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  • 1
    Electronic Resource
    Electronic Resource
    Weinheim : Wiley-Blackwell
    Zeitschrift für anorganische Chemie 535 (1986), S. 63-85 
    ISSN: 0044-2313
    Keywords: Chemistry ; Inorganic Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Description / Table of Contents: Formation of Cyclic Silylphosphanes. Reaction of Li-Phosphides with R2SiCl2 (R—Me, Et, t-Bu)The reaction of Me2SiCl2 with Li-phosphides (mixture of LiPH2, Li2PH) leads to the formation of Me2Si(PH2)Cl 1, Me2Si(PH2)2 2, H2P—SiMe2—PH—SiMe2Cl 3, (H2P—SiMe2)2PH 4, (HP—SiMe2)3 6, 5, 7, 8, 9, 10, 40. Excess of phosphides in Et2O - as well as excess of LiPH2 - favourably forms 10. Li2PH (virtually free of Li3P and LiPH2) is obtained by reaction of LiPH2 · DME with LiBu; Li3P by reaction of PH3 with LiBu in toluene. Isomerization by Li/H migration determines the course of reaction of the PH-bearing compounds with Li-phosphides. With Me2SiCl2 Li3P mainly generates compound 10.The reaction of the Li-phosphides with Et2SiCl2 mainly leads to (HP—SiEt2)3 18 and (HP—SiEt2)2 17 as well as to Et2Si(PH2)Cl 11, Et2Si(PH2)2 12, (ClEt2Si)2PH 13, H2P—SiEt2—PH—SiEt2Cl 14, (H2P—SiEt2)2PH 15 and 16. In the reaction with LiPH2 · DME the same compounds are obtained and isomerization by Li/H migration (formation of PH3) already begins at -70°C. In toluene ClEt2Si—P(SiEt2)2P—SiEt2Cl is additionally formed. Derivatives of 9, 10, 40 are not observed.The reaction of (t-Bu)2SiCl2 with LiPH2 leads to HP[Si(t-Bu)2]2PH 20 (yield 76%) and formation of PH3, the reaction with Li2PH to 20 (54%) besides HP[Si(t-Bu)2]2PLi 21.
    Notes: Die Umsetzung von Me2SiCl2 mit Li-Phosphiden (Gemisch aus LiPH2, Li2PH) führt zur Bildung der Verbindungen Me2Si(PH2)Cl 1, Me2Si(PH2)2 2, H2P—SiMe2—PH—SiMe2Cl 3, (H2P—SiMe2)2PH 4, (HP—SiMe2)3 6, 5, 7, 8, 9, 10, 40. Die Bildung von 10 wird durch einen Phosphidüberschuß in Et2O - auch an LiPH2 - begünstigt. Li2PH (weitgehend frei von Li3P und LiPH2) wird aus LiPH2 · DME und LiBu erhalten; Li3P aus PH3 und LiBu in Toluol. Ummetallierungsprozesse der PH-haltigen Verbindungen mit Li-Phosphiden bestimmen den Reaktionsablauf. Li3P bildet mit Me2SiCl2 bevorzugt Verbindung 10.Die Umsetzung der Li-Phosphide mit Et2SiCl2 führt bevorzugt zu (HP—SiEt2)3 18 und (HP—SiEt2)2 17 sowie zu Et2Si(PH2)Cl 11, Et2Si(PH2)2 12, (ClEt2Si)2PH 13, H2P—SiEt2—PH—SiEt2Cl 14, (H2P—SiEt2)2PH 15 und 16. Bei der Umsetzung mit LiPH2 · DME bilden sich die gleichen Verbindungen, und die Ummetallierung (PH3-Entwicklung) beginnt bereits bei -70°C. In Toluol entsteht zusätzlich ClEt2Si—P[SiEt2]2P—SiEt2Cl. Derivate von 9, 10, 40 werden nicht gebildet.Die Umsetzung von (t-Bu)2SiCl2 mit LiPH2 führt zu HP[Si(t-Bu)2]2PH 20 (Ausbeute 76%) unter PH3-Entwicklung, die von Li2PH zu 20 (54%) neben HP[Si(t-Bu)2]2PLi 21.
