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  • 1
    ISSN: 0948-1907
    Keywords: Chemistry ; Polymer and Materials Science
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Additional Material: 3 Ill.
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1022-1336
    Keywords: Chemistry ; Polymer and Materials Science
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Physics
    Notes: We compared the cross-polymerization of diacetylene units, incorporated in different ways into polyamide (PA) matrices: as fragments of the PA main chains (PA1) and as pendant groups of the PA main chains (PA2). At room temperature the reaction proceeds only in PA1 via 1,4-addition (cross-links I). However at high temperature besides of cross-links I another type of cross-links (cross-links II) is formed, presumably via 1,2-addition reaction. In PA2 only cross-links of type II are formed at high temperatures.
    Additional Material: 2 Ill.
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1434-1948
    Keywords: Cyclophanes ; σ-Bonded silyl-, germyl-, stannyl derivatives ; Grignard reactions ; Chemistry ; General Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Notes: Symmetrically 4,16-disubstituted (3a-c) and bridged (6a, b) organometallic paracyclophane derivatives have been synthesized for use as monomeric precursors of organometallic poly-p-xylylenes. Both types of compounds were obtained by lithiation of the appropriately substituted paracyclophane bromides (1 or 4) and subsequent quenching of the resulting lithioparacyclophane derivatives with organometallic electrophiles. For the synthesis of 4,16-bis(trimethylsilyl)[2.2]paracyclophane (3a) we also examined the Grignard reaction, and as a result the first successful use of a 4,16-bis Grignard reagent is described. According to the spectral data, the bridged compounds 6a, c are formed as diastereomeric mixtures of a meso- and a d,l form. The diastereomers were separated by fractional recrystallization and characterized.
    Additional Material: 1 Ill.
    Type of Medium: Electronic Resource
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  • 4
    ISSN: 1022-1352
    Keywords: Chemistry ; Polymer and Materials Science
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Physics
    Notes: Block copolymers of unsubstituted poly(p-xylylene)(PPX) and Ge- or Sn-organic bridged PPX (GePPX and SnPPX) were prepared by pyrolysis of specially synthesized organometallic p-cyclophane precursors followed by deposition and polymerization of the thus produced p-xylylene monomers. The copolymer structure and thermal behavior were investigated depending on deposition temperature (10 and -196°C). The copolymer PPX-GePPX obtained from solid monomers deposited at -196°C (2a) consists of long quasi-independent PPX and GePPX blocks and has paracrystalline structure. Thermal treatment of 2a near 160°C yields crystalline regions of PPX along with paracrystalline aggregates of GePPX. Pyrolysis of this system near 300°C in an inert atmosphere results in the formation of Ge crystals in PPX matrix. In contrast, the copolymer PPX-GePPX produced by simultaneous deposition and polymerization at 10°C (2a′) contains shorter blocks of PPX and GePPX than the copolymer deposited at -196°C. Copolymer 2a′ turns to the amorphous state during thermal treatment, and its pyrolysis does not lead to Ge-crystal formation; hence the supramolecular structure of the polymer plays an important role in inorganic phase formation. The copolymer PPX-SnPPX (2b) is formed only at a deposition temperature of -196°C; deposition at 10°C yields oligomeric resins. The structure of 2b is nearly the same as that of 2a; pyrolysis of 2b in air results in SnO2-crystal formation in a PPX matrix.
    Additional Material: 3 Ill.
