cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.811432
title: (Table 3) Physical properties of DSDP Hole 72-515A

description: Hole 515A was drilled in the southern Brazil Basin by the Glomar Challenger on DSDP Leg 72, using the newly developed hydraulic piston corer (HPC). A total of 108 m of undisturbed terrigenous mud (T1) and sandy mud (T2) was obtained (see site chapter, Site 515, this volume). The core was sampled at levels that corresponded to 50-kPa increments of overburden pressure to determine if a pattern of clay fabric development could be discerned. After criticalpoint drying and gold-palladium coating, 15 samples were analyzed with a scanning electron microscope (SEM). Clay fabric consists of randomly oriented, large and small domains of face-to-face (FF) stacked clay particles, frequently linked together by short "chains" in an edge-to-face (EF) orientation. As overburden pressure increases, linkages decrease, and the "chains" become incorporated into the domains. Distortion of platelike domains into "cornflake" structures (well-crystallized montmorillonite?) and spherical aggregates occurs at overburden pressures of 400 kPa. Orientation parallel with bedding occurs at 500 kPa as the "cornflake" structures become flattened and compressed. Maximum fabric development occurs at 590 kPa. Large plates and coalesced domains form a pervasive linear FF pattern, interrupted by a few large and small EF bridging structures. Deformation of the large EF-oriented plates occurs, forming circular, pitlike voids. Fabric development in cores from this deep-sea site follows well the developmental model suggested by Bennett and others (1981) for Mississippi Delta clays with high to medium void ratios.
description: Supplement to: Faas, Richard W; Crocket, David S (1983): Clay fabric development in a Deep-Sea Core: Site 515, Deep Sea Drilling Project Leg 72. In: Barker, PF; Carlson, RL; Johnson, DA; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 72, 519-535
DOI: 10.1594/pangaea.824960
title: Moisture and density (MAD) measured on IODP Hole 334-U1379C

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.778470
title: Moisture and density (MAD) measured on IODP Hole 317-U1352C

description: Geocode = Depth CSF-A (m). MAD data are acquired on ~10 mL sediment or rock subsamples by measuring three out of four material parameters: wet (saturated) mass and/or volume, and dry mass and/or volume after 24 h drying in a convection oven. The combination of measurements is defined by the submethod (A, B, C, D). Wet (A, B, C) and dry (A, B, C, D) mass is determined using motion-compensated signals from commercial Mettler-Toledo balances. Wet volume (A, B, D) is determined by the sample's geometric dimensions using calipers. Dry volume (C, D) is measured by helium pycnometry. Submethods A and B are not recommended by IODP). Submethod C is suitable for saturated materials such as fine-grained sediments. Submethod D is suitable for unsaturated porous material such as certain limestones and basalts. From the moisture and volume measurements, the following phase relationships are calculated: wet and dry water content, wet bulk density, dry bulk density, grain density, porosity, and void ratio. Technical Note 26 Chapter 2: http://www-odp.tamu.edu/publications/tnotes/tn26/CHAP2.PDF
DOI: 10.1594/pangaea.826276
title: Moisture and density (MAD) measured on IODP Hole 330-U1372A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.763502
title: Moisture and density (MAD) measured on IODP Hole 325-M0054B
DOI: 10.1594/pangaea.824561
title: Moisture and density (MAD) measured on IODP Hole 318-U1360A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.826031
title: Moisture and density (MAD) measured on IODP Hole 327-U1363B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.826323
title: Moisture and density (MAD) measured on IODP Hole 330-U1375B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.828699
title: Moisture and density (MAD) measured on IODP Hole 336-U1382B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.828701
title: Moisture and density (MAD) measured on IODP Hole 336-U1383D

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.475943
title: Geochemistry of sediment core MH_31 from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.828702
title: Moisture and density (MAD) measured on IODP Hole 336-U1383E

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.785906
title: Moisture and density (MAD) measured on IODP Hole 333-C0012E

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.825972
title: Moisture and density (MAD) measured on IODP Hole 329-U1366D

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.828887
title: Moisture and density (MAD) measured on IODP Hole 339-U1389C

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.828888
title: Moisture and density (MAD) measured on IODP Hole 339-U1389E

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.763500
title: Moisture and density (MAD) measured on IODP Hole 325-M0053A
DOI: 10.1594/pangaea.827309
title: Moisture and density (MAD) measured on IODP Hole 329-U1368D