    Additional Material: 3 Tab.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Weinheim : Wiley-Blackwell
    Zeitschrift für anorganische Chemie 535 (1986), S. 95-105 
    ISSN: 0044-2313
    Keywords: Chemistry ; Inorganic Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Description / Table of Contents: Investigations on Lithiation and Substitution of HP[Si(t-Bu)2]2PHHP[Si(t-Bu)2]2PH 1 is monolithiated by reaction with LiPH2 · DME or LiBu in toluene. The crystalline compound HP[Si(t-Bu)2]2PLi · 2 DME 2 can be isolated in DME. Reaction of 2 with Me2SiCl2 leads to HP[Si(t-Bu)2]2P—SiMe2Cl 4, ClMe2Si—P[Si(t-Bu)2]2P—SiMe2Cl 5, HP[Si(t-Bu)2]2P—SiMe2—P[Si(t-Bu)2] 2PH 6. Isomerization by Li/H migration between 4 and 2 leads to the formation of 5. Reaction of Li(t-Bu) with 1 or 2 yields LiP[Si(t-Bu)2]2PLi 3 by further lithiation. 3 could not be obtained purely, only in a mixture with 2. These compounds favourably generate with t-BuPCl2 in hexane Cl(t-Bu)P—P[Si(t-Bu)2]2P—P(t-Bu)Cl 9, in THF HP[Si(t-Bu)2]2P—P(t-Bu)—P[Si(t-Bu)2]2 PH 12 (main product), 9, H(t-Bu)P—P[Si(t-Bu)2]2P—P(t-Bu)Cl 10, H(t-Bu)P—P[Si(t-Bu)2]2P—P(t-Bu)H 11 as well as HP[Si(t-Bu)2]2P—P(t-Bu)H 13 and HP[Si(t-Bu)2]2P—P(t-Bu)2 14.
    Notes: HP[Si(t-Bu)2]2PH 1 wird mit LiPH2 · DME oder LiBu in Toluol monolithiiert. Aus DME ist die kristalline Verbindung HP[Si(t-Bu)2]2PLi · 2 DME 2 zu isolieren. Durch Umsetzung von 2 mit Me2SiCl2 bilden sich HP[Si(t-Bu)2]2P—SiMe2Cl 4, ClMe2Si—P[Si(t-Bu)2]2P—SiMe2Cl 5, HP[Si(t-Bu)2]2P—SiMe2—P[Si(t-Bu)2] 2PH 6. Die Bildung von 5 aus 2 ist auf die Umlithiierung zwischen 4 und 2 zurückzuführen. Durch Einwirkung von Li(t-Bu) auf 1 bzw. 2 erfolgt eine weitere Lithiierung zum LiP[Si(t-Bu)2]2PLi 3. 3 war jedoch nicht rein, sondern nur im Gemische mit 2 zu erhalten. Diese bilden mit t-BuPCl2 in Hexan bevorzugt Cl(t-Bu)P—P[Si(t-Bu)2]2P—P(t-Bu)Cl 9, in THF HP[Si(t-Bu)2]2P—P(t-Bu)—P[Si(t-Bu)2]2 PH 12 (Hauptprodukt), 9, H(t-Bu)P—P[Si(t-Bu)2]2P—P(t-Bu)Cl 10, H(t-Bu)P—P[Si(t-Bu)2]2P—P(t-Bu)H 11 sowie HP[Si(t-Bu)2]2P—P(t-Bu)H 13 und HP[Si(t-Bu)2]2P—P(t-Bu)2 14.
