cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.815192
title: Pigment concentrations from three stations at Potter Cove, King George Island, West Antarctic Peninsula

description: Samples analyzed by Donato Giovannelli (mailto:donato.giovannelli@an.ismar.cnr.it) and Manini Elena (mailto:e.manini@ismar.cnr.it). For the pigment analysis sediment cores were sliced at 0-1, 1-3 and 3-5 cm layers. The analysis of chlorophyll-a (Chl-a) and phaeopigments was carried out according to Lorenzen (1980, doi:10.4319/lo.1967.12.2.0343). Pigments were extracted (12 h at 4 °C in the dark) from each layer using 5 ml of 90% acetone. Extracts were analysed fluorometrically to estimate the chlorophyll-a and phaeopigment concentration, after acidification with 200 ml 0.1N HCl. The concentrations of Chl-a and phaeopigments (expressed in µg/g of dry sediment) were summed to obtain the total chlorophyll concentration (Chloroplastic Pigments Equivalent, CPE).
DOI: 10.1594/pangaea.757896
title: (Table 1) Alkenones and GDGT analysis for core-top sediments from the southern Adriatic Sea

description: Environmental data: Chl-a=Chlorophyll-a. SSS=Salinity; an=annual, sp=spring (Mar-Apr-May), su=summer (Jun-Jul-Aug), au=autumn (Sep-Oct-Nov), wi=winter (Dec-Jan-Feb) (Zonneveld et al., 2009).
DOI: 10.1594/pangaea.757315
title: Alkenon concentrations of Creatcesous sediments of DSDP Hole 76-534A (Table 1)

description: We here report the discovery of unusual distributions of long-chain alkenones (C37-C42) in two Cretaceous black shales from the Blake-Bahama Basin, western North Atlantic. These sediments are Cenomanian (c. 95 Ma) and mid-Albian (c. 105 Ma) in age, thus significantly extending the geological range of these compounds. The precise source of these lipids is, as yet, unknown, although they may derive from an ancient ancestor of Emiliania huxleyi.
description: # = concentration estimated by mas fragmentography due to co-evolution. &lt;1 = trace amount detected.
description: Supplement to: Farrimond, Paul; Brassell, Simon C (1985): Alkenones in Cretaceous black shales, Blake-Bahama Basin, western North Atlantic. Organic Geochemistry, 10(4-6), 897-903
DOI: 10.1594/pangaea.815221
title: (Table 1) Low molecular weight hydrocarbon concentrations and organic carbon contents at DSDP Hole 71-511

description: C2-C8 hydrocarbons (36 compounds identified) from 56 shipboard sealed, deep-frozen core samples of DSDP Leg 71, Site 511, Falkland Plateau, South Atlantic, were analyzed by a combined hydrogen stripping-thermovaporization method. Concentrations, which represent hydrocarbons dissolved in the pore water and adsorbed to the mineral surfaces of the sediment, vary from 24 ng/g of dry weight sediment in Lithologic Unit 4 to 17,400 ng/g in Lithologic Unit 6 ("black shale" unit). Likewise, the organic carbon normalized C2-C8 hydrocarbon concentrations range from 104 to 3.5 x 105 ng/g Corg. The latter value is more than one order of magnitude lower than expected for petroleum source beds in the main phase of oil generation. The low maturity at 600 meters depth is further supported by light hydrocarbon concentration ratios. The change of the kerogen type from Lithologic Unit 5 (Type III) to 6 (Type II) is evidenced by changes in the C6 and C7 hydrocarbon composition. Redistribution phenomena are observed close to the Tertiary-Cretaceous unconformity and at the contact between the "black shale" unit and the overlying Cretaceous chalks and claystones. Otherwise, the low molecular weight hydrocarbons in Hole 511 are formed in situ and remain at their place of formation. The core samples turned out to be contaminated by large quantities of acetone, which is routinely used as a solvent during sampling procedures onboard Glomar Challenger.
description: Sediment depth is given in mbsf. # = about; #0 = concentration below or near detection limit, empty cells = not measured or not determined because of peak overlapping.
description: Supplement to: Schaefer, Rainer G; von der Dick, Hans; Leythaeuser, Detlev (1983): C2–C8 hydrocarbons in sediments from Deep Sea Drilling Project Leg 71, Site 511, Falkland Plateau, South Atlantic. In: Ludwig, WJ; Krasheninnikov, VA; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 71, 1033-1043
DOI: 10.1594/pangaea.855497
title: Biomarker proxies on sediment core PS87/086-3
DOI: 10.1594/pangaea.887832
title: IP25 and Uk'37 proxy record of sediment core SO202/1_27-6
DOI: 10.1594/pangaea.807139
title: (Table 4) Pyrolyzate hydrocarbons for various temperature ranges at DSDP Leg 81 Holes

