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  • 1980-1984  (1,015,988)
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  • 1
    Monograph available for loan
    Monograph available for loan
    Novosibirsk : Izdatel'stvo "Nauka", Sibirskoe otdelenie
    Associated volumes
    Call number: ZSP-801-482
    In: Trudy Instituta Geologii i Geofiziki, Vypusk 482
    Description / Table of Contents: Translation of abstract: The book examines issues of biostratigraphy and paleontology of the Devonian and Carboniferous of the West Siberian Lowland and its mountain frame. New data on Devonian biostratigraphy of the Tomsk region (from wells), Gorny Altai, and the eastern slope of the Urals are presented; Devonian foraminifera of the Tomsk region, Gorny Altai and the eastern slope of the Urals, stromatoporates of the Tomsk region and conodonts of the Altai Mountains and Salair are described. On the Carboniferous, new data are provided on the stratigraphy of the Zaisan region and the Ekibastuz basin. The publication is intended for a wide range of geologists and paleontologists.
    Description / Table of Contents: В книге рассматриваются вопросы биостратиграфии и палеонтологии девона и карбона Западно-Сибирской низменности и ее горного обрамления. Приводятся новые данные пo биостратиграфии девона Томской области (по скважинам), Горному Алтаю, восточному склону Урала; описаны девонские фораминиферы Томской области, Горного Алтая и восточного склона Урала, строматопораты Томской области и конодонты Горного Алтая и Салаира. По карбону приводятся новые данные по стратиграфии Призайсанья и Экибастузского бассейна. Издание рассчитано на широкий кpyг геологов и палеонтологов.
    Type of Medium: Monograph available for loan
    Pages: 143 Seiten , Illustrationen
    Series Statement: Trudy Instituta Geologii i Geofiziki Vypusk 482
    Language: Russian
    Note: Translation of Table of Contents On the composition and age of Paleozoic sediments from the Luginetskaya 170 well (Tomsk region) / O. I. Bogush, V. I. Bidzhakov, V. N. Dubatolov, V. M. Zadorozhny, N. M. Zaslavskaya, G. D. Isaev, V. L. Klishevich, V. I. Krasnov, T. A. Moskalenko, L. S. Ratanov, M. V. Stepanova, V. G. Khromykh, L. I. Sheshegova, O. V. Yuferev Devonian foraminiferal complexes of the Pudinsky megaswell (Tomsk region) / O. V. Yuferev, O. I. Bogush, V. M. Zadorozhny, V. I. Krasnov, L. S. Ratanov, G. D. Isaev New genus of Devonian foraminifera / V. I. Chuvashov, O. V. Yuferev New Devonian foraminifera from the family Parathuramminidae / V. M. Zadorozhny, O. V. Yuferev Stromatoporates and their distribution in sediments penetrated by the Luginetskaya 170 well / V. G. Khromykh Devon region of Cheremshanki (Altai Mountains) / L. M. Aksenova, O. I. Bogush, Yu. A. Dubatolova, V. N. Dubatolov, V. M. Zadorozhny, E. N. Polenova, A. A. Puzyrev, N. Ya. Spassky, O. V. Yuferev Polygonograptidae familia nova (systematics, stratigraphic and geographical distribution) / A. M. Obut, N. V. Sennikov Foraminifera of the Middle Devonian of the eastern slope of the Urals / L. G. Petrova Limestones of the Koltubai Formation of the Southern Urals / B. I. Chuvashov, O. V. Yuferev The importance of foraminifera for the identification of Frasnian deposits in the oil-bearing Paleozoic of the southeastern part of the Western Siberian Plate / V. M. Zadorozhny On non-marine bivalves of the Ekibastuz basin / G. G. Aksenova, O. A. Betekhtina, M. Ya. Tokareva On the issue of systematics of paraturammin / V. M. Zadorozhny, O. V. Yuferev Photo tables and explanations for them , СОДЕРЛЖАНИЕ О составе и возрасте отложений палеозоя скважины Лугинецкая 170 (Томская область) / О. И. Богуш, В. И. Биджаков, В. Н . Дубатолов, В. М. Задорожный, Н. М. Заславская, Г. Д. Исаев, В. Л. Клишевич, В. И. Краснов, Т. А. Москаленко, Л. С. Ратанов , М. В. Степанова, В. Г. Хромых, Л. И. Шешегова , О. В. Юферев Комплексы девонских фораминифер Пудинского мегавала (Томская область) / О. В. Юферев, О. И. Богуш, В. М. Задорожный, В. И. Краснов, Л. С. Ратанов, Г. Д. Исаев Новый род девонских фораминифер / В. И. Чувашов, О. В. Юферев Новые девонские фораминиферы из семейства Parathuramminidae / В. М. Задорожный, О. В. Юферев Строматопораты и их распределение в отложениях, вскрытых