    Additional Material: 2 Tab.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Weinheim : Wiley-Blackwell
    Zeitschrift für die chemische Industrie 53 (1940), S. 327-331 
    ISSN: 0044-8249
    Keywords: Chemistry ; General Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Additional Material: 3 Ill.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Weinheim : Wiley-Blackwell
    Zeitschrift für anorganische Chemie 535 (1986), S. 86-94 
    ISSN: 0044-2313
    Keywords: Chemistry ; Inorganic Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Description / Table of Contents: 1,3,5,7-Tetraphospha-2,4,6,8,9-decamethyl-2,4,6,8,9-pentasila-bicyclo (3.3.1)-nonan. Structure and ReactionsThe structure of the title compound 1 (white quad-shaped crystals, mp. 193°C) obtained by reaction of Li2PH with Me2SiCl2, is identified by 31PNMR and mass spectra as well as X-ray structure analysis. Compound 1 crystallizes in the monoclinic space group C2/c (No. 15) with a = 1563.6(28) pm, b = 1166.7(9) pm, c = 2556.0(27) pm, = 87.07(12)° and Z = 8 formula units in the elementary cell. The molecule has approximately mm (C2v) symmetry. The boat-boat conformation characterizes 1 as direct precursor of the dodecamethyl-hexasila-tetraphospha-adamantane. The bond lengths and bond angles are normal with d̄(P—Si) = 224.5 pm and d̄(Si—Me) = 186.0 pm. The H bonded to P are directed exocyclic.1 reacts with (CO)4CrNBD (NBD = Norbornadiene) (bidentate ligand) to (SiMe2)5P2(PH)2Cr(CO)4 2 while closing the structure of compound 1 to the adamantane structure via the inserted Cr(CO)4.
    Notes: Die Struktur der durch Umsetzung von Li2PH mit Me2SiCl2 gebildeten Titelverbindungen 1 (weiße, quaderförmige Kristalle, Smp. 193°C) wird durch 31P-NMR- und massenspektrometrische Untersuchung sowie durch die Röntgenstrukturanalyse ermittelt. 1 kristallisiert monoklin in der Raumgruppe C2/c (Nr. 15) mit a = 1563,6(28) pm, b = 1166,7(9) pm, c = 2556,0(27) pm, β 87,07(12%) und Z = 8 Molekülen in der Elementarzelle. Das Molekül besitzt angenähert die Symmetrie mm (C2v), liegt in der Boot-Boot-Konformation vor und ist damit die direkte Vorstufe zum Dodekamethyl-hexasila-tetraphosphaadamantan. Bindungsabstände und Bindungswinkel mit den Mittelwerten d̄(P—Si) = 224,5 pm und d̄(Si—Me) = 186,0 pm sind normal. Die an P gebundenen Protonen zeigen ringauswärts.1 reagiert mit (CO)4CrNBD (NBD = Norbornadien) (zweizähniger Ligand) zum (SiMe2)5P2(PH)2Cr(CO)4 2, in dem die Struktur von Verbindung 1 über das eingebaute Cr(CO)4 zur Adamantanstruktur geschlossen wird.
    Additional Material: 2 Ill.
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  • 5
    Publication Date: 2023-11-14
    Description: Agulhas leakage, the warm and salty inflow of Indian Ocean water into the Atlantic Ocean, is of importance for the climate-relevant Atlantic Meridional Overturning Circulation. South of Africa, the eastward turning Agulhas Current sheds Agulhas rings, cyclones and filaments of order 100 km that carry the Indian Ocean water into the Cape Basin and further into the Atlantic. Here, we show that the resolution of submesoscale flows of order 10 km in an ocean model leads to 40 % more Agulhas leakage and more realistic Cape Basin water-masses compared to a parallel non-submesoscale resolving simulation. Moreover, we show that submesoscale flows strengthen shear-edge eddies and in consequence lee cyclones at the northern edge of the Agulhas Current, as well as the leakage pathway in the region of the filaments that takes place outside of mesoscale eddies. This indicates that the increase in leakage can be attributed to stronger Agulhas filaments, when submesoscale flows are resolved.
    Description: Leakage of warm, salty waters from the Indian Ocean into the Atlantic increases by up to 40 % in high-resolution numerical ocean model simulations, suggesting that low-resolution models underestimate this key part of the global meridional overturning circulation.
