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333 results for “Kyrgyzstan”
Fifty years of firn evolution on Grigoriev ice cap, Tien Shan, Kyrgyzstan
<p><strong>README Grigoriev data</strong></p> <p><strong>Overview</strong></p> <p>The Grigoriev data collection consists of the following files, which are briefly explained further below.<br>From a relatively large number of files and for clarity, we provide mainly those files which have been directly<br>used in the generation of figures contained in Machguth et al. (2024). While the use in figure<br>creation was the main selection criteria, the files have not been truncated to data shown in the figures. <br>The files contain more information than shown in the figures. A few files have been added for completeness although<br>not used to create figures (see below).</p> <p>The data sets provided in this repository are listed in the following. Most of these tables contain relatively raw data. <br>The suggested citations are added in brackets. Please also check Table 1 in Machguth et al. (2024) for potential further references.</p> <p>- 1990_GRG_90_H1-BETA.xlsx (Arkhipov et al., 1996; Thompson et al., 1997)<br>- 1990_GRG_90_H1-CHM.xlsx (Arkhipov et al., 1996; Thompson et al., 1997)<br>- 1990_GRG_90_H1-STRAT.xlsx (Arkhipov et al., 1996; Thompson et al., 1997)<br>- 1990_GRG_90_H2-CHM.xlsx (Arkhipov et al., 1996; Thompson et al., 1997)<br>- 1990_GRG_90_H2-STRAT.xlsx (Arkhipov et al., 1996; Thompson et al., 1997)<br>- 1990_H1-H2_2018_Grigoriev_MI-decadal.xlsx (Arkhipov et al., 1996; Thompson et al., 1997; Machguth et al., 2024)<br>- 2001_GRG_01_S1-EE.xlsx (Arkhipov et al., 2004; Mikhalenko et al., 2005)<br>- 2001_metals.pdf (Usubaliev, 2003)<br>- 2003_GRG03-S1-EE_001.xlsx (Mikhalenko et al., 2005; Kutuzov, 2005)<br>- 2003_GRG03-S2-EE 001.xlsx (Mikhalenko et al., 2005; Kutuzov, 2005)<br>- 2003_pits.xlsx (Mikhalenko et al., 2005; Kutuzov, 2005)<br>- 2003_temperature_density.xlsx (Mikhalenko et al., 2005; Kutuzov, 2005)<br>- 2003_temperature_logger_data.xls (Mikhalenko et al., 2005; Kutuzov, 2005)<br>- 2018_density_stratigraphy_field_and_PSI_by_centimeter.xlsx (Machguth et al., 2024)<br>- 2018_PSI_dating_20230517.xlsx (Eichler et al., 2020; Machguth et al., 2024)</p> <p><br><strong>Detailed Information</strong></p> <p>1990_GRG_90_H1-BETA.xlsx: refers to Core 1 1990 (labelled H1 probably for "Hole 1"). Unknown to what the 1991 data refer, likely a repeat measurement.</p> <p>1990_GRG_90_H1-CHM.xlsx: Chemistry Core 1 1990.</p> <p>1990_GRG_90_H1-STRAT.xlsx: Stratigraphic information Core 1 1990</p> <p>1990_GRG_90_H2-CHM.xlsx: Chemistry Core 2 1990</p> <p>1990_GRG_90_H2-STRAT.xlsx: Stratigraphic information Core 2 1990</p> <p>1990_H1-H2_2018_Grigoriev_MI-decadal.xlsx: This table we calculated from the 1990 tables as well as the 2018 data for the purpose of visualizing<br> decadal means in MIs (Fig. 7). Decadal dating of the 1990 cores was done based on the bomb horizon of 1963 (Thompson et al., 1993, 1997), <br> decadal picks from Thompson et al. (1993) and personal communication by Lonnie Thompson (email 19 June 2023).</p> <p>2001_GRG_01_S1-EE.xlsx: 2001 core, stable water isotope ratios, firn temperatures, percentage of infiltration ice, stratigraphy</p> <p>2003_GRG03-S1-EE_001.xlsx: 2003 51m and 22.6m cores, 51m core was drilled thermally, 22.6m core mechanically. For the latter similar data as for 2001</p> <p>2003_GRG03-S2-EE 001.xlsx: 2003 21.3m core. Reduced amount of measured parameters compared to e.g. 2001 core. </p> <p>2003_pits.xlsx: Stratigraphy and density measured in a series of snow pits in 2003.