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  • 5
    Publication Date: 2024-01-04
    Keywords: Eurasian Arctic seas; File content; File format; File name; File size; Grain-size distributions; sediment; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 10 data points
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  • 6
    Publication Date: 2024-01-04
    Description: Within the Russian-German collaborative research project The Changing Arctic Transpolar System (CATS; see www.transdrift.info), benthic species distributions have been modelled across large geographic scales in Eurasian Arctic seas. As surficial seafloor sediment grain size is one important explanatory variable used in these modelling studies, we compiled open-access information from 23 data sets on this environmental parameter, pooling validated grain-size data from a total of 2,134 sampling sites distributed across the Barents, Kara, Laptev and East Siberian Seas, as well as some abyssal regions of the central Arctic Ocean. As grain-size distributions are differently scaled in western European and Russian sources, all data were uniformly transformed to the Udden-Wentworth scale using the "approximation" function in R prior to further processing and archiving. For this, a linear interpolation was utilized to split the 50-100 µm grain-size fraction used in Russian data sets into the silt (≤ 63 µm) and sand (〉 63 µm) fraction of the Udden-Wentworth scale. Using the kriging R package "automap", interpolated maps were created showing the geographic distribution of the percentages (%) of fine (silt and clay: ≤ 63 µm) and coarse (〉 63 µm to 2 mm) grain-size fractions in surface seafloor sediments. These maps were first created in the Sea Ice Polar Stereographic North CRS projection, followed by a transformation to the standard WGS84 CRS projection.
    Keywords: Eurasian Arctic seas; Grain-size distributions; sediment
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 7
    Publication Date: 2024-02-02
    Keywords: 104-1; 109-1; 111-2; 114-1; 117-1; 120-1; 121-1; 122-2; 287-2; 57-04; 57-06; 57-07; 57-08; 57-09; 57-11; 57-12; 57-13; 57-14; 57-20; 58-08; 61-1; 76-2; Akademik Boris Petrov; Akademik Ioffe; Akademik Sergey Vavilov; Amundsen Basin; Arctic; Arctic Ocean; ARK-I/3; ARK-II/4; ARK-II/5; ARK-III/3; ARK-IV/3; ARK-V/2; ARK-VIII/2; ARK-VIII/3; ARK-XI/1; ASV13; ASV13_1088-G; ASV13_1092-G; ASV13_1093-G; ASV13_1094-G; ASV13_1112-G; ASV13_1117-G; ASV13_1118-G; ASV13_1119-G; ASV13_1123-G; ASV13_1124-G; ASV13_1125-G; ASV13_1126-G; ASV13_1127-G; ASV13_1128-G; ASV13_1129-G; ASV13_1130; ASV13_1137-G; ASV13_1150-G; ASV13_1151-G; ASV13_1157-G; Barents Sea; BC; Box