    Description: Agence Nationale de la Recherche (French National Research Agency) https://doi.org/10.13039/501100001665
    Description: https://hdl.handle.net/20.500.12085/c572cde8-a82c-4c2d-9bd7-288dfc8f1939
    Description: https://www.aoml.noaa.gov/phod/gdp/data.php
    Description: https://resources.marine.copernicus.eu/?option=com_csw&view=details&product_id=GLOBAL_REANALYSIS_PHY_001_030
    Description: https://resources.marine.copernicus.eu/?option=com_csw&view=details&product_id=SEALEVEL_GLO_PHY_L4_REP_OBSERVATIONS_008_047
    Keywords: ddc:551.46 ; Climate and Earth system modelling ; Physical oceanography
    Language: English
    Type: doc-type:article
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  • 6
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    Unknown
    PANGAEA
    In:  Supplement to: Steinle, Lea; Graves, Carolyn; Treude, Tina; Ferre, Benedicte; Biastoch, Arne; Bussmann, Ingeborg; Berndt, Christian; Krastel, Sebastian; James, Rachael H; Behrens, Erik; Böning, Claus W; Greinert, Jens; Sapart, Célia-Julia; Scheinert, Markus; Sommer, Stefan; Lehmann, Moritz F; Niemann, Helge (2015): Water column methanotrophy controlled by a rapid oceanographic switch. Nature Geoscience, 8(5), 378–382, https://doi.org/10.1038/ngeo2420
    Publication Date: 2023-03-03
    Description: Large amounts of the greenhouse gas methane are released from the seabed to the water column where it may be consumed by aerobic methanotrophic bacteria. This microbial filter is consequently the last marine sink for methane before its liberation to the atmosphere. The size and activity of methanotrophic communities, which determine the capacity of the water column methane filter, are thought to be mainly controlled by nutrient and redox dynamics, but little is known about the effects of ocean currents. Here, we report measurements of methanotrophic activity and biomass (CARD-FISH) at methane seeps west of Svalbard, and related them to physical water mass properties (CTD) and modelled current dynamics. We show that cold bottom water containing a large number of aerobic methanotrophs was rapidly displaced by warmer water with a considerably smaller methanotrophic community. This water mass exchange, caused by short-term variations of the West Spitsbergen Current, constitutes a rapid oceanographic switch severely reducing methanotrophic activity in the water column. Strong and fluctuating currents are widespread oceanographic features common at many methane seep systems and are thus likely to globally affect methane oxidation in the ocean water column.
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 7
    Publication Date: 2023-03-25
    Description: Connectivity is a fundamental process driving the persistence of marine populations and their adaptation potential in response to environmental change. In this study, we analysed the population genetics of two morphologically highly similar deep-sea sponge clades (Phakellia hirondellei and the 'Topsentia-and-Petromica (TaP)' clade) at three locations in the Cantabrian Sea. Sponge taxonomy was assessed by spicule analyses, as well as by 18S sequencing and COI sequencing. The corresponding host microbiome was analysed by 16S rRNA gene sequencing. In addition we set up an oceanographic modelling framework, for which we used seawater flow cytometry data (derived from bottom depths of CTD casts) as ground-truthing data.