</p> <p>2003_temperature_density.xlsx: Density and temperature measured in 2003 22.6m core. Comparison of T_ice at 4440 m a.s.l. to 1962 core (Dikikh, 1965)</p> <p>2003_temperature_logger_data.xls: Firn temperatures measured through a thermistor chain during 3 days in June 2003. Data from 14 June have been used for Fig. 5.</p> <p>2018_density_stratigraphy_field_and_PSI_by_centimeter.xlsx: 2018 core stratigraphy and density. This is a somwhat outdated file which shows the data per centimetre.<br> The file compares the two measurements of density (only the one from the laboratory was used in Machguth et al., 2024). <br> Also contains visually observed dust layers (not shown in Machguth et al., 2024)</p> <p>2018_PSI_dating_20230517.xlsx: Complete data from the analysis of the 2018 core.</p> <p><br><strong>Bibliography</strong></p> <p>Arkhipov, S. M., Mikhalenko, V. N., & Thompson, L. (1996). Struktura i stratigrafiya deyatel’nogo sloya lednika Grigor’eva na Tyan’-Shanye (Structure and stratigraphy of the active layer <br>of the Griroriev glacier in the Tjan-Shan). Materialy Glyatsiologicheskikh Issledovaniy (Data of Glaciological Studies), 80, 68–83.</p> <p>Arkhipov, S. M., Mikhalenko, V. N., Kunakhovich, M. G., Dikikh, A. N., and Nagornov, O. V.: Termicheskiy reshim, uslovija l’doobrazovanija i akkumulatsija na lednike Grigor’eva (Tyan’-<br>Shan), v 1962–2001 gg. (Thermal regime, types of ice formation and accumulation on the Grigoriev glacier (Tien Shan), 1962–2001), Materialy Glyatsiologicheskikh Issledovaniy (Data<br>of Glaciological Studies), 96, 77–83, 2004.</p> <p>Eichler, A., Kronenberg, M., Brütsch, S., Rüthi, M., Heule, M., Schwikowski, M., et al. (2020). Chernobyl horizon in a Central Asian ice core. <br>Annual Report 2019 - Laboratory of Environmental Chemistry - PSI, 31.</p> <p>Kutuzov, S. S.: Prostranstvennie izmenenija i stroenie lednikov vnutrennogo Tyan’-Shanya za poslednie 150 let (Spatial changes and structure of the glaciers of the inner Tien Shan over the last 150<br>years), Master’s thesis, Lomonossov State University, Moskva, 2005.</p> <p>Machguth, H., Eichler, A., Schwikowski, M., Brütsch, S., Mattea, E., Kutuzov, S., et al. (2024). Fifty years of firn evolution on Grigoriev ice cap, Tien Shan, Kyrgyzstan. <br>The Cryosphere, 18(4), 1633–1646. https://doi.org/10.5194/tc-18-1633-2024</p> <p>Mikhalenko, V. N., Kutuzov, S. S., Fayzrakhmanov, F. F., Nagornov, . B., Thompson, L. G., Kunakhovich, M. G., Arkhipov, S. M., Dikikh, A. N., and Usubaliev, R.: Sokrashhenie oledenenija<br>Tyan’-Shanja v XIX – nachale XXI vv.: rezul’taty kernovoro burenija i izmerenija temperatury v skvazhinakh (Glacier recession in the Tien Shan from the XIX to the beginning of the XXI century:<br>results from ice core drilling and borehole temperature measurements), Materialy Glyatsiologicheskikh Issledovaniy (Data of Glaciological Studies), 98, 175–182, 2005.</p> <p>Thompson, L. G., Mosley-Thompson, E., Davis, M., Lin, P. N., Yao, T., Dyurgerov, M., & Dal, J. (1993). “Recent warming” ice core evidence from tropical ice cores with emphasis <br>on Central Asia. Global Planet. Change, 7(1–3), 145–156. https://doi.org/10.1016/0921-8181(93)90046-Q</p> <p>Thompson, L. G., Mikhalenko, V., Mosley-Thompson, E., Durgerov, M., Lin, P. N., Moskalevsky, M., et al. (1997). Ice core records of recent climatic variability: Grigoriev and It-Tish ice caps <br>in Central Tien Shan, Central Asia. Materialy Glyatsiologicheskikh Issledovaniy (Data of Glaciological Studies), 81, 100–109.</p> <p>Usubaliev, R. A. (2003). Khimitcheskoe zagryaznenie lednikov Tyan’-Shanya (na primere lednika Grigor’eva) (Chemical pollution of Tien Shan glaciers (on the example of Grigoriev Glacier)). <br>Izvestija Natsional’noy Akademii Nauk Kirgizskoy Respubliki (News of the National Academy of Sciences of the Kyrgyz Republic), 4, 154–160.</p>