description: These values do not represent the true pyrolysis products, since olefins are not differentiated from napthenes by the mass spectrometer or the Robinson (1971) computer program. The data are used for relative comparison of pyrolysis samples.
DOI: 10.1594/pangaea.884794
title: Sterols in sediment core PS92/039-2
DOI: 10.1594/pangaea.780375
title: (Table 3-3) Rates of carbon dioxide assimilation, methane formation, and methane oxidation in bottom sediments of Poligon I near the Congo River mouth
DOI: 10.1594/pangaea.759566
title: Organic marker compounds in surface sediments from the Nordic Seas

description: Organic geochemical analyses of marine surface sediments from the continental margins of East Greenland and West Spitsbergen provide for a biomarker-based estimate of recent sea ice conditions in the northern North Atlantic. By means of the sea ice proxy IP25 and phytoplankton derived biomarkers (e.g. brassicasterol, dinosterol) we reconstruct sea ice and sea surface conditions, respectively. The combination of IP25 with a phytoplankton marker (in terms of a phytoplankton marker-IP25 index; PIP25) proves highly valuable to properly interpret the sea ice proxy signal as an under- or overestimation of sea ice coverage can be circumvented. A comparison of this biomarker-based assessment of the sea ice distribution in the study area with (1) modern remote sensing data and (2) numerical modelling results reveals a good agreement between organic geochemical, satellite and modelling observations. The reasonable simulation of modern sea ice conditions by means of a regional ocean-sea ice model demonstrates the feasibility to effectively integrate the complex atmospheric and oceanic circulation features as they prevail in the study area. The good correlation between modelled sea ice parameters and the biomarker-based estimate of sea ice coverage substantiates that linking proxy and model data occurs to be a promising concept in terms of a cross-evaluation. This combinatory approach may provide a first step towards quantitative sea ice reconstructions by means of IP25. Future IP25 studies on marine surface sediments from the Arctic realm, however, are recommended to extend and validate this new attempt of using IP25 in combination with a phytoplankton marker as a quantitative measure for sea ice reconstructions.
description: For further details on the total organic carbon data cited in the article we refer to the data set entries by Kierdorf (2006) doi:10.1594/PANGAEA.499864 and Birgel and Stein (2004) doi:10.1594/PANGAEA.191089. Dataset has been reformated after discussion with the PI.
DOI: 10.1594/pangaea.811152
title: Pigments in surface sediments of Potter Cove, King George Island, Antarctic Peninsula
DOI: 10.1594/pangaea.841464
title: (Table 1) Organic and inorganic geochemical analysis of Late Jurassic to Early Cretaceous black shale sediments from the Norwegian-Greenland Seaway

description: The Late Jurassic to Early Cretaceous (Volgian-Ryazanian) was a period of a second-order sea-level low stand, and it provided excellent conditions for the formation of shallow marine black shales in the Norwegian-Greenland Seaway (NGS). IKU Petroleum Research drilling cores taken offshore along the Norwegian shelf were investigated with geochemical and microscopic approaches to (1) determine the composition of the organic matter, (2) characterize the depositional environments, and (3) discuss the mechanisms which may have controlled production, accumulation, and preservation of the organic matter. The black shale sequences show a wide range of organic carbon contents (0.5-7.0 wt %) and consist of thermally immature organic matter of type II to II/III kerogen. Rock-Eval pyrolysis revealed fair to very good petroleum source rock potential, suggesting a deposition in restricted shallow marine basins. Well-developed lamination and the formation of autochthonous pyrite framboids further indicate suboxic to anoxic bottom water conditions. In combination with very low sedimentation rates it seems likely that preservation was the principal control on organic matter accumulation. However, a decrease of organic carbon preservation and an increase of refractory organic matter from the Volgian to the Hauterivian are superimposed on short-term variations (probably reflecting Milankovitch cycles). Various parameters indicate that black shale formation in the NGS was gradually terminated by increased oxidative conditions in the course of a sea-level rise.
description: Supplement to: Langrock, Uwe; Stein, Ruediger; Lipinski, Marcus; Brumsack, Hans-Jürgen (2003): Late Jurassic to Early Cretaceous black shale formation and paleoenvironment in high northern latitudes: Examples from the Norwegian-Greenland Seaway. Paleoceanography, 18(3), 1074
DOI: 10.5281/zenodo.15054361
title: YOUTH SPORTS DEVELOPMENT AND COMMUNITY IMPACT
DOI: 10.5281/zenodo.15054362
title: YOUTH SPORTS DEVELOPMENT AND COMMUNITY IMPACT
DOI: 10.1594/pangaea.838050
title: Pollen profile OLDCAMP, Russia