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.829169
title: Moisture and density (MAD) measured on IODP Hole 340-U1395B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.475985
title: Geochemistry of sediment core M1_MULT226 from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.825280
title: Moisture and density (MAD) measured on IODP Hole 329-U1368F

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.763494
title: Moisture and density (MAD) measured on IODP Hole 325-M0047A
DOI: 10.1594/pangaea.824457
title: Moisture and density (MAD) measured on IODP Hole 318-U1358B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.826429
title: Moisture and density (MAD) measured on IODP Hole 329-U1367C

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.828456
title: Moisture and density (MAD) measured on IODP Hole 323-U1339B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.744514
title: (Table 2) Forms of sulfur occurrence in bottom sediments from the Gulf of California
DOI: 10.1594/pangaea.817785
title: (Table 2) Oedometer test conditions, specimen properties, and results for samples from IODP Sites 317-U1351, 317-U1352, 317-U1353 and 317-U1354

description: DEPTH, sediment/rock = Depth CSFA (m)Empty cells = not applicable
DOI: 10.1594/pangaea.828457
title: Moisture and density (MAD) measured on IODP Hole 323-U1340A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.763482
title: Moisture and density (MAD) measured on IODP Hole 325-M0033A
DOI: 10.1594/pangaea.775940
title: Eh, pH and contents of Fe, Mn, organic carbon, CaCO3, Mo, and W in bottom sediments of the Stromboli Canyon at Station PGS-1963
DOI: 10.1594/pangaea.817569
title: (Table 1) Sediment properties at DSDP Leg 67 Holes

description: The plasticity characteristics of the Quaternary sediments of the Guatemalan continental margin were determined from five sites drilled during Leg 67 of the Deep Sea Drilling Project. The 64 samples analyzed are from various marine environments, including the Cocos Plate, Middle America Trench, and the trench lower slope to midslope of the Guatemalan continental slope. The sediments are primarily hemipelagic muds and trench-fill turbidites and include quantities of siliceous and calcareous biogenic components. The sediments are generally classified as organic clays of medium to high plasticity, containing micaceous sands and silts, with 14% classed as inorganic clays of medium to high plasticity. High sedimentation rates in Quaternary sediments are the result, in part, of sediment gravity flows that depend upon rheological properties, i.e., sediment plasticity. Mudflows and cohesive debris flows appear to be significant downslope transport mechanisms in these highly plastic sediments.
description: Supplement to: Faas, Richard W (1982): Plasticity characteristics of the Quaternary sediments of the Guatemalan Continental Slope, Middle America Trench, and Cocos Plate - Leg 67, Deep Sea Drilling Project. In: Abouin, J; von Huene, R; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 67, 639-644
DOI: 10.1594/pangaea.763490
title: Moisture and density (MAD) measured on IODP Hole 325-M0041A
DOI: 10.1594/pangaea.763491
title: Moisture and density (MAD) measured on IODP Hole 325-M0042A
DOI: 10.1594/pangaea.828460
title: Moisture and density (MAD) measured on IODP Hole 323-U1343A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.777784
title: (Table 2) Sulfates in interstitial waters and solid phase of bottom sediments from the Pacific Ocean to the east of Japan
DOI: 10.1594/pangaea.786357
title: (Table 1) Physical properties of bottom sediments from Core ASV16-1372
DOI: 10.1594/pangaea.611511
title: Water content of sediment core LD05/AC_24
DOI: 10.1594/pangaea.726372
title: (Table 1) Thermal conductivity, porosity, wet weight water content, bulk and grain density, and sonic velocity of ODP Hole 113-690B
DOI: 10.1594/pangaea.819892
title: Organic matter, carbonate, and siliciclastic components of sediment core St09
DOI: 10.1594/pangaea.475963
title: Geochemistry of sediment core MH_32KA from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.475977
title: Geochemistry of sediment core M1_MULT198 from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.475982
title: Geochemistry of sediment core M1_MULT219 from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.828877
title: Moisture and density (MAD) measured on IODP Hole 339-U1385A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.824046
title: Moisture and density (MAD) measured on IODP Hole 320-U1336B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.829167
title: Moisture and density (MAD) measured on IODP Hole 340-U1394B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.605221
title: Groundwater observations at Sarso Beach, Red Sea (Table 1)
DOI: 10.1594/pangaea.758850
title: (Table 6) Concentrations of various components in bottom sediments near the Curieuse Island
DOI: 10.1594/pangaea.778558
title: Chemical composition New-Euxinian and pre-New-Euxinian sediments from Core $, Black Sea