Small mammal survey in Narati (China) and Sary-Mogul (Kyrgyzstan)
<p>Field surveys were conducted in September 2006 at Narati (China) and September 2014 at Sary Mogul (Kyrgyzstan) using trapping and transect methods. See <a href="https://dataosu.obs-besancon.fr/FR-18008901306731-2015-08-06-20">dat@osu</a> for general metadata and Marston et al. (2022), cited below (submitted) for sampling details.</p> <p><a href="https://zenodo.org/record/7413284/files/Narati_transect.csv?download=1">Narati_transect.csv</a> : transects of over 41 km were surveyed in grassland areas between 1509-3335 m altitude. Each row corresponds to an approximatively 130 m segment, divided into 20 intervals of ten paces. Activity indicators identifiable to species or genus level (including foraging corridors, ground holes, earth tumuli and small mammal faeces) were recorded. The abundance index is the number of intervals where presence indicators were observed divided by the number of intervals walked (n = 20). The geographical coordinates are the centroïd of each segment.</p> <p><a href="https://zenodo.org/record/7413284/files/Narati_traplines.txt?download=1">Narati_traplines_rd.txt</a>: small mammal relative densities obtained using standard trapping as described in Marston et al. (2022).</p> <p><a href="https://zenodo.org/record/7413284/files/Sary_Mogul_transect.csv?download=1">Sary_Mogul_transect.csv</a>: For each transect, 20 intervals of 10 paces were surveyed with activity indicators identifiable to species or genus level (including foraging corridors, ground holes, earth tumuli and small mammal faeces) recorded. Relative density scores of small mammal presence (the number of intervals where presence indicators were observed) were produced for each species for each transect. In Sary Mogul, field surveys comprised 37 transects as described in <a href="https://doi.org/10.3390/rs11010039">Marston and Giraudoux (2019</a>)</p> <p><a href="https://zenodo.org/record/7413284/files/Sary_Mogul_traplines_rd.txt?download=1">Sary_Mogul_traplines_rd.txt</a>: small mammal relative densities obtained using standard trapping as described in Marston et al. (2022).</p>
Environmental proxy data from the Chap archaeological site (Kyrgyzstan)
<p>Sediment particle size, magnetic susceptibility, loss-on-ignition (LOI) and pollen data from the Chap archaeological site (described in Motuzaite Matuzeviciute et al. 2019, 2021, 2022).</p> <p>Particle size analysis using Malvern Mastersizer 2000 after treatment with HCl and H2O2.</p> <p>Particle size end members (EM 1 & 2) modelled using Analysize package (Paterson & Heslop 2015) for Matlab.</p> <p>Dimensionless magnetic susceptibility (Κ) readings were taken using a Bartington MS2B at low (0.46 kHz) and high (4.6 kHz) frequencies. Mass magnetic susceptibility (χ) was calculated by dividing Κ by sample bulk density. The percentage of frequency dependent components (χ­­<sub>fd%</sub>) was calculated as 100[(χ<sub>lf </sub>– χ<sub>hf</sub>)/χ<sub>lf</sub>].</p> <p>For LOI calculations, samples were weighed, fired at 550 degrees C for 4 hours, re-weighed then fired at 950 degrees C for 4 hours. </p> <p>Pollen was extracted following heavy liquid methods described in Leipe et al. (2019).</p> <p>Units in dataset:</p> <p>Centimetre (cm)</p> <p>Relative abundance (%)</p> <p>Absolute abundance (#)</p> <p>Sorting (σg) – after Folk & Ward (1957)</p> <p>Mass magnetic susceptibility (SI/g)</p>