скважиной Лугинецкая 170 / В. Г. Хромых Девон района Черемшанки (Горный Алтай) / Л. М. Аксенова, О. И. Богуш, Ю. А. Дубатолова, В. Н. Дубатолов, В. М. Задорожный, Е. Н. Поленова, А. А. Пузырев, Н. Я. Спасский, О. В. Юферев Polygonograptidae familia nova (систематика, стратиграфическое и географическое распространение) / А. М. Обут, Н. В. Сенников Фораминиферы среднего девона восточного склона Урала / Л. Г. Петрова Известняки колтубаиской свиты Южного Урала / Б. И. Чувашов, О. В. Юферев Значение фораминифер для выделения франских отложений в нефтеносном палеозое юго-восточной части 3ападно-Сибирской плиты / В. М. Задорожный О неморских двустворках Экибастузского бассейна / Г. Г. Аксенова, О. А. Бетехтина, М. Я. Токарева К вопросу о систематике паратураммин / В. М. Задорожный, О. В. Юферев Фототаблицы и объяснения к ним , In kyrillischer Schrift
    Location: AWI Archive
    Branch Library: AWI Library
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  • 2
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    PANGAEA
    In:  Supplement to: Bada, Jeffrey L; Man, Eugene H (1980): Amino acid diagenesis in Deep Sea Drilling Project cores: Kinetics and mechanisms of some reactions and their applications in geochronology and in paleotemperature and heat flow determinations. Earth-Science Reviews, 16(1), 21-55, https://doi.org/10.1016/0012-8252(80)90003-3
    Publication Date: 2024-05-15
    Description: Several amino acid diagenetic reactions, which take place in the deep-sea sedimentary environment, were investigated, using various Deep Sea Drilling Project (DSDP) cores. Initially it was found that essentially all the amino acids in sediments are bound in peptide linkages; but, with increasing age, the peptide bonds undergo slow hydrolysis that results in an increasingly larger fraction of amino acids in the free state. The hydrolysis half-life in calcareous sediments was estimated to be ~1–2 million years, while in non-carbonate sediment the hydrolysis rate may be considerably slower. The amino acid compositions and the extent of racemization of several amino acids were determined in various fractions isolated from the sediments. These analyses demonstrated that the mechanism, kinetics, and rate of amino acid diagenesis are highly dependent upon the physical state (i.e., free, bound, etc.) in which the amino acids exist in the sedimentary environment. In the free state, serine and threonine were found to decompose primarily by a dehydration reaction, while in the bound state (residue or HCl-insoluble fraction) a reversible aldol-cleavage reaction is the main decomposition pathway of these amino acids. The change in amino acid composition of the residue fraction with time was suggested to be due to the hydrolysis of peptide bonds, while in foraminiferal tests the compositional changes over geological time are the result of various decomposition reactions. Reversible first-order racemization kinetics are not observed for free amino acids in sediments. The explanation for these anomalous kinetics involves a complex reaction series which includes the hydrolysis of peptide bonds and the very rapid racemization of free amino acids. The racemization rates of free amino acids in sediments were found to be many orders of magnitude faster than those predicted from elevated temperature experiments using free amino acids in aqueous solution. The racemization rate enhancement of free amino acids in sediments may be due to the catalysis of the reaction by trace metals. Reversible first-order kinetics are followed for amino acids in the residue fraction isolated from sediments; the rate of racemization in this fraction is slower than that predicted for protein-bound amino acids. Various applications of amino acid diagenetic reactions are discussed. Racemization and the decomposition reaction of serine and threonine can both be used, with certain limitations, to make rough age estimates of deep-sea sediments back to several million years. The extent of racemization in foraminiferal tests which have been dated by some other independent technique can be used to estimate geothermal gradients, and thus heat flows, and to evaluate the bottom water temperature history in certain oceanic areas.
