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  • 1990-1994  (36)
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  • 1
    Keywords: Earth sciences,++history ; Earth sciences++History ; Aufsatzsammlung ; Konferenzschrift ; Erde ; Entwicklung ; Sedimentation ; Tektonik
    Type of Medium: Book
    Pages: XXII, 490 S. , graph. Darst.
    ISBN: 0125103409
    DDC: 550.09
    RVK:
    Language: English
    Note: Literaturangaben
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  • 2
    ISSN: 0018-019X
    Keywords: Chemistry ; Organic Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Notes: Chemistry of α-Aminonitriles. Aldomerisation of Glycolaldehyde Phosphate to rac-Hexose 2,4,6-Triphosphates and (in Presence of Formaldehyde) rac-Pentose 2,4-Diphosphates: rac-Allose 2,4,6-Triphosphate and rac-Ribose 2,4-Diphosphate Are the Main Reaction ProductsGlyclaldehyde phosphate aldomerizes in aqueous NaOH solution to a product mixture containing the racemates of the two diastereoisomeric tetrose 2,4-diphosphates and eight hexose 2,4,6-triphosphates. At room temperature in the absence of air and after 7 days, a solution 0.08Min glycolaldehyde phosphate (=formylmethyl dihydrogenphosphate)and 2M in NaOH gives products, in up to 80% yield, with a tetrose/hexose derivative ratio of ca 1:10 and with rac-allose, 2,4,6-triphosphate comprising up to 50% of the mixture of sugar phosphates. When the reaction is run under the same conditions but in the presence of 0.5 mol-equiv. of formaldehyde, sugar phosphates are formed in up to 45% yield, with pentose 2,4-diphosphates now predominating over hexose triphosphates by a ration f 3:1 rac-Ribose 2,4-diphosphate is found to be the major component, the ratios am ribose, arabinose, lyxose, and xylose 2,4-diphosphates being 52:14:23:11 in a representative experiment. The pentose diphosphates are constitutionally stable under the reaction conditions (observed for 23 weeks), but the diastereoisomeric ratios slowly change with time (tc 22:34:30:14 after 23 weeks), showing that ribose 2,4-diphosphate is not the thermodynamically favored diastereoisomer. The observed product distributions in both the pentose and the hexose series (after 1 week) reveal an aldolization mode that is preferentially erythro in the product-determining step (the reaction of glycolaldehyde phosphate as its enolate with glycerinaldehyde 2-phosphate and tetrose 2,4-diphosphate, respectively). An attempt is made to rationalize both this fact and the kinetic predominance of ribose 2,4-diphosphate in the pentose series and allose 2,4,6-triphosphate in the hexose series. Their configuration along the C-chain can be interpreted as corresponding to a minimum number of 1-5 repulsions in the packing of phosphate and OH substituents and minimal steric interaction between substituents at the reaction centers in the transition state of the product-determining step. The aldomerization of glycolaldehyde phosphate in the presence of formaldehyde is a variant of the formose reaction, It avoids the formation of complex formose product mixtures, largely as a consequence of the fact that aldoses which are phosphorylated at the C(2)
    Additional Material: 13 Ill.