National Checklists 2017: Kyrgyzstan Species List
Lists of taxa for each country and a few other administrative zones harvested from effechecka using simplified versions of geonames polygons. See <p></p>https://github.com/diatomsRcool/checklists for details<p></p>A list of species from Kyrgyzstan collected using effechecka and geonames polygons
National Checklists 2019: Kyrgyzstan Species List
Lists of taxa for each country and a few other administrative zones harvested from effechecka using simplified versions of geonames polygons. See <p></p>https://github.com/diatomsRcool/checklists for details.<p></p>A list of species from Kyrgyzstan collected using effechecka and geonames polygons
Figs 34-42 in A revision of Geostiba of the West Palaearctic region. XXVII. New species from Georgia and Kyrgyzstan, and additional records (Coleoptera, Staphylinidae, Aleocharinae)
Figs 34-42: Geostiba prominens (34-37) and G. dentata (38-42): (34, 38) male forebody in dorsal view; (35) male forebody in lateral view; (36-37, 41-42) median lobe of aedeagus in lateral and in ventral view; (39) head in lateral view; (40) male abdominal segments VI-VII. Scale bars: 34-35, 38-40: 0.5 mm; 36-37, 41-42: 0.1 mm.
Figure 9 in A checklist of the water mites of Central Asia with description of six new species (Acari, Hydrachnidia) from Kyrgyzstan
Figure 9 Atractides sonkulensisn. sp., female paratype: A – coxal field; B – genital field; C – palp, lateral view; D – palp, lateral view; E – I-L-5 and -6. Scale bars = 100 μm.
Figure 10 in A checklist of the water mites of Central Asia with description of six new species (Acari, Hydrachnidia) from Kyrgyzstan
Figure 10 Photographs of sampling sites: A – KR3, Ala Archa NP, spring outlet (locus typicusof Atractides alaarchaensis n. sp.); B – KR32, stream near Son Kul lake (locus typicusof Atractides sonkulensisn. sp.); C – KR10, spring in Grigorievka canyon (locus typicusof Atractides grigorievkan. sp.); D – KR8, Chon-Kemin NP, upper part of stream near Ashu resort (locus typicusof Torrenticola kyrgyzican. sp.); E – KR15, river on the road to May Saz Pass (locus typicusof Wandesia albertii n. sp.); F – KR22, stream in Karakal region (locus typicusof Atractides manasi n. sp.); G – KR23, rheohelocrenic spring in Karakal region (sampling site of Atractides grigorievkan. sp.); H – KR31, river near Son Kol Lake (sampling site of Atractides sonkulensisn. sp.).
Figure 8 in A checklist of the water mites of Central Asia with description of six new species (Acari, Hydrachnidia) from Kyrgyzstan
Figure 8 Atractides sonkulensisn. sp., male (A, C-F holotype, B paratype): A – idiosoma, ventral view; B – posterior margin of coxal shield; C – palp, lateral view; D – palp, medial view; E – genital field; F – I-L-5 and -6. Scale bars = 100 μm.
Figure 5 Atractides alaarchaensis n in A checklist of the water mites of Central Asia with description of six new species (Acari, Hydrachnidia) from Kyrgyzstan
Figure 5 Atractides alaarchaensis n. sp., male holotype: A – idiosoma, ventral view; B – I-L-5 and -6; C – palp, medial view; D – palp, lateral view; E – genital field. Scale bars = 100 μm.