    Keywords: 15-148; 15-149; 25-241; 25-242; 25-249; 27-262; 37-332; 37-332A; 37-333; Caribbean Sea/BASIN; Caribbean Sea/RIDGE; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Indian Ocean//BASIN; Indian Ocean//CHANNEL; Indian Ocean//RIDGE; Indian Ocean//TROUGH; Leg15; Leg25; Leg27; Leg37; North Atlantic/VALLEY
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 3
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    PANGAEA
    In:  P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow | Supplement to: AK43 Team (1990): Biological and Geological Bottom Investigations in the South Atlantic. P.P. Shirshov Institute of Oceanology, USSR Academy of Sciences, Transactions, vol. 126. Nauka Publ. (Moscow); Vinogradova, N.G. (Ed.), 208 pp
    Publication Date: 2024-05-15
    Description: The book is devoted to investigations of benthic fauna and geology of the Southern Atlantic Ocean. These works have been carried out in terms of exploring biological structure of the ocean and are of great importance for development of this fundamental problem. They are based on material collected during Cruise 43 of R/V Akademik Kurchatov in 1985-1986 and Cruise 43 of R/V Dmitry Mendeleev in 1989. Problems of quantitative distribution, group composition and trophic structure of benthos in the Southern Scotia Sea, along the east-west Transatlantic section along 31°30'S, and offshore Namibia in the area of the Benguela upwelling are under consideration in the book. Authors present new data on fauna of several groups of deep-sea bottom animals and their zoogeography. Much attention is paid to analysis of morphological structure of the Scotia Sea floor considered in terms of plate tectonics. Bottom sediments along the Transatlantic section and facial variation of sediments in the area of South Shetland Islands and of the continental margin of Namibia are under consideration.
    Keywords: 37-332A; 37-332B; 37-333A; 37-335; 38-344; 45-396B; 49-407; 49-410A; 49-413; AK43-4834; AK43-4877; AK43-4878; AK43-4879; AK43-4880; AK43-4881; AK43-4882; AK43-4887; AK43-4889; AK43-4890; AK43-4891; AK43-4893; AK43-4896; AK43-4898; AK43-4899; AK43-4900; AK43-4901; AK43-4902; AK43-4903; AK43-4904; AK43-4905; AK43-4906; AK43-4907; AK43-4910; AK43-4912; AK43-4923; AK43-4925; AK43-4926; AK43-4927; AK43-4928; AK43-4929; AK43-4931; AK43-4932GR; AK43-4933; AK43-4934; AK43-4935; AK43-4936; AK43-4938; AK43-4939; AK43-4940; AK43-4943; AK43-4944GR; AK43-4945; AK43-4946; AK43-4947; AK43-4948; AK43-4948GR; AK43-4949; AK43-4952; AK43-4955; AK43-4956; Akademik Kurchatov; AKU43; Angola Basin; Archive of Ocean Data; ARCOD; Argentinian Basin; Cape Basin; DRILL; Drilling/drill rig; GC; Glomar Challenger; Grab; GRAB; Gravity corer; Leg37; Leg38; Leg45; Leg49; MULT; Multiple investigations; North Atlantic; North Atlantic/FRACTURE ZONE; North Atlantic/Greenland Sea/RIDGE; North Atlantic/RIDGE; North Atlantic/SEDIMENT POND; North Atlantic/VALLEY; OKEAN; Okean Grab; Rio Grande Rise; South Atlantic Ridge
    Type: Dataset
    Format: application/zip, 13 datasets
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  • 4
    Publication Date: 2024-05-15
    Keywords: AWI_Glac; BER01S90_01; Berkner Island (Reinwarthhöhe); Calculated from mass/volume; Density, mass density; Depth, bottom/max; DEPTH, ice/snow; Depth, top/min; Filchner-Ronne-Ice-Shelf-Project; FRISP 1992; Glaciology @ AWI; Isotope ratio mass spectrometry; Sampling/drilling ice; SNOWPIT; Snow pit; SSBerkN North-dome; δ18O, water
    Type: Dataset
    Format: text/tab-separated-values, 160 data points
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  • 5
    Publication Date: 2024-05-15
    Keywords: 47KA; AGE; Calculated, see reference(s); Calculated from mass/volume; Carbon, organic, total; Cibicides wuellerstorfi, δ13C; Cibicides wuellerstorfi, δ18O; Density, dry bulk; DEPTH, sediment/rock; East Pacific; Element analyser CHN, LECO; GEOMETEP III; GIK/IfG; Globoquadrina dutertrei, δ13C; Globoquadrina dutertrei, δ18O; Institute for Geosciences, Christian Albrechts University, Kiel; KAL15; Kasten corer 15 cm; Mass spectrometer Finnigan MAT 251; Sedimentation rate; SO26; SO26_47KA; Sonne
    Type: Dataset
    Format: text/tab-separated-values, 242 data points
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  • 6
    Publication Date: 2024-05-15