    Type of Medium: Electronic Resource
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  • 3
    Publication Date: 2023-07-18
    Keywords: 21-209; AGE; Calculated; Cibicidoides sp., δ13C; Cibicidoides sp., δ18O; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Globigerinoides ruber, δ13C; Globigerinoides ruber, δ18O; Glomar Challenger; Leg21; Mass spectrometer VG Isogas Prism; Sample code/label; South Pacific/Coral Sea/PLATEAU; Δδ13C; Δδ18O; δ18O, reconstructed
    Type: Dataset
    Format: text/tab-separated-values, 447 data points
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  • 4
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    PANGAEA
    In:  Supplement to: Müller, Daniel W; Müller, Paul A; McKenzie, Judith A (1990): Strontium isotopic ratios as fluid tracers in Messinian evaporites of the Tyrrhenian Sea (western Mediterranean Sea). In: Kastens, KA; Mascle, J; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 107, 603-614, https://doi.org/10.2973/odp.proc.sr.107.194.1990
    Publication Date: 2024-01-09
    Description: Strontium isotopic ratios of gypsums recovered from upper Miocene (Messinian) evaporites at ODP Leg 107 Holes 652A, 653B, and 654A (Tyrrhenian Sea) are lower than expected. The values for the Messinian balatino-like gypsum, single gypsum crystals, and anhydrites range from 0.70861 to 0.70886 and are approximately 25 * 10**-5 less than would be expected for evaporites precipitated from Messinian seawater (0.70891-0.70902). Pre-evaporitic planktonic foraminifers from Hole 654A show variable degrees of dolomitization and 87Sr/86Sr values that irregularly decrease upward from normal marine values approximately 81m below the lowest evaporite occurrence. This suggests diagenetic alteration by advecting interstitial water with a low 87Sr/86Sr ratio or that the lower Sr isotopic ratios for the Messinian evaporites could have resulted from a greater influence of fresh water on the Sr isotopic composition of the desiccating Tyrrhenian Sea. Fluctuations of the 87Sr/86Sr-ratio for evaporites in the sedimentary cycles recognized for Holes 653B and 654A, the generally low Sr isotopic ratio of river water entering the Mediterranean Sea, and the presence of dwarf marine microfossils suggest that the 87Sr/86Sr ratio of the evaporites responded to hydrologic variations in a very restricted basin with variable rates of marine and fresh water input. The strontium isotopic ratios of the Messinian anhydrites from the proposed lacustrine sequence at Hole 652A fall in the same range as the marine evaporites from Holes 654A and 653B. This suggests a common or similar origin of the brines at the three locations. The complex depositional and hydrologic conditions in the Mediterranean during the Messinian salinity crisis preclude the use of Sr isotopic values from the evaporites for stratigraphic correlation and dating. They are, however, very useful in the interpretation of the depositional history of the basin. General calculations assuming a closed system suggest that the 87Sr/86Sr ratio of Messinian seawater (-0.7090) could be reduced to that of the evaporites (-0.7087) by mixing with fresh water (e.g., Nile River) in times of 10**4 to 10**5 yr.
    Keywords: 107-652A; 107-653B; 107-654A; DRILL; Drilling/drill rig; Joides Resolution; Leg107; Ocean Drilling Program; ODP; Tirreno Sea
    Type: Dataset
    Format: application/zip, 6 datasets
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  • 5
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    PANGAEA
    In:  Supplement to: Mead, Gregory; Hodell, David A; Müller, Daniel W; Ciesielski, Paul F (1991): Fine-fraction carbonate oxygen and carbon isotope results from Site 704: implications for movement of the polar front during the late Pliocene. In: Ciesielski, PF; Kristoffersen, Y; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 114, 437-458, https://doi.org/10.2973/odp.proc.sr.114.152.1991
    Publication Date: 2024-01-09
    Description: Ocean Drilling Program Site 704 in the subantarctic South Atlantic was drilled to investigate the response of the Southern Ocean to climatic and Oceanographic developments during the late Neogene. Stable oxygen and carbon isotopes of fine-fraction (〈63 µm) carbonate were analyzed to supplement similar analyses of benthic and planktonic foraminifers. The fine fraction is generally composed primarily of coccoliths, and isotopic analyses of the fine fraction were made to complement the foraminiferal analyses. The isotopic curves thus generated suggest paleoceanographic changes not recognizable by the use of benthic and planktonic foraminifers alone. The global Chron 6 carbon isotope shift, found at 253-244 mbsf (6.39-6.0 Ma) at Site 704 in the planktonic and benthic record, is seen in the fine-fraction d13C record as a gradual decrease from 255 mbsf (6.44 Ma) to 210 mbsf (4.24 Ma). At 170 mbsf, mean d18O values of Neogloboquadrina pachyderma increase by 0.6 per mil-0.7 per mil (Hodell and Ciesielski, 1991, doi:10.2973/odp.proc.sr.114.150.1991), reflecting decreased temperature and increased continental ice volume. Accumulation rates increase by 3.3 times above this depth (which corresponds to an age of 2.5 Ma), suggesting increased upwelling and biologic productivity. Carbon isotopic values of fine-fraction carbonate decrease by about 1.5 per mil at 2.6 Ma; however, no change is recorded in the d13C of N. pachyderma. The fine-fraction d13C shift slightly precedes an average l per mil decrease in d13C in benthic foraminifers. The cause of the benthic d13C shift (most likely due to a change in deep water circulation; Hodell and Ciesielski, 1991) is probably not directly related to the fine-fraction shift. The fine-fraction shift is most likely caused by (1) a change in the upwelling to productivity ratio at this site, with increased upwelling bringing lighter carbon to surface waters, more productivity, and higher sedimentation rates and (2) a change in the particle composition of the fine fraction. The increased upwelling is probably due to a northward migration of the Antarctic Polar Front to a position nearer Site 704.
