothoidae (Crustacea: Amphipoda) including new and re-described species
Fig. 10. Leucothoe reimeri sp. nov., holotype, ♂, length 5.9 mm (ZMB 29750, slide 5096); paratype, ♀, length 5.5 mm (ZMB 29751, slide 5097).
Fig. 5 in Red Sea Leucothoidae (Crustacea: Amphipoda) including new and re-described species
Fig. 5. Leucothoe bannwarthi (Schellenberg, 1928), ♂, length 3.0 mm (MCRCr 7726); ♀, length 3.0 mm (MVRCr 7725).
Fig. 4 in Red Sea Leucothoidae (Crustacea: Amphipoda) including new and re-described species
Fig. 4. Leucothoe bannwarthi (Schellenberg, 1928), ♂, length 3.0 mm (MCRCr 7726); ♀, length 3.0 mm (MVRCr 7725).
Data for [Changing abundance of magnetofossil morphologies in pelagic red clay around Minamitorishima, western North Pacific]
<p>----</p> <p>Note added in Aug 27, 2018.</p> <p>There is an error in the file sratios_MR15E01PC12.xlsx.</p> <p>Please refer to another upload, doi: 10.5281/zenodo.1404158.</p> <p>----</p> <p> </p> <p>This is the data used in the manuscript:</p> <p>Changing abundance of magnetofossil morphologies in pelagic red clay around Minamitorishima, western North Pacific</p>
Red Gelao (Shajing) audio word list
<p>On July 27, 2012 in Fengyan, Shajing Township, Qianxi County, Guizhou, China, I recorded the last remaining Red Gelao speaker of Shajing Township, Li Tingju 李庭举 (age 80). She was accompanied by her middle-aged daughter, Li Zhongying 李忠英. Both were illiterate and could not even read or write their own names. Li Tingju was not easy to work with, as she declined to repeat each word three times into my microphone and only wanted to say random words that would randomly come to her memory. She was not fluent in Gelao, and only knew possibly a few dozen to a few hundred vocabulary words, as well as a few songs. Altogether, I only obtained 3 songs and less than 20-30 vocabulary words from her.</p> <p> </p>
Stable isotopes and radiocarbon dating results on Late Pleistocene red deer and horse from the Serinyà caves (Girona, Catalonia, Spain)
<p>Table 1: Minimum (Min), maximum (Max), mean and standard-deviations (SD) of <em>δ</em><sup>13</sup>C<sub>carb</sub> and <em>δ</em><sup>18</sup>O<sub>carb</sub> values per horse and red deer tooth. Numbers in bold indicate isotopic values corresponding to peaks (summer) or troughs (winter) detected from clear sinusoidal patterns in <em>δ</em><sup>18</sup>O<sub>carb</sub> values. Numbers in bold correspond to minimum and maximum values in teeth revealing a sinusoidal pattern. LM3 and UM3 stand for lower third molar and upper third molar, respectively. LM2 stands for lower second molar. R is for the right side, L is for the left side. N: number of analyses.</p> <p>Table 2: Minimum, maximum, mean and standard-deviations of <em>δ</em><sup>13</sup>C<sub>coll</sub>, <em>δ</em><sup>15</sup>N<sub>coll</sub> for horse and red deer per technocomplex phases. na stands for not applicable. N: number of samples.</p> <p>Table A.1: Detailed isotopic results (<em>δ</em><sup>13</sup>C<sub>carb</sub> and <em>δ</em><sup>18</sup>O<sub>carb</sub>) for horse teeth with incremental sampling. Underlined numbers correspond to outlier data. Brackets are added around isotopic values that are not considered for further interpretation. R stands for the right side, L is for the left side.</p> <p>Table A.2: Detailed isotopic results (<em>δ</em><sup>13</sup>C<sub>carb</sub> and <em>δ</em><sup>18</sup>O<sub>carb</sub>) for red deer teeth with incremental sampling. Underlined numbers correspond to outlier data. Brackets are added around isotopic values that are not considered reliable for further interpretation. R is for the right side, L is for the left side.