description: Geochemical data on New-Euxinian sediments and the first data on pre-New-Euxinian sediments of the Black Sea are reported in the paper. 4 meter long sediment core was collected in August 1977 during Cruise 61 of R/V Vityaz.
DOI: 10.1594/pangaea.878130
title: (Table 1) Average water content, supported and unsupported dry dose rate, environmental dose rate, equivalent dose and age for OSL samples from sediment core MD03-2607
DOI: 10.1594/pangaea.797469
title: (Table 1) Index physical properties for consolidation samples of ODP Sites 167-1020 and 167-1021
DOI: 10.1594/pangaea.809686
title: (Table 1) Physical properties at DSDP Hole 77-535
DOI: 10.1594/pangaea.475962
title: Geochemistry of sediment core MH_29SK from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.475964
title: Geochemistry of sediment core MH_35KA from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.615772
title: Grain size composition of Norwegian Sea bottom sediments, Core PL-96-010 sampled from R/V Professor Logachev in 1996
DOI: 10.1594/pangaea.767619
title: (Table 3) Concentrations of organic compounds in surface layer bottom sediments of the Obskay Guba and the Kara Sea
DOI: 10.1594/pangaea.611514
title: Water content of sediment core LD05/AC_34
DOI: 10.1594/pangaea.790795
title: (Table 1) Hydrocarbon contents in bottom sediments during the May 2005 flood, Dvina River estuary

description: Stations Dvina05-9 and Dvina05-57 to 60 had to be omitted due to missing geographical positions. For data on the May 2006 flood see Nemirovskaya (2011) dataset: doi:10.1594/PANGAEA.790780.
DOI: 10.1594/pangaea.475954
title: Geochemistry of sediment core MH_11SK from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.475984
title: Geochemistry of sediment core M1_MULT223 from the Indian Ocean (Appendix)
DOI: 10.1594/pangaea.742510
title: (Figure 2) Physical properties, grain size distribution and contents of carbonate and organic carbon of sediment core JR104-GC368

description: Analysed on bulk sediment samples. Further relevant datasets see Hillenbrand et al. (2009): mineralogical analysis of the clay fraction doi:10.1594/PANGAEA.711158, measurement of shear strength doi:10.1594/PANGAEA.711085.
DOI: 10.1594/pangaea.771106
title: (Table 4.2.8) Rate of sulfate reduction and abundance of sulfate-reducing bacteria in Upper Holocene bottom sediments of the Baltic Sea
DOI: 10.1594/pangaea.760952
title: Fig. 4 Sedimentology of core Lz1084 from the central lake basin
DOI: 10.1594/pangaea.611505
title: Water content of sediment core LD05/AC_14
DOI: 10.1594/pangaea.725830
title: (Table 2) Physical properties of surface sediments from the Enisei section and Al and Si contents in their dry bulk matter
DOI: 10.1594/pangaea.744500
title: (Table 1) Redox conditions and contents of chemical components in bottom sediments from the Eastern Pacific and Gulf of California
DOI: 10.1594/pangaea.742504
title: (Figure 2) Physical properties, grain size distribution and contents of carbonate and organic carbon of sediment core JR104-GC371

description: Analysed on bulk sediment samples. Further relevant datasets see Hillenbrand et al. (2009): mineralogical analysis of the clay fraction doi:10.1594/PANGAEA.711160, measurement of shear strength doi:10.1594/PANGAEA.711087.
DOI: 10.1594/pangaea.813396
title: (Table 1) Thermal conductivity and water content at DSDP Hole 71-511

description: At Hole 511, on the margin of Maurice Ewing Bank, eastern Falkland Plateau, successful bottom hole temperature measurements were made at 52.5 and 113 meters below the seafloor. The results show a regular increase of temperature with depth of 0.074 °C m**-1.Conductivity measurements on core samples, made on board ship and at the Lamont-Doherty repository, gave a mean value of 0.842 W °C**-1 m**-1. The heat flow indicated by these observations is 62.3 mW m**-2 (1.49 HFU), a value that is compatible with the geological evolution of the plateau.
description: Supplement to: Langseth, Marcus G; Ludwig, William J (1983): A heat flow measurement on the Falkland Plateau. In: Ludwig, WJ; Krasheninnikov, VA; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 71, 299-303
DOI: 10.1594/pangaea.727174
title: (Table 2) Contents of organic compounds in the surface layer of bottom sediments from the north Caspian Sea shelf