    Keywords: Accession number, genetics; amplicon sequencing; Angeles Alvarino; Area/locality; Bacteria; Bay of Biscay; CTD/Rosette; CTD1; CTD10; CTD11; CTD12; CTD13; CTD14; CTD15; CTD2; CTD3; CTD4; CTD5; CTD6; CTD7; CTD8; CTD9; CTD-RO; Date/Time of event; Deep-sea Sponge Grounds Ecosystems of the North Atlantic; DEPTH, water; DR10; DR15; DR4; DR7; DR9; Dredge, rock; DRG_R; Event label; flow cytometry; Flow cytometry; Geology, comment; Latitude of event; Longitude of event; Measurement conducted; Method/Device of event; Phytoplankton; population genetics; Porifera; Sample code/label; Sample ID; single-nucleotide polymorphisms (SNPs); SponGES; SponGES_0617; SPONGES_0617_04-DR4; SPONGES_0617_07-CTD1; SPONGES_0617_12-CTD2; SPONGES_0617_13-CTD3; SPONGES_0617_15-DR7; SPONGES_0617_18-CTD4; SPONGES_0617_19-CTD5; SPONGES_0617_23-DR9; SPONGES_0617_24-CTD6; SPONGES_0617_27-CTD7; SPONGES_0617_28-DR10; SPONGES_0617_29-CTD8; SPONGES_0617_40-CTD9; SPONGES_0617_42-CTD10; SPONGES_0617_46-CTD11; SPONGES_0617_49-CTD12; SPONGES_0617_55-CTD13; SPONGES_0617_58-CTD14; SPONGES_0617_60-DR15; SPONGES_0617_61-CTD15
    Type: Dataset
    Format: text/tab-separated-values, 550 data points
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  • 8
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Scott, Rebecca; Biastoch, Arne; Agamboue, Pierre D; Bayer, Till; Boussamba, Francois L; Formia, Angela; Godley, Brendan J; Mabert, Brice D K; Manfoumbi, Jean C; Schwarzkopf, Franziska; Sounguet, Guy-Philippe; Wagner, Patrick; Witt, Matthew J (2017): Spatio-temporal variation in ocean current-driven hatchling dispersion: Implications for the world's largest leatherback sea turtle nesting region. Diversity and Distributions, https://doi.org/10.1111/ddi.12554
    Publication Date: 2023-10-28
    Description: This data set describes the location of virtual floats representing turtle hatchlings throughout 60 modeled years. Floats were constrained to remain within depths of 0-6 m due to the positive buoyancy of hatchlings. Floats were first assigned to one of 20,000 random release locations within a large release area 125-400 km offshore from nesting beaches throughout the Republic/Democratic Republic of the Congo, Gabon and Equatorial Guinea spanning latitudes of c. 6°S to 3.5°N. For each month over the 4-month long hatching season (January-April), each of the 20,000 floats was assigned a random release day and drift simulations ran every year during the period 1960-2007 resulting in drift trajectories of approx. 4 million virtual floats. See Scott et al., 2017, Spatio-temporal variation in ocean current-driven hatchling dispersion: Implications for the world's largest leatherback sea turtle nesting region. Diversity Distrib, http://dx.doi.org/10.1111%2Fddi.12554 for details as to the model parameters. Each data set consists of data on the float ID (number 1,2,3 etc..) and its trajectory attributes (latitude/longitude) at each time step. Data are also provided on the temperature, salinity and density of the float at its respective position/time step. Data sets are sorted by float release date, and contain one data file for each year. Each data file has 11 columns, which contain the following data: float id, longitude, latitude, depth, time step, temperature, salinity, density, no time steps since start, distance to start point, bearing from start point
    Keywords: Climate - Biogeochemistry Interactions in the Tropical Ocean; File content; File format; File name; File size; Model; Sea-turtle_model; SFB754; Uniform resource locator/link to model result file