description: This dataset was archived on 2014-11-03 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.5281/zenodo.15054377
title: TECHNOLOGICAL INNOVATIONS IN SPORTS EQUIPMENT
DOI: 10.5281/zenodo.15054378
title: TECHNOLOGICAL INNOVATIONS IN SPORTS EQUIPMENT
DOI: 10.5281/zenodo.15054383
title: LINGUO CULTURAL ANALYSIS OF THE KING ARTHUR LEGEND DISCOURSE
DOI: 10.5281/zenodo.15054384
title: LINGUO CULTURAL ANALYSIS OF THE KING ARTHUR LEGEND DISCOURSE
DOI: 10.1594/pangaea.830236
title: Geochemistry of sediment core BLS
DOI: 10.1594/pangaea.921184
title: Sterols in sediment core PS100/270-1
DOI: 10.1594/pangaea.921395
title: Pollen and spore content in floodplain sediments of the Tambey River mouth (well 198-YuV)
DOI: 10.1594/pangaea.72128
title: Gaschromatographic analysis of sediment core MD01-2453
DOI: 10.1594/pangaea.708685
title: (Table 2) Concentrations (in dry sediments) of free alkenones, fatty acids, and alcohols in oxidized and unoxidized turbidites from ODP Hole 157-951B
DOI: 10.1594/pangaea.708686
title: (Table 2) Concentrations (in dry sediments) of free alkenones, fatty acids, and alcohols in oxidized and unoxidized turbidites from ODP Hole 157-952A
DOI: 10.1594/pangaea.65432
title: Alkenon data of sediment core MD97-2151
DOI: 10.1594/pangaea.72129
title: Gaschromatographic analysis of sediment core MD01-2457
DOI: 10.1594/pangaea.808659
title: (Table 1) Summary of low-molecular-weight hydrocarbon concentrations, organic carbon contents, Rock-Eval pyrolysis and lithology at DSDP Leg 79 Holes

description: A series of core samples taken during Cruise 79 of Glomar Challenger, drilling offshore Morocco (Mazagan Plateau), is analyzed for their low-molecular-weight hydrocarbon contents. Fifty-four samples from DSDP Holes 544A, 545, 547A, and 547B, deep frozen on board immediately after recovery, are studied by a hydrogen-stripping/thermovaporization technique combined with capillary gas chromatography. Thirty-eight compounds in the C2-C8 molecular range, including saturated, olefinic, and aromatic hydrocarbons, are identified.Because of large differences in organic carbon contents, the total C2-C8 hydrocarbon concentrations vary from about 20 to 1500 ng/g dry sediment weight in the whole sample series. Organic-carbon normalized values are about 3.2 x 10**4 ng/g Corg for Lithologic Subunits IIIA and IIIB at Site 545 (Cenomanian to Aptian) and 1.0 x 10**5 ng/g Corg for Unit V at Site 547 (Cenomanian to Albian) reflecting the slightly more advanced maturity stage at the latter site. Values exceeding 10**5 ng/g Corg (Site 545) and 2 x 10**5 ng/g Corg (Site 547) are associated with samples that are very lean in organic carbon and are generally rich in carbonate. These samples are enriched by small amounts of gaseous hydrocarbons.A detailed study of individual hydrocarbon concentrations, plotted against depth, reveal additional indications for migration phenomena. At Site 547, for instance, the most mobile hydrocarbons studied (e.g., ethane) appear to migrate by diffusion or a related process from more than 700 m depth toward the surface.
description: Sediment depth is given in mbsf. #0 = concentration below or near detection limit (light hydrocarbons), &lt;1 = value insignificant (pyrolysis).
description: Supplement to: Schaefer, Rainer G; Leythaeuser, Detlev; Gormly, James (1984): Generation and migration of low-molecular-weight hydrocarbons in sediments of Deep Sea Drilling Project Leg 79, Sites 544, 545, and 547, offshore Morocco. In: Hinz, K; Winterer, EL; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 79, 743-773
DOI: 10.1594/pangaea.891590
title: Organic contaminants in sediment core from Duluth-Superior Harbor at Minnesota Point, Minnesota, USA