description: Py=pyrene, Bp=benz(a)pyrene, Chr=chrysene, Pl=perylene, Fl=fluoranthene, An=anthracene
DOI: 10.1594/pangaea.759912
title: (Table 4) Physical properties of ODP Hole 122-762C

description: Sediment depth is given in mbsf. This table is compiled from shipboard measurements (Haq, et al., 1990, doi:10.2973/odp.proc.ir.122.1990).
DOI: 10.1594/pangaea.755956
title: (Table 1) Organic matter and biochemical composition of bottom sediments and interstitial waters of several Antarctic areas

description: Amounts of organic matter, proteins, carbohydrates and lipids were studied in the upper layer of bottom sediments and interstitial waters on the shelf and slope of the Lazarev Sea, the eastern section of the Bransfield Strait, north of the South Georgia Island, and in the northern Peru area. Biological activity of bottom sediments was determined by measuring protease activity (decomposition of proteins to amino acids) and activity of the electron transport system (rate of oxidation of organic matter to CO2 and H2O). Recirculation time of proteins and time of complete oxidation of organic matter to CO2 and H2O were determined. Recirculation time of proteins and of organic matter in the production-destruc¬tion cycle averaged 2 to 3 orders of magnitude shorter in the Antarctic regions than in the Peru area. Interstitial waters are assumed to play a principal role in circulation of organic matter at water-sediment-interstitial water interfaces.
description: Supplement to: Andreeva, N M; Agatova, Alina I (1985): Biological activity of bottom sediments in some Antarctic regions and off the coast of Peru. Oceanology, 25(6), 738-743
DOI: 10.1594/pangaea.784116
title: (Table T1) Density, porosity, void ratio, diffusivity and permeability of ODP Site 185-1149 sediments

description: The subduction of oceanic plates regulates crustal growth, influences arc volcanism, and refertilizes the mantle. Continental growth occurs by subduction of crustal material (seawater components, marine sediments, and basaltic crust). The geochemical and physical evolution of the Earth's crust depends, in large part, on the fate of subducted material at convergent margins (Armstrong, 1968, doi:10.1029/RG006i002p00175; Karig and Kay, 1981, 10.1098/rsta.1981.0108). The crustal material on the downgoing plate is recycled to various levels in the subduction zone. The recycling process that takes place in the "Subduction Factory" is difficult to observe directly but is clearly illuminated using chemical tracers. Von Huene and Scholl (1991, doi:10.1029/91RG00969) and Plank and Langmuir (1993, doi:10.1038/362739a0) preliminarily calculated a large flux of subducted materials. By mass balancing the chemical tracers and measuring the fractionations that occur between them, the Subduction Factory work and the effect on the Earth's evolution can be estimated. In order to elucidate this mass balance, Ocean Drilling Program Leg 185 drilled two deepwater shales into the oceanic crust situated in the Mariana-Izu Trenches and recovered core samples of incoming oceanic crust. The calculations of mass circulation in the subduction zone, however, did not take into account the mass transfer properties within subducted oceanic crust, although the dewatering fluid and diffused ions may play an important role in various activities such as seismogeneity, serpentine diapiring, and arc volcanism. Thus, this paper focuses on the quantitative measurements of the physical and mass transfer properties of subducted oceanic crust.
description: Supplement to: Hirono, Tetsuro (2003): Data report: Measurement of mass transfer properties with subducted oceanic plate. In: Ludden, JN; Plank, T; Escutia, C (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 185, 1-14
DOI: 10.1594/pangaea.776638
title: A 3.1.1. Municipal waste incineration ash: material description - material parameter
DOI: 10.1594/pangaea.785111
title: (Table 1) Summary of CT values, attenuation coefficients, density, and porosity of ODP Site 131-808A samples