    Keywords: 114-704A; 114-704B; DRILL; Drilling/drill rig; Joides Resolution; Leg114; Ocean Drilling Program; ODP; South Atlantic Ocean
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 6
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    PANGAEA
    In:  Supplement to: Chamley, Hervè; Robert, Christian; Müller, Daniel W (1993): The clay-mineralogical record of the last 10 million years off northeastern Australia. In: McKenzie, JA; Davies, PJ; Palmer-Julson, A; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 133, 461-470, https://doi.org/10.2973/odp.proc.sr.133.247.1993
    Publication Date: 2024-01-09
    Description: Clay mineral assemblages for the last 10 m.y. are described for Site 823, at 16°S in the Queensland Trough, to the northeast of Australia. Largely unaffected by diagenetic influences, these mostly express the evolution of northeastern Australian continental environments during the late Neogene: (1) beginning during the late Miocene at about 7.0 Ma is an increase of illite derived from rocky substrates at the expense of smectite from deeply weathered soils; this increase was the result of increasing aridity in the Australian interior and globally cooler temperatures, associated with increases in Antarctic glaciation; (2) concomitant and further increases of kaolinite fluxes to the Queensland Trough during the late Miocene-early Pliocene largely reflect an increase in rainfall in northeastern Australia; (3) increases in both soil- and rock-derived minerals probably intensified as a result of late Neogene uplift of the eastern highlands; (4) clay-mineral associations during the Pliocene and Pleistocene display minor variations only and probably resulted in part from differential settling and sea-level changes; (5) similar trends of clay-mineral variations occur at both ODP Site 823 and DSDP Site 588 (Lord Howe Rise). Less abundant kaolinite relative to illite at Site 588 nevertheless suggests a southward decrease of continental humidity and/or of the eastern highlands uplift; (6) influences of global climate and oceanic and atmospheric circulations on clay-mineral associations dominated during the late Miocene and were progressively replaced by influences of more regional environmental variations during the Pliocene and especially the Pleistocene.
    Keywords: Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 7
    Publication Date: 2024-01-09
    Keywords: 133-811A; AGE; Calculated; Cibicidoides sp., δ13C; Cibicidoides sp., δ18O; Coral Sea; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Globigerinoides ruber, δ13C; Globigerinoides ruber, δ18O; Joides Resolution; Leg133; Mass spectrometer VG Isogas Prism; Ocean Drilling Program; ODP; Sample code/label; Δδ13C; Δδ18O; δ18O, reconstructed
    Type: Dataset
    Format: text/tab-separated-values, 657 data points
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  • 8
    Publication Date: 2024-01-09
    Keywords: 133-817A; 133-818B; Age model; Age model, optional; Coral Sea; Datum level; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; Event label; Joides Resolution; Leg133; Ocean Drilling Program; ODP
    Type: Dataset
    Format: text/tab-separated-values, 114 data points
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  • 9
    Publication Date: 2024-01-09
    Keywords: 133-819A; 133-820A; 133-821A; 133-823A; 133-824A; 133-825A; Chlorite; Coral Sea; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Epoch; Event label; Illite; Joides Resolution; Kaolinite; Leg133; Mixed layer clay minerals; Ocean Drilling Program; ODP; Palygorskite; Sample code/label; Smectite; X-ray diffraction TEXTUR, clay fraction
    Type: Dataset
    Format: text/tab-separated-values, 120 data points
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  • 10
    Publication Date: 2024-01-09
    Keywords: 133-818B; AGE; Aragonite, fractionated; Calcite, fractionated; Carbonate, fractionated; Carbonate bomb (Müller & Gastner, 1971); Cibicidoides spp., δ13C; Cibicidoides spp., δ18O; Coral Sea; Counting 〉355 µm fraction; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Globigerinoides sacculifer, δ13C; Globigerinoides sacculifer, δ18O; Grain size, sieving; Joides Resolution; Leg133; Magnesium-Calcite; Mass spectrometer VG Isogas Prism; Ocean Drilling Program; ODP; Pteropoda; Size fraction 〈 0.063 mm, mud, silt+clay; X-ray diffraction (XRD)
    Type: Dataset
    Format: text/tab-separated-values, 2126 data points
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