Figure 2 in A checklist of the water mites of Central Asia with description of six new species (Acari, Hydrachnidia) from Kyrgyzstan
Figure 2 Torrenticola kyrgyzican. sp., female holotype: A – frontal margin of idiosoma, dorsal view; B – dorsal shield; C – ventral shield; D – palp, medial view; E – gnathosomal base and chelicera. Scale = 100 μm.
Figure 7 Atractides alaarchaensis n in A checklist of the water mites of Central Asia with description of six new species (Acari, Hydrachnidia) from Kyrgyzstan
Figure 7 Atractides alaarchaensis n. sp., deutonymph: A – I-L-5 and -6; B – palp, medial view; C – genital field. Scale bars = 100 μm.
Figure 6 Atractides alaarchaensis n in A checklist of the water mites of Central Asia with description of six new species (Acari, Hydrachnidia) from Kyrgyzstan
Figure 6 Atractides alaarchaensis n. sp., female paratype: A – coxal field; B – I-L-5 and -6; C – palp, lateral view; D – genital field. Scale bars = 100 μm.
Figure 4 Atractides manasi n in A checklist of the water mites of Central Asia with description of six new species (Acari, Hydrachnidia) from Kyrgyzstan
Figure 4 Atractides manasi n. sp., female holotype: A – idiosoma, dorsal view; B – idiosoma, ventral view; C – genital field; D – I-L-5 and -6; E – palp, medial view; F – palp, lateral view. Scale bars = 100 μm.
Figure 3 in A checklist of the water mites of Central Asia with description of six new species (Acari, Hydrachnidia) from Kyrgyzstan
Figure 3 Atractides grigorievkan. sp., female holotype: A – idiosoma, ventral view; B – genital field; C – palp, lateral view; D – palp, medial view; E – I-Leg; F – I-L-5 and -6; G – sword setae (S-1 and -2) at the ventrodistal margin of I-L-5. Scale bars = 100 μm.
Figure 1 Wandesia albertii n in A checklist of the water mites of Central Asia with description of six new species (Acari, Hydrachnidia) from Kyrgyzstan
Figure 1 Wandesia albertii n. sp., female holotype: A – coxal and genital field; B – palp, medial view; C – palp, lateral view; D – chelicere; E – acetabula (Ac-1-3, from left to right); F – I-Leg; G – II-Leg; H – III-Leg; I – IV-Leg. Scale = 100 μm.
Figs 2–6 in A New Species Of The Genus Paradryomyza Ozerov (Diptera: Dryomyzidae) From Kyrgyzstan
Figs 2–6. Paradryomyza kirgizica sp. n., holotype (2, 4–6) and P. setosa (Bigot, 1886) (3). 2 – mid femur, posteroventrally; 3, 4 – antenna; 5 – postabdomen, lateral view; 6 – same, ventral view.
Fig. 11 in Two new outstanding species of the genus Hedychridium Abeille from Kyrgyzstan (Hymenoptera: Chrysididae)
Fig. 11. Hedychridium planifrons du Buysson (United Arab Emirates), habitus of female, dorsal view. Scale bar: 1.0 mm.
Figs 1–4 in Two new outstanding species of the genus Hedychridium Abeille from Kyrgyzstan (Hymenoptera: Chrysididae)
Figs 1–4. Hedychrid- ium karakolense sp. nov., holotype, fe- male (Kyrgyzstan): 1, habitus, dorsal view; 2, habitus, lateral view; 3, head, dorsal view; 4, metasoma, dorsolateral view. Scale bar: 1.0 mm.
Figs 7–10 in Two new outstanding species of the genus Hedychridium Abeille from Kyrgyzstan (Hymenoptera: Chrysididae)
Figs 7–10. Hedychridium tarbinskyi sp. nov., holotype, female (Kyrgyzstan): 7, habitus, dorsal view; 8, habitus, lateral view; 9, metasoma, dorsolateral view; 10, head, dorsal view. Scale bar: 1.0 mm.
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