    Type: Dataset
    Format: text/tab-separated-values, 60 data points
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  • 9
    Publication Date: 2024-02-27
    Keywords: 0; 1; 10; 100; 101; 102; 103; 104; 105; 106; 107; 108; 109; 11; 110; 111; 112; 113; 114; 115; 116; 117; 118; 119; 12; 120; 121; 122; 123; 124; 125; 126; 127; 128; 13; 14; 15; 16; 17; 18; 19; 2; 20; 21; 22; 23; 24; 25; 26; 27; 28; 29; 3; 30; 31; 32; 33; 34; 35; 36; 37; 38; 39; 4; 40; 41; 42; 43; 44; 45; 46; 47; 48; 49; 5; 50; 51; 52; 53; 54; 55; 56; 57; 58; 59; 6; 60; 61; 62; 63; 64; 65; 66; 67; 68; 69; 7; 70; 71; 72; 73; 74; 75; 76; 77; 78; 79; 8; 80; 81; 82; 83; 84; 85; 86; 87; 88; 89; 9; 90; 91; 92; 93; 94; 95; 96; 97; 98; 99; Calculated; CTD, Sea-Bird SBE 911plus; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; Latitude of event; Longitude of event; Maria S. Merian; MSM38; MSM38_343; MSM38_344; MSM38_345; MSM38_347; MSM38_348; MSM38_349; MSM38_350; MSM38_354; MSM38_355; MSM38_358; MSM38_359; MSM38_360; MSM38_361; MSM38_363; MSM38_364; MSM38_365; MSM38_366; MSM38_367; MSM38_368; MSM38_369; MSM38_370; MSM38_372; MSM38_373; MSM38_374; MSM38_375; MSM38_376; MSM38_377; MSM38_378; MSM38_379; MSM38_380; MSM38_381; MSM38_382; MSM38_383; MSM38_384; MSM38_385; MSM38_386; MSM38_387; MSM38_388; MSM38_389; MSM38_390; MSM38_391; MSM38_392; MSM38_393; MSM38_394; MSM38_395; MSM38_396; MSM38_397; MSM38_398; MSM38_399; MSM38_400; MSM38_401; MSM38_402; MSM38_403; MSM38_404; MSM38_405; MSM38_406; MSM38_407; MSM38_408; MSM38_409; MSM38_410; MSM38_411; MSM38_412; MSM38_413; MSM38_414; MSM38_415; MSM38_417; MSM38_418; MSM38_419; MSM38_420; MSM38_421; MSM38_422; MSM38_423; MSM38_424; MSM38_425; MSM38_426; MSM38_427; MSM38_428; MSM38_429; MSM38_430; MSM38_431; MSM38_432; MSM38_433; MSM38_434; MSM38_435; MSM38_436; MSM38_437; MSM38_438; MSM38_439; MSM38_440; MSM38_441; MSM38_442; MSM38_443; MSM38_444; MSM38_445; MSM38_446; MSM38_447; MSM38_448; MSM38_449; MSM38_450; MSM38_451; MSM38_452; MSM38_453; MSM38_454; MSM38_455; MSM38_456; MSM38_457; MSM38_458; MSM38_459; MSM38_460; MSM38_461; MSM38_462; MSM38_463; MSM38_464; MSM38_465; MSM38_466; MSM38_467; MSM38_468; MSM38_469; MSM38_470; MSM38_471; MSM38_472; MSM38_473; MSM38_474; MSM38_475; MSM38_476; MSM38_477; MSM38_478; MSM38_479; MSM38_480; Oxygen; Oxygen sensor, SBE 43; Pressure, water; Salinity; Temperature, water; Temperature, water, potential
    Type: Dataset
    Format: text/tab-separated-values, 2181198 data points
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  • 10
    Publication Date: 2024-02-02
    Keywords: Campaign of event; CTD/Rosette; CTD-RO; Date/Time of event; Depth, bottom/max; DEPTH, water; Event label; Latitude of event; Longitude of event; Maria S. Merian; MSM21/4; MSM21/4_546-2; MSM21/4_550-1; MSM21/4_551-1; MSM21/4_552-1; MSM21/4_553-1; MSM21/4_554-1; MSM21/4_555-1; MSM21/4_556-1; MSM21/4_557-1; MSM21/4_558-1; MSM21/4_559-1; MSM21/4_580-1; MSM21/4_581-1; MSM21/4_582-1; MSM21/4_583-1; MSM21/4_584-1; MSM21/4_613-1; MSM21/4_633-1; MSM21/4_634-1; MSM21/4_635-1; MSM21/4_636-1; MSM21/4_637-1; MSM21/4_638-1; MSM21/4_639-1; MSM21/4_640-1; MSM21/4_641-1; MSM21/4_642-1; MSM21/4_654-1; MSM21/4_655-1; North Greenland Sea; Salinity; Sample code/label; Temperature, water; Type
    Type: Dataset
    Format: text/tab-separated-values, 55415 data points
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