description: This paper presents results of an interdisciplinary investigation of the relation between fluids, fluid flow, and deformation in the toe region of the Nankai accretionary prism. The techniques include thin-section petrography, SEM, TEM and microprobe analyses, and X-ray computed tomography as well as laboratory experiments. Together, the data suggest three structural/hydrologic regimes within the prism. These are: (1) the accreting sediments above the décollement zone, (2) the décollement zone, and (3) the underthrust sediments. The regime above the décollement is characterized by sediments that are progressively dewatered through both a penetrative fabric and a pervasive, but apparently poorly interconnected, set of core-scale deformation structures. The décollement is characterized by a relatively high density of structures/meter and is considered to be a regime of low stress but frequent failure. Hydrologically the décollement retards the vertical flow of fluids and enhances the potential for overpressuring in the footwall. Finally, the footwall regime contains very few tectonic structures and is structurally isolated from the stresses related to plate convergence. This regime provides an important component to the tectonics of the Nankai prism, however, because it supplies the overpressured fluids that cause the d?collement to fail at relatively low shear stresses.
description: Supplement to: Byrne, Timothy; Maltman, Alex J; Stephenson, Emma; Soh, Wonn; Knipe, Rob (1993): Deformation structures and fluid flow in the toe region of the Nankai accretionary prism. In: Hill, IA; Taira, A; Firth, JV; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 131, 83-101
DOI: 10.1594/pangaea.786522
title: (Table 1) Floral and faunal characteristics of five sites in northern Victoria Land
DOI: 10.1594/pangaea.757085
title: (Table 1) Mineral phosphorus contents in bottom sediments and interstitial waters of the Southeast Atlantic

description: Concentrations of mineral phosphorus in interstitial waters from sediments of the Southeast Atlantic generally increases from the ocean bed to the continental slope and shelf. In diatomaceous oozes of the Southwest Africa shelf, phosphorus concentration in fresh interstitial waters reaches 2.5 mg/l in absence of phosphorite concretions and 0.1-0.7 mg/l in their presence. After prolonged storage of samples concentration of dissolved mineral phosphorus sometimes increases up to 7-8 mg/l. The key factor regulating phosphorus content of solid and liquid phases of unaltered sediments are content and composition of organic matter.
description: Supplement to: Baturin, Gleb N (1972): Phosphorus in interstitial waters of sediments of the Southeastern Atlantic. Oceanology, 12, 849-855
DOI: 10.1594/pangaea.817701
title: (Table 2) Consolidation test results and geotechnical properties of samples tested from DSDP Hole 66-488
DOI: 10.1594/pangaea.819891
title: Organic matter, carbonate, and siliciclastic components of sediment core Oh09
DOI: 10.1594/pangaea.763741
title: (Table 1a) Geochemical parameters of bottom sediments from the Ob River mouth area
DOI: 10.1594/pangaea.817703
title: (Table 4) Consolidation test results and geotechnical properties of samples tested from DSDP Hole 66-491
DOI: 10.1594/pangaea.789389
title: (Table 2) Physical properties of sediment at DSDP Hole 93-603B
DOI: 10.1594/pangaea.775941
title: Eh, pH and contents of Fe, Mn, organic carbon, CaCO3, Mo, and W in bottom sediments of the Stromboli Canyon at Station PGS-1960
DOI: 10.1594/pangaea.820068
title: (Table 1) Sample description and tetrapyrrole pigment yield at DSDP Leg 60 Holes

description: In order to provide a better understanding of the fate of sedimentary chlorophyll and chlorophyll degradation products in all kinds of environments, we have recently expanded our studies to include examination of sediments returned from Legs which are not rich in organic matter, nor are even primarily biogenic. Eight core samples from the Mariana Basin and Trench, obtained from DSDP Leg 60, were analyzed for products of chlorophyll diagenesis. To date, the sediment samples from the South Philippine Sea have been the most organically barren examined. Through elimination of the bias of examining only sediments rich in organic matter, we hope that the fate of chlorophyllous material on a more global scale will eventually be elucidated.
description: Sediment depth is given in mbsf. Empty cells = no data.
description: Supplement to: Baker, Earl W; Louda, William (1982): Chlorophyll derivatives in sediments of the South Philippine Sea, Deep Sea Drilling Project Leg 60. In: Hussong, DM; Uyeda, S; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 60, 497-500
DOI: 10.1594/pangaea.784189
title: (Table 41-2) Redox potential, water content, and calcium carbonate and organic carbon contents in bottom sediments collected by cores within the Tajura Rift