description: Organic contaminants that were not detected:1-Methylnaphthalene; 1,1-Dichloroethane: 1,1-Dichloroethene; 1,1-Dichloropropene; 1,1,1-Trichloroethane; 1,1,1,2-Tetrachloroethane; 1,1,2-Trichloroethane; 1,1,2-Trichlorotrifluoroethane; 1,1,2,2-Tetrachloroethane; 1,2-Dibromo-3-chloropropane; 1,2-Dibromoethane (EDB); 1,2-Dichlorobenzene; 1,2-Dichloroethane; 1,2-Dichloropropane; 1,2-Diphenylhydrazine; 1,2,3-Trichlorobenzene; 1,2,3-Trichloropropane; 1,2,4-Trichlorobenzene; 1,2,4-Trimethylbenzene; 1,3-Dichlorobenzene; 1,3-Dichloropropane; 1,3,5-Trimethylbenzene; 1,4-Dichlorobenzene; 2-Butanone (MEK); 2-Chloronaphthalene; 2-Chlorophenol; 2-Chlorotoluene; 2-Methylnaphthalene; 2-Methylphenol(o-Cresol); 2-Nitroaniline; 2-Nitrophenol; 2,2-Dichloropropane; 2,4-Dichlorophenol; 2,4-Dimethylphenol; 2,4-Dinitrophenol; 2,4-Dinitrotoluene; 2,4,5-Trichlorophenol; 2,4,6-Trichlorophenol; 2,6-Dinitrotoluene; 3-Nitroaniline; 3,3'-Dichlorobenzidine; 3&4-Methylphenol(m&p Cresol); 4-Bromophenylphenyl ether; 4-Chloro-3-methylphenol; 4-Chloroaniline; 4-Chlorophenylphenyl ether; 4-Chlorotoluene; 4-Methyl-2-pentanone (MIBK); 4-Nitroaniline; 4-Nitrophenol; 4,6-Dinitro-2-methylphenol; Acenaphthene; Acenaphthylene; Acetone; Allyl chloride; Anthracene; Benzo(a)anthracene; Benzo(a)pyrene; Benzo(b)fluoranthene; Benzo(ghi)perylene; Benzo(k)fluoranthene; bis(2-Chloroethoxy)methane; bis(2-Chloroethyl) ether; bis(2-Chloroisopropyl) ether; bis(2-Ethylhexyl)phthalate; Bromobenzene; Bromochloromethane; Bromodichloromethane; Bromoform; Bromomethane; Butylbenzylphthalate; Carbazole; Carbon tetrachloride; Chlorobenzene; Chloroethane; Chloroform; Chloromethane; Chrysene; cis-1,2-Dichloroethene; cis-1,3-Dichloropropene; Di-n-butylphthalate; Di-n-octylphthalate; Dibenz(ah)anthracene; Dibenzofuran; Dibromochloromethane; Dibromomethane; Dichlorodifluoromethane; Dichlorofluoromethane; Diethyl ether (Ethyl ether); Diethylphthalate; Dimethylphthalate; Ethylbenzene; Fluoranthene; Fluorene; Hexachloro-13-butadiene; Hexachlorobenzene; Hexachloroethane; Indeno(123-cd)pyrene; Isophorone; Isopropylbenzene (Cumene); Methyl-tert-butyl ether; Methylene Chloride; n-Butylbenzene; N-Nitroso-di-n-propylamine; N-Nitrosodimethylamine; N-Nitrosodiphenylamine; n-Propylbenzene; Naphthalene; Nitrobenzene; p-Isopropyltoluene; PCB-1016 (Aroclor 1016); PCB-1221 (Aroclor 1221); PCB-1232 (Aroclor 1232); PCB-1242 (Aroclor 1242); PCB-1248 (Aroclor 1248); PCB-1254 (Aroclor 1254); PCB-1260 (Aroclor 1260); PCB-1262 (Aroclor 1262); PCB-1268 (Aroclor 1268); Pentachlorophenol; Phenanthrene; Phenol; Pyrene; sec-Butylbenzene; Styrene; tert-Butylbenzene; Tetrachloroethene; Tetrahydrofuran; Toluene; trans-1,2-Dichloroethene; trans-1,3-Dichloropropene; Trichloroethene; Trichlorofluoromethane; Vinyl chloride; Xylene (Total)
DOI: 10.1594/pangaea.900720
title: Biomarkers of sediment cores from site GS15-198-38
DOI: 10.1594/pangaea.919992
title: Biomarkers of sediment core MSM05/3_343310-5-1, extracted by Accelerated Solvent Extractor (ASE)
DOI: 10.1594/pangaea.919993
title: Biomarkers of sediment core MSM05/3_343310-5-1, extracted by ultrasonication (US)
DOI: 10.5281/zenodo.15054381
title: CHIZMA GEOMETRIYASI. MARKAZIY VA PARALLEL PROYEKSIYALAR VA ULARNING XOSSALARI