    Keywords: AK43-4834; AK43-4893; AK43-4896; AK43-4898; AK43-4899; AK43-4900; AK43-4901; AK43-4902; AK43-4903; AK43-4904; AK43-4905; AK43-4906; AK43-4907; AK43-4910; AK43-4912; Akademik Kurchatov; AKU43; Aluminium oxide; Angola Basin; Archive of Ocean Data; ARCOD; Argentinian Basin; Atomic absorption spectrometry (AAS); Cadmium; Calcium carbonate; Calculated from mass/volume; Cape Basin; Carbon, organic, total; Chromium; Cobalt; Copper; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Elevation of event; Event label; GC; Grab; GRAB; Gravity corer; Ion selective probe; Iron; Latitude of event; Lead; Lithium; Longitude of event; Manganese; Nickel; Oxidation reduction (RedOx) potential; Rio Grande Rise; Silicon dioxide; South Atlantic Ridge; Strontium; Sulfur, total; Titanium dioxide; Vanadium; Water content, wet mass; Wet chemistry; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 308 data points
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  • 7
    Publication Date: 2024-05-15
    Keywords: AGE; Age, standard deviation; BC; Biogeochemical Ocean Flux Study; BOFS; BOFS11889#4; BOFS9C; Box corer; Calcium carbonate; Calculated from mass/volume; Coulometrics Carbon Analyzer; D184; Density, dry bulk; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Discovery (1962); JGOFS; Joint Global Ocean Flux Study; Northeast Atlantic; Thorium; Thorium, standard deviation; Thorium/Uranium ratio; Thorium/Uranium ratio, standard deviation; Thorium-230; Thorium-230, standard deviation; Thorium-230/Thorium-232 activity ratio; Thorium-230/Thorium-232 activity ratio, standard deviation; Thorium-230 excess; Thorium-230 excess, standard deviation; Uranium; Uranium, standard deviation; Uranium-234; Uranium-234, standard deviation; Uranium-234/Uranium-238 activity ratio; Uranium-234/Uranium-238 activity ratio, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 231 data points
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  • 8
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    Publication Date: 2024-05-15
    Keywords: 108-658; Accumulation rate, clay 〈 2 µm; Accumulation rate, siliciclastics; Accumulation rate, silt 〉 6 µm; AGE; Calculated, see reference(s); Calculated from mass/volume; Canarias Sea; COMPCORE; Composite Core; Density, dry bulk; Depth, composite; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Intercore correlation; Joides Resolution; Leg108; Mode, grain size; Ocean Drilling Program; ODP; Sample code/label; Siliciclastics; Size fraction 〈 0.002 mm, clay; Size fraction 〉 0.006 mm, silt; Water content, wet mass; X-ray diffraction TEXTUR, clay fraction
    Type: Dataset
    Format: text/tab-separated-values, 5451 data points
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  • 9
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    PANGAEA
    Publication Date: 2024-05-15
    Keywords: 108-659; Accumulation rate, clay 〈 2 µm; Accumulation rate, siliciclastics; Accumulation rate, silt 〉 6 µm; AGE; Calcium carbonate; Calculated, see reference(s); Calculated from mass/volume; COMPCORE; Composite Core; Density, dry bulk; Depth, composite; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Element analyser CHN, LECO; Grain size, SEDIGRAPH 5000; Intercore correlation; Joides Resolution; Leg108; Mode, grain size; Ocean Drilling Program; ODP; Sample code/label; Siliciclastics; Size fraction 〈 0.002 mm, clay; Size fraction 〉 0.006 mm, silt; South Atlantic Ocean; X-ray diffraction TEXTUR, clay fraction
    Type: Dataset
    Format: text/tab-separated-values, 7935 data points
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  • 10
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    PANGAEA
    Publication Date: 2024-05-15
    Keywords: 108-661A; Accumulation rate, calcium carbonate; Accumulation rate, siliciclastics; AGE; Calcium carbonate; Calculated, see reference(s); Calculated from mass/volume; Density, dry bulk; Depth, composite; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Element analyser CHN, LECO; Grain size, SEDIGRAPH 5000; Intercore correlation; Joides Resolution; Leg108; Ocean Drilling Program; ODP; Sample code/label; Siliciclastics; South Atlantic Ocean
    Type: Dataset
    Format: text/tab-separated-values, 665 data points
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