corer; BP00; BP00-02/02; BP00-02/03; BP00-05/04; BP00-07/08; BP00-08/03; BP00-09/03; BP00-13/03; BP00-14/02; BP00-15/03; BP00-15/04; BP00-16/03; BP00-17/02; BP00-17/03; BP00-19/01; BP00-22/03; BP00-26/03; BP00-28/01; BP00-29/02; BP00-29/03; BP00-30/01; BP00-31/01; BP00-35/03; BP00-36/08; BP00-38/01; BP01; BP01-01/07; BP01-03/02; BP01-07/01; BP01-08/01; BP01-11/03; BP01-14/01; BP01-16/01; BP01-21/01; BP01-23/01; BP01-24/01; BP01-25/01; BP01-28/05; BP01-28/06; BP01-29/01; BP01-30/05; BP01-31/05; BP01-32/01; BP01-33/01; BP01-34/05; BP01-34/06; BP01-36/01; BP01-37/05; BP01-38/01; BP01-41/05; BP01-41/06; BP01-43/06; BP01-45/05; BP01-47/01; BP01-47/02; BP01-48/05; BP01-48/06; BP01-51/04; BP01-55/04; BP01-56/05; BP01-57/01; BP01-58/04; BP01-60/01; BP01-61b/05; BP01-61b/06; BP01-63/01; BP01-64/04; BP01-64/05; BP01-65/04; BP01-66/04; BP01-67/01; BP01-68/04; BP01-70/05; BP01-72a/02; BP01-73/04; BP01-73a/01; BP01-74/01; BP01-75/01; BP01-76/01; BP01-77/01; BP01-78/01; BP01-79/01; BP01-80/05; BP01-82/01; BP01-83/01; BP97; BP97-10; BP97-12; BP97-17; BP97-19; BP97-21; BP97-27; BP97-32; BP97-35; BP97-39; BP97-42; BP97-43; BP97-46; BP97-47; BP97-48; BP97-49; BP97-50; BP97-52; BP97-55; BP97-56; BP97-58; BP99; BP99-01/04; BP99-02/05; BP99-03/05; BP99-04/05; BP99-05/01; BP99-08/05; BP99-11/05; BP99-12/05; BP99-13/05; BP99-17/05; BP99-18/06; BP99-19/05; BP99-24/05; BP99-24/06; BP99-25/05; BP99-25/06; BP99-28/05; BP99-29/05; BP99-30/06; BP99-31/06; BP99-32/06; BP99-38/05; BP99-39/05; CTD/Rosette; CTD-RO; DEPTH, sediment/rock; DIVERSE; Don-1959-10; Don-1959-11; Don-1959-12; Don-1959-13; Don-1959-2; Don-1959-20; Don-1959-23; Don-1959-39; Don-1959-4; Don-1959-40; Don-1959-41; Don-1959-42; Don-1959-43; Don-1959-44; Don-1959-45; Don-1959-46; Don-1959-47; Don-1959-48; Don-1959-49; Don-1959-5; Don-1959-51; Don-1959-52; Don-1959-53; Don-1959-54; Don-1959-55; Don-1959-56; Don-1959-58; Don-1959-59; Don-1959-6; Don-1959-60; Don-1959-63; Don-1959-64; Don-1959-65; Don-1959-66; Don-1959-67; Don-1959-68; Don-1959-69; Don-1959-8; Don-1959-9; D-S-1959-2; D-S-1959-4; D-S-1959-5; D-S-1959-6; East Siberian Sea; Elevation of event; Eurasian Arctic seas; Event label; Exp-1953-1; Exp-1953-106; Exp-1953-107; Exp-1953-108; Exp-1953-112; Exp-1953-118; Exp-1953-119; Exp-1953-121; Exp-1953-129; Exp-1953-13; Exp-1953-130; Exp-1953-131; Exp-1953-134; Exp-1953-135; Exp-1953-137; Exp-1953-15; Exp-1953-160; Exp-1953-161; Exp-1953-162; Exp-1953-17; Exp-1953-179; Exp-1953-182; Exp-1953-183; Exp-1953-186; Exp-1953-187; Exp-1953-19; Exp-1953-195; Exp-1953-197; Exp-1953-198; Exp-1953-199; Exp-1953-2; Exp-1953-200; Exp-1953-201; Exp-1953-202; Exp-1953-22; Exp-1953-23; Exp-1953-27; Exp-1953-36; Exp-1953-37; Exp-1953-4; Exp-1953-40; Exp-1953-41; Exp-1953-42; Exp-1953-43; Exp-1953-44; Exp-1953-45; Exp-1953-46; Exp-1953-47; Exp-1953-48; Exp-1953-49; Exp-1953-5; Exp-1953-50; Exp-1953-52; Exp-1953-53; Exp-1953-54; Exp-1953-55; Exp-1953-6; Exp-1953-8; Exp-1953-9; Exp-1953-90; Exp-1953-91; Exp-1953-92; Exp-1953-94; Exp-1953-95; Exp-1953-96; Exp-1953-97; Exp-1953-98; Exp-1954-1; Exp-1954-10; Exp-1954-100; Exp-1954-103; Exp-1954-105; Exp-1954-106; Exp-1954-107; Exp-1954-114; Exp-1954-115; Exp-1954-116; Exp-1954-117; Exp-1954-118; Exp-1954-119; Exp-1954-12; Exp-1954-120; Exp-1954-122; Exp-1954-124; Exp-1954-128; Exp-1954-129; Exp-1954-132; Exp-1954-133; Exp-1954-134; Exp-1954-135; Exp-1954-136; Exp-1954-138; Exp-1954-139; Exp-1954-14; Exp-1954-141; Exp-1954-145; Exp-1954-146; Exp-1954-147; Exp-1954-15; Exp-1954-155; Exp-1954-157; Exp-1954-16; Exp-1954-164; Exp-1954-165; Exp-1954-166; Exp-1954-167; Exp-1954-17; Exp-1954-182; Exp-1954-185; Exp-1954-20; Exp-1954-203; Exp-1954-204; Exp-1954-206; Exp-1954-207; Exp-1954-208; Exp-1954-21; Exp-1954-210; Exp-1954-211; Exp-1954-212; Exp-1954-22; Exp-1954-229; Exp-1954-23; Exp-1954-232; Exp-1954-236; Exp-1954-237; Exp-1954-25; Exp-1954-26; Exp-1954-29; Exp-1954-30; Exp-1954-31; Exp-1954-33; Exp-1954-34; Exp-1954-35; Exp-1954-36; Exp-1954-37; Exp-1954-41; Exp-1954-42; Exp-1954-43; Exp-1954-44; Exp-1954-46; Exp-1954-47; Exp-1954-48; Exp-1954-49; Exp-1954-50; Exp-1954-51; Exp-1954-56; Exp-1954-59; Exp-1954-61; Exp-1954-68; Exp-1954-69; Exp-1954-76; Exp-1954-78; Exp-1954-80; Exp-1954-81; Exp-1954-82; Exp-1954-84; Exp-1954-85; Exp-1954-86; Exp-1954-89; Exp-1954-91; Exp-1954-92; Exp-1954-93; Exp-1954-99; Exp-1955-10; Exp-1955-104; Exp-1955-105; Exp-1955-106; Exp-1955-108; Exp-1955-11; Exp-1955-122; Exp-1955-123; Exp-1955-124; Exp-1955-125; Exp-1955-127; Exp-1955-128; Exp-1955-129; Exp-1955-13; Exp-1955-130; Exp-1955-131; Exp-1955-132; Exp-1955-133; Exp-1955-134; Exp-1955-135; Exp-1955-136; Exp-1955-137; Exp-1955-139; Exp-1955-14; Exp-1955-143; Exp-1955-144; Exp-1955-145; Exp-1955-146; Exp-1955-147; Exp-1955-148; Exp-1955-149; Exp-1955-151; Exp-1955-152; Exp-1955-153; Exp-1955-154; Exp-1955-155; Exp-1955-156; Exp-1955-157; Exp-1955-158; Exp-1955-159; Exp-1955-16; Exp-1955-160; Exp-1955-161; Exp-1955-164; Exp-1955-165; Exp-1955-166; Exp-1955-167; Exp-1955-17; Exp-1955-18; Exp-1955-19; Exp-1955-196; Exp-1955-197; Exp-1955-198; Exp-1955-199; Exp-1955-2; Exp-1955-20; Exp-1955-201; Exp-1955-202; Exp-1955-204; Exp-1955-205; Exp-1955-206; Exp-1955-207; Exp-1955-21; Exp-1955-214; Exp-1955-22; Exp-1955-24; Exp-1955-25; Exp-1955-3; Exp-1955-36; Exp-1955-37; Exp-1955-39; Exp-1955-4; Exp-1955-41; Exp-1955-42; Exp-1955-43; Exp-1955-44; Exp-1955-45; Exp-1955-47; Exp-1955-5; Exp-1955-51; Exp-1955-52; Exp-1955-53; Exp-1955-54; Exp-1955-55; Exp-1955-56; Exp-1955-58; Exp-1955-59; Exp-1955-6; Exp-1955-60; Exp-1955-62; Exp-1955-65; Exp-1955-66; Exp-1955-67; Exp-1955-7; Exp-1955-72; Exp-1955-73; Exp-1955-74; Exp-1955-76; Exp-1955-8; Exp-1955-9; Exp-1955-90; Exp-1955-93; Exp-1955-94; Exp-1955-95; Exp-1956-11; Exp-1956-12; Exp-1956-2; Exp-1956-22; Exp-1956-23; Exp-1956-27; Exp-1956-29; Exp-1956-3; Exp-1956-30; Exp-1956-47; Exp-1956-48; Exp-1956-49; Exp-1956-50; Exp-1956-51; Exp-1956-52; Exp-1956-6; Exp-1956-8; Exp-1956-9; Exp-1959-12/1; Exp-1959-14/2; Exp-1959-15/3; Exp-1959-16/4; Exp-1959-179/16; Exp-1959-183/17; Exp-1959-199/18; Exp-1959-202/19; Exp-1959-214/20; Exp-1959-215/21; Exp-1959-225/22; Exp-1959-226/23; Exp-1959-229/24; Exp-1959-230/25; Exp-1959-