description: Ushbu maqolada "Chizma geometriyasi" mavzusi doirasida markaziy va parallel proeksiyalar tahlil qilinadi. Markaziy proeksiyalar obyektlarning uch oʻlchovli koʻrinishini ikki oʻlchovli tashqi koʻrinishga oʻtkazish jarayonini nazarda tutadi. Bu turdagi proeksiyada obyektdan koʻz nuqtasiga qarab chizilgan chiziqlar yordamida tasvir yaratiladi. Parallel proeksiyalar esa obyektlarning oʻlchovlari va nisbatlarini saqlagan holda, ularni toʻgʻridan-toʻgʻri koʻrinishda chizish imkonini beradi.

Maqolada har bir proeksiyaning xossalari, qoʻllanilish sohalari va amaliyotda qanday ishlatilishi haqida batafsil maʻlumot beriladi. Shuningdek, proeksiyalarni tushunish va ulardan samarali foydalanish uchun zarur boʻlgan matematik asoslar ham koʻrib chiqiladi. Markaziy va parallel proeksiyalarning farqlari va ularning chizma geometriyasidagi oʻrni, shuningdek, bu metodlar yordamida yaratilgan chizmalar misollari keltiriladi. 

Umumiy qilib aytganda, ushbu maqola chizma geometriyasi faniga qiziqadigan talabalar va mutaxassislar uchun muhim manba boʻlib, proeksiyalarni chuqur tushunishga yordam beradi.
DOI: 10.5281/zenodo.15054382
title: CHIZMA GEOMETRIYASI. MARKAZIY VA PARALLEL PROYEKSIYALAR VA ULARNING XOSSALARI

description: Ushbu maqolada "Chizma geometriyasi" mavzusi doirasida markaziy va parallel proeksiyalar tahlil qilinadi. Markaziy proeksiyalar obyektlarning uch oʻlchovli koʻrinishini ikki oʻlchovli tashqi koʻrinishga oʻtkazish jarayonini nazarda tutadi. Bu turdagi proeksiyada obyektdan koʻz nuqtasiga qarab chizilgan chiziqlar yordamida tasvir yaratiladi. Parallel proeksiyalar esa obyektlarning oʻlchovlari va nisbatlarini saqlagan holda, ularni toʻgʻridan-toʻgʻri koʻrinishda chizish imkonini beradi.

Maqolada har bir proeksiyaning xossalari, qoʻllanilish sohalari va amaliyotda qanday ishlatilishi haqida batafsil maʻlumot beriladi. Shuningdek, proeksiyalarni tushunish va ulardan samarali foydalanish uchun zarur boʻlgan matematik asoslar ham koʻrib chiqiladi. Markaziy va parallel proeksiyalarning farqlari va ularning chizma geometriyasidagi oʻrni, shuningdek, bu metodlar yordamida yaratilgan chizmalar misollari keltiriladi. 

Umumiy qilib aytganda, ushbu maqola chizma geometriyasi faniga qiziqadigan talabalar va mutaxassislar uchun muhim manba boʻlib, proeksiyalarni chuqur tushunishga yordam beradi.
DOI: 10.1594/pangaea.667083
title: (Table 2) Major, trace element and isotopic composition of sediments from DSDP Hole 86-581
DOI: 10.1594/pangaea.921180
title: IP25 and highly branched isoprenoids in sediment core PS100/270-1
DOI: 10.1594/pangaea.496682
title: (Tables 2, 3, 4) Biogeochemical data from surface sediments in the Aegean Sea
DOI: 10.1594/pangaea.897416
title: Pigment concentration of sediment during a mesocosm experiment with addition of Palmaria decipiens and Desmarestia anceps to sediments from Potter Cove
DOI: 10.1594/pangaea.897418
title: Bacterial fatty acids during a mesocosm experiment with addition of Palmaria decipiens and Desmarestia anceps to sediments from Potter Cove