</p> <p>Table A.3: Results of elemental analysis on bone or dentine (N<sub>bone or dentine</sub>) and collagen (C<sub>coll</sub>, N<sub>coll</sub>, C:N<sub>coll</sub>) and of isotopic analysis on collagen (<em>δ</em><sup>13</sup>C<sub>coll</sub>, <em>δ</em><sup>15</sup>N<sub>coll</sub>) from horse (<em>Equus ferus</em>), red deer (<em>Cervus elaphus</em>) at the Serinyà caves. Underlined numbers correspond to outlier data. Brackets are added around isotopic values that are not considered reliable for further interpretation. R is for the right side, L is for the left side. * species determination confirmed by ZooMS analysis. Tüb. stands for Tübingen and NU for National University.</p> <p>Table A.4: Results of elemental analysis on bone or dentine (N<sub>bone or dentine</sub>) and collagen (C<sub>coll</sub>, N<sub>coll</sub>, C:N<sub>coll</sub>) and of isotopic analysis on collagen (<em>δ</em><sup>13</sup>C<sub>coll</sub>, <em>δ</em><sup>15</sup>N<sub>coll</sub>) from large bovids (<em>Bos/Bison</em>) and muskox (<em>Ovibos moschatus</em>) at the Serinyà caves. Underlined numbers correspond to outlier data. Brackets are added around isotopic values that are not considered reliable for further interpretation. R is for the right side, L is for the left side. * species determination confirmed by ZooMS analysis. Tüb. stands for Tübingen.</p> <p>Table A.5: Results of elemental analysis on collagen (C<sub>coll</sub>, N<sub>coll</sub>, C:N<sub>coll</sub>) and of isotopic analysis on collagen (<em>δ</em><sup>13</sup>C<sub>coll</sub>,<em>δ</em><sup>15</sup>N<sub>coll</sub>) and radiocarbon dates (<sup>14</sup>C) from horse (<em>Equus ferus</em>), red deer (<em>Cervus elaphus</em>), reindeer (<em>Rangifer tarandus</em>), muskox (<em>Ovibos moschatus</em>), rabbit (<em>Oryctolagus cuniculus</em>) and human (<em>Homo sapiens</em>) at the Serinyà caves. R is for the right side, L is for the left side. * species determination confirmed by ZooMS analysis. na stands for not applicable, nd for not determined and ind for indetermined.</p>
FIG. 1 in Microsatellite development in the freshwater red alga Batrachospermum gelatinosum (L.) De Candolle (Batrachospermales, Rhodophyta)
FIG. 1. — Images of Batrachospermum gelatinosum (L.) De Candolle: A, gametophytes fixed to a log at Cedar Bog in Ohio. Often this species has a brown to olive-green color; B, multiple gametophytes in a 55 cm diameter bowl;C, a single gametophyte mounted on herbarium paper. Photo credits: A, Stacy A. KruegerHadfield; B, C, Morgan L. Vis. Scale bars: A, 10 cm; B, 1.5 cm; C, 1 cm.
А – типовые местонахоЖдениЯ: Зал. ЛаврентиЯ (красный маркер), б. ПровидениЯ (Зеленый маркер); B, B' – иЗобраЖениЯ раковины (B) и Зуба радулы (B') Bela violacea var. nodulosa. Вр=14.5 мм, ДЗ=0.25 мм, иЗ: Krause [1885, pl. 18, figs. 4, 12]; C, C' – синтип Bela violacea var. nodulosa (C) и увеличенный участок предпоследнего оборота (C'), ZMB 37860, Вр=12 мм (фотографиЯ – с раЗрешениЯ ZMB); D–I – иЗменчивость Curtitoma violacea: D – Pleurotoma violacea var. brevis. ZIN беЗ номера, ЗФИ, о-в Аполлонова, Американский Залив, 3–4 м. Вр=8.2 мм; E – Defrancia becki. ZIN беЗ номера, ЗФИ, о-в Кука, 3–4 м. Вр=9.1 мм; F – Bela violacea var. laevior. Вр=12 мм, иЗ: Sars [1878, pl. 17, fig. 3]; G – Bela bicarinata var. geminolineata. ZIN 21324/28, Баренцево море, Югорский Шар, 13 м. Вр=8.7 мм; H – Pleurotoma bicarinata. ZIN 41203/156, ЗФИ, о-в ГрЭм-БЭм, 12–15 м. Вр=8.4 мм; I, I' – Зубы радулы типичной (I) и беЗкилевой (I') форм. ДЗ=0.12 мм и 0.21 мм, соответственно, иЗ: [Sars, 1878, pl. 9, figs. 7, 8]; J – иЗобраЖение раковины Lora inequita. Вр=11 мм, иЗ: Dall [1919, pl. 16, fig. 9]; K – голотип Lora inequita, USNM 222238. Вр=11 мм (фотографиЯ – с раЗрешениЯ USNM); L, L' – Oenopota inequita sensu Bogdanov non Dall: раковины (L) и Зуб радулы (L'). Вр=12 мм и 11.6 мм, соответственно, ДЗ=0.15 мм, иЗ: Богданов [1990, рис. 175, 176, 422 (7)]. A – type localities: Lawrence Bay (red circle), Providence Bay (green circle); B, B' – images of the shell (B) and tooth of the radula (B') of Bela violacea var. nodulosa. H=14.5 mm, L=0.25 mm, after Krause [1885, pl. 18, figs. 4, 12]; C, C' – a syntype of Bela violacea var. nodulosa (C) and the enlarged section of the penultimate whorl (C'), ZMB 37860, H=12 mm (photo – courtesy of ZMB); D–I – variability of Curtitoma violacea: D – Pleurotoma violacea var. brevis. ZIN uncatalogued, Franz Josef Land, Apollonova Isl., American Gulf, 3–4 m. H=8.2 mm; E – Defrancia becki. ZIN uncatalogued, Franz Josef Land, Cook Isl., 3–4 m. H=9.1 mm; F – Bela violacea var. laevior. H=12 mm, after Sars [1878, pl. 17, fig. 3]; G – Bela bicarinata var. geminolineata. ZIN 21324/28, Barents Sea, Ugra Shar, 13 m. H=8.7 mm; H – Pleurotoma bicarinata. ZIN 41203/156, Franz Josef Land, Graham-Bam Isl., 12–15 m. H= 8.4 mm; I, I' – teeth of typical (I) and keelless (I') forms. L=0.12 mm and 0.21 mm, respectively; after Sars [1878, pl. 9, figs. 7,8]; J – image of Lora inequita. H=11 mm, after Dall [1919, pl.16, fig. 9]; K – the holotype of Lora inequita, USNM 222238. H=11 mm (photo – courtesy of USNM); L, L' – Oenopota inequita sensu Bogdanov non Dall: shells (L) and tooth (L'). H=12 mm and 11.6 mm, respectively, L=0.15 mm, after Bogdanov [1990, figs. 175, 176, 422 (7)]. in Curtitoma nodulosa (Krause, 1885) comb. nov. (Gastropoda: Mangeliidae), a rare species twice described from the northern part of Bering Sea
А – типовые местонахоЖдениЯ: Зал. ЛаврентиЯ (красный маркер), б. ПровидениЯ (Зеленый маркер); B, B' – иЗобраЖениЯ раковины (B) и Зуба радулы (B') Bela violacea var. nodulosa. Вр=14.5 мм, ДЗ=0.25 мм, иЗ: Krause [1885, pl. 18, figs. 4, 12]; C, C' – синтип Bela violacea var. nodulosa (C) и увеличенный участок предпоследнего оборота (C'), ZMB 37860, Вр=12 мм (фотографиЯ – с раЗрешениЯ ZMB); D–I – иЗменчивость Curtitoma violacea: D – Pleurotoma violacea var. brevis. ZIN беЗ номера, ЗФИ, о-в Аполлонова, Американский Залив, 3–4 м. Вр=8.2 мм; E – Defrancia becki. ZIN беЗ номера, ЗФИ, о-в Кука, 3–4 м. Вр=9.1 мм; F – Bela violacea var. laevior. Вр=12 мм, иЗ: Sars [1878, pl. 17, fig. 3]; G – Bela bicarinata var. geminolineata. ZIN 21324/28, Баренцево море, Югорский Шар, 13 м. Вр=8.7 мм; H – Pleurotoma bicarinata. ZIN 41203/156, ЗФИ, о-в ГрЭм-БЭм, 12–15 м. Вр=8.4 мм; I, I' – Зубы радулы типичной (I) и беЗкилевой (I') форм. ДЗ=0.12 мм и 0.21 мм, соответственно, иЗ: [Sars, 1878, pl. 9, figs. 7, 8]; J – иЗобраЖение раковины Lora inequita. Вр=11 мм, иЗ: Dall [1919, pl. 16, fig. 9]; K – голотип Lora inequita, USNM 222238. Вр=11 мм (фотографиЯ – с раЗрешениЯ USNM); L, L' – Oenopota inequita sensu Bogdanov non Dall: раковины (L) и Зуб радулы (L'). Вр=12 мм и 11.6 мм, соответственно, ДЗ=0.15 мм, иЗ: Богданов [1990, рис. 175, 176, 422 (7)]. A – type localities: Lawrence Bay (red circle), Providence Bay (green circle); B, B' – images of the shell (B) and tooth of the radula (B') of Bela violacea var. nodulosa. H=14.5 mm, L=0.25 mm, after Krause [1885, pl. 18, figs. 4, 12]; C, C' – a syntype of Bela violacea var. nodulosa (C) and the enlarged section of the penultimate whorl (C'), ZMB 37860, H=12 mm (photo – courtesy of ZMB); D–I – variability of Curtitoma violacea: D – Pleurotoma violacea var. brevis. ZIN uncatalogued, Franz Josef Land, Apollonova Isl., American Gulf, 3–4 m. H=8.2 mm; E – Defrancia becki. ZIN uncatalogued, Franz Josef Land, Cook Isl., 3–4 m. H=9.1 mm; F – Bela violacea var. laevior. H=12 mm, after Sars [1878, pl. 17, fig. 3]; G – Bela bicarinata var. geminolineata. ZIN 21324/28, Barents Sea, Ugra Shar, 13 m. H=8.7 mm; H – Pleurotoma bicarinata. ZIN 41203/156, Franz Josef Land, Graham-Bam Isl., 12–15 m. H= 8.4 mm; I, I' – teeth of typical (I) and keelless (I') forms. L=0.12 mm and 0.21 mm, respectively; after Sars [1878, pl. 9, figs. 7,8]; J – image of Lora inequita. H=11 mm, after Dall [1919, pl.16, fig. 9]; K – the holotype of Lora inequita, USNM 222238. H=11 mm (photo – courtesy of USNM); L, L' – Oenopota inequita sensu Bogdanov non Dall: shells (L) and tooth (L'). H=12 mm and 11.6 mm, respectively, L=0.15 mm, after Bogdanov [1990, figs. 175, 176, 422 (7)].
Data from: A multifaceted ecological assessment reveals the invasion of the freshwater red macroalga Montagnia macrospora (Batrachospermales, Rhodophyta) in Taiwan
<p>Invasive freshwater macroalgae are rarely described. <em>Montagnia macrospora</em> is a freshwater red alga introduced from South America to East Asia via the global aquarium trade. The earliest occurrence record of this alga in Taiwan is dated 2005. To determine whether <em>M. macrospora </em>has become invasive in Taiwan and to understand the traits that facilitated its invasion, we took a multifaceted approach that combines examination of ecological background and population genetic analysis. Our island-wide survey showed that <em>M. macrospora</em> is widespread in the field across Taiwan, where the climate greatly differs from that of South America, and can self-sustain for nearly a decade. Our population genetic analysis revealed a lack of genetic diversity of <em>M. macrospora</em> in Taiwan, consistent with the hypothesis that the alga expanded through asexual reproduction. Moreover, during our long-term ecological assessments and field surveys, we observed that<em>M. macrospora</em> is an ecological generalist that can survive in a wide range of temperature, pH, illumination, and nutrient enrichment. Taken together, our data suggest that <em>M. macrospora</em> has successfully invaded the freshwater ecosystems ofTaiwan, likely due to its ability to disperse asexually and to grow under broad environmental conditions. We hope that our study brings attention to invasive freshwater algae, which have been overlooked in conservation planning and management.</p>
Figure 10 in Extensive vertebrate tracksite from the Upper Red Formation (middle-late Miocene), west Zanjan, northwestern Iran
Figure 10. Recent snake trails on creek sediments. Arrows show lateral pressures during the crawling of snakes (Abbassi, 2020). Length of hammer equals 30 cm.
Figure 8 in Extensive vertebrate tracksite from the Upper Red Formation (middle-late Miocene), west Zanjan, northwestern Iran
Figure 8. (a–b) Ichnospecies Iranipeda abeli trackway, preserved as convex hyporelief, and its sketch. Scale equals 10 cm and same for (a).
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