231/26; Exp-1959-232/27; Exp-1959-234/28; Exp-1959-235/29; Exp-1959-236/30; Exp-1959-237/31; Exp-1959-238/32; Exp-1959-240/33; Exp-1959-241/34; Exp-1959-242/35; Exp-1959-251/36; Exp-1959-252/37; Exp-1959-253/38; Exp-1959-254/39; Exp-1959-256/40; Exp-1959-26/8; Exp-1959-265/41; Exp-1959-265/42; Exp-1959-27/9; Exp-1959-28/10; Exp-1959-29/11; Exp-1959-32/13; Exp-1959-33/14; Exp-1959-34/15; Exp-1960-10; Exp-1960-109; Exp-1960-110; Exp-1960-111; Exp-1960-113; Exp-1960-118; Exp-1960-119; Exp-1960-122; Exp-1960-125; Exp-1960-126; Exp-1960-131; Exp-1960-138; Exp-1960-139; Exp-1960-142; Exp-1960-152; Exp-1960-159; Exp-1960-17; Exp-1960-18; Exp-1960-21; Exp-1960-23; Exp-1960-24; Exp-1960-26; Exp-1960-28; Exp-1960-32; Exp-1960-35; Exp-1960-36; Exp-1960-37; Exp-1960-48; Exp-1960-50; Exp-1960-67; Exp-1960-81; Exp-1960-9; Exp-1960-91; Exp-1960-95; Exp-1961-101/25; Exp-1961-102/26; Exp-1961-103/27; Exp-1961-104/28; Exp-1961-105/29; Exp-1961-110/30; Exp-1961-111/31; Exp-1961-112/32; Exp-1961-115/33; Exp-1961-120/35; Exp-1961-123/36; Exp-1961-124/37; Exp-1961-19/2; Exp-1961-21/3; Exp-1961-23/4; Exp-1961-26/5; Exp-1961-28/6; Exp-1961-
    Type: Dataset
    Format: text/tab-separated-values, 4266 data points
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  • 8
    Publication Date: 2018-06-11
    Description: The p2b domain of Rous sarcoma virus (RSV) Gag and the p6 domain of HIV-1 Gag contain late assembly (L) domains that engage the ESCRT membrane fission machinery and are essential for virus release. We now show that the PPXY-type RSV L domain specifically recruits the BAR domain protein PACSIN2 into virus-like particles (VLP), in addition to the NEDD4-like ubiquitin ligase ITCH and ESCRT pathway components such as TSG101. PACSIN2, which has been implicated in the remodeling of cellular membranes and the actin cytoskeleton, is also recruited by HIV-1 p6 independent of its ability to engage the ESCRT factors TSG101 or ALIX. Moreover, PACSIN2 is robustly recruited by NEDD4-2s, a NEDD4-like ubiquitin ligase capable of rescuing HIV-1 budding defects. The NEDD4-2s–induced incorporation of PACSIN2 into VLP correlated with the formation of Gag-ubiquitin conjugates, indicating that PACSIN2 binds ubiquitin. Although PACSIN2 was not required for a single cycle of HIV-1 replication after infection with cell-free virus, HIV-1 spreading was nevertheless severely impaired in T cell lines and primary human peripheral blood mononuclear cells depleted of PACSIN2. HIV-1 spreading could be restored by reintroduction of wild-type PACSIN2, but not of a SH3 domain mutant unable to interact with the actin polymerization regulators WASP and N-WASP. Overall, our observations indicate that PACSIN2 promotes the cell-to-cell spreading of HIV-1 by connecting Gag to the actin cytoskeleton.
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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  • 9
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