description: Bacterial fatty acids, extracted from samples from core sediments.
DOI: 10.1594/pangaea.855869
title: Biogeochemical measurements of sediments collected at station MSM15/1_506-1 in the Black Sea during the MSM15/1 cruise in 2010
DOI: 10.1594/pangaea.885341
title: Ladderane in ODP Site 201-1229
DOI: 10.1594/pangaea.787052
title: (Table T2) Total organic carbon content, hydrocarbon characteristics and hydrogen and oxygen index of samples from ODP Hole 180-1109D
DOI: 10.1594/pangaea.892651
title: Organic geochemistry of ODP Site 202-1234
DOI: 10.1594/pangaea.496680
title: (Table 1) Chlorophyll and phaeopigment concentrations in surface sediments of the Cretan Sea

description: Undisturbed sediment samples were collected using a multicorer (Barnett, Watson and Connelly (1984): 8 cores, i.d. 9.5 cm), penetrating 20-30 cm deep into the sediments. Upon recovery all cores were vertically divided into 5 layers: 0-1, 1-2, 2-4, 4-6, 6-10 cm depth. For carbohydrate, lipid and protein datas see dataset: doi:10.1594/PANGAEA.759831.
DOI: 10.1594/pangaea.757599
title: Phospholipids in ODP Leg 190 samples (Table 2)

description: Deep subsurface sediments from the Nankai Trough, Japan Sea, ODP Leg 190, sites 1173, 1174, 1177, and near-surface sediments from Hydrate Ridge, NE-Pacific have been analysed by high performance liquid chromatography (HPLC)–electrospray ionisation (ESI)-mass spectrometry (MS). The main objective was to utilize the presence of intact phospholipids as a direct indicator of viable microorganisms. The extracts of Nankai Trough sediments were found to contain a variety of phospholipid (PL) structures, well-known to stem from microorganisms, to depths as great as 745 mbsf and in situ temperatures as high as 85 °C. In addition, high relative amounts of lysophospholipids (e.g. lysophosphatidylcholines) exceeding those of the regular phospholipids were detected. Diglyceride mass fragments of various PLs have been assigned to fatty acyl side-chains of typical chain length (C14, C16, C18, C20) and degree of unsaturation (zero, one or two double bonds). Similar results were obtained for the phospholipid distribution in extracts of organic matter-rich Hydrate Ridge sediments. To date, the enhanced occurrence of lysophospholipids cannot be explained completely but a response to increasing thermal and ecological stress seems probable.
description: Supplement to: Zink, Klaus-Gerhard; Wilkes, Heinz; Disko, Ulrich; Elvert, Marcus; Horsfield, Brian (2003): Intact phospholipids - microbial life markers in marine deep subsurface sediments. Organic Geochemistry, 34(6), 755-769
DOI: 10.1594/pangaea.745039
title: EPOCA 2009 Svalbard benthic experiment: sediments
DOI: 10.1594/pangaea.422528
title: Pigments and TOC of sediment core ARA-4/96-LL17

description: Knauer, Germany, with UV-Vis diode-array detector (Barspec Chrom-A-Scope) and fluorescence (Shimadzu RF-551) detector
DOI: 10.1594/pangaea.422532
title: Pigments of sediment core IOW211670-7

description: Knauer, Germany, with UV-Vis diode-array detector (Barspec Chrom-A-Scope) and fluorescence (Shimadzu RF-551) detector
DOI: 10.1594/pangaea.422530
title: Pigments and TOC of sediment core IOW009602-2GC-4

description: Knauer, Germany, with UV-Vis diode-array detector (Barspec Chrom-A-Scope) and fluorescence (Shimadzu RF-551) detector
DOI: 10.1594/pangaea.830234
title: Geochemistry of sediment core HYT
DOI: 10.1594/pangaea.385551
title: Nucleic acids in sediment core 12930-036
DOI: 10.1594/pangaea.720990
title: Pigments of sediment core 12930-087
DOI: 10.1594/pangaea.833896
title: (Table 3) Estimated concentrations of aromatic biomarkers and selected aromatic hydrocarbons ratios
DOI: 10.1594/pangaea.886227
title: Pigment concentrations in sediments from three stations (Faro, Creek, Isla D) in Potter Cove, Antarctic