ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • Data  (202)
  • 2020-2024  (202)
  • 1985-1989
  • 1955-1959
  • 2022  (202)
Collection
Keywords
Publisher
Years
  • 2020-2024  (202)
  • 1985-1989
  • 1955-1959
  • 2020-2023  (3)
Year
  • 1
    Publication Date: 2023-08-28
    Description: The study reported here involved the analysis of 12 rare earth and 13 minor elements in 13 nodules from the S.W. Pacific; 1 nodule from equatorial N. Pacific (DOMES Site C) as well as 1 nodule and 2 crusts from the Hawaiian-Emperor chain. After collection the samples were oven dried, ground with a pestle and mortar, and passed through a 50 ?m nylon sieve. The samples were prepared for spark source mass spectrometric analysis by mixing them in a ratio of 1:1, with ultra pure graphite powder. Pure Lu203 was mixed with the graphite (final concentration 500 ppm). The chemical analysis was performed by Spark Source Mass Spectrometry. Selected isotope images on the photoplate were used to determine the Q-2 emulsion response curve. The mass spectrometric data are considered to have a precision of ± 15% (based on repeat analyses of the U.S.G.S. standard BCR-1).
    Keywords: Arsenic; Barium; Caesium; CH10010; CH-100-76PC; CHA-281; CHA-285; Chain; Challenger1872; CK-76-1; Deposit type; DEPTH, sediment/rock; Description; DOMES Site C; Dredge; Dredge, pipe; Dredge, rock; DRG; DRG_P; DRG_R; Dysprosium; Elevation of event; ELT24; ELT24.002-RS; ELT24.015-RS; ELT24.017-RS; Eltanin; Erbium; Europium; Event label; FFGR; Free-fall grab; Gadolinium; Geochemistry; Grab; GRAB; H.M.S. Challenger (1872); Hafnium; Holmium; Identification; Kana Keoki; KK72; KK72MW-RD32; KK760806; KK760806-01,KK760806-02,KK76; KK760806-01-RD11; KK760806-01-RD7; Lanthanum; Latitude of event; Lead; Longitude of event; MANGANESE 76; manganese micronodule; manganese nodule; Method/Device of event; Method comment; Neodymium; Niobium; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; NZOI-Tangaroa_22; ocean; Pacific Ocean; PC; Piston corer; Praseodymium; RAV76-FFG14; RAV76-FFG6; RAV76-FFG8; Ravikai; RAVIKAI76; RNK-16; Rubidium; S03G06 (Station 3); S05G08 (Station 5); S11G14 (Station 11); Samarium; sediment; Shape; Size; Southern Ocean; South Pacific Ocean; Spark Source Mass Spectrometry; STA18; Strontium; TANG22-G1004C; TANG22-G994; TANG-76; TANG76I-140D; TANG76I-165A2; Tangaroa (1960); Terbium; Thorium; Tin; Uranium; Ytterbium; Yttrium; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 451 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2024-03-15
    Description: Ocean acidification (OA) poses a major threat to calcifying organisms such as reef-building corals, typically leading to reduced calcification rates. Mechanisms to compensate the effects of OA on coral growth may, however, involve processes other than calcification. Yet, the physiological patterns mediating coral growth under OA are not fully understood, despite an extensive body of literature characterizing physiological changes in corals under OA. Therefore, we conducted a three-month laboratory experiment with six scleractinian coral species (Acropora humilis, Acropora millepora, Pocillopora damicornis, Pocillopora verrucosa, Porites cylindrica, and Porites lutea) to assess physiological parameters that potentially characterize growth (calcification, volume, and surface area), maintenance (tissue biomass, and lipid and protein content), and cellular stress (apoptotic activity) response under ambient (pH 7.9) and low pH (pH 7.7). We identified genus- and species-specific physiological parameters potentially mediating the observed growth responses to low pH. We found no significant changes in calcification but species showed decreasing growth in volume and surface area, which occurred alongside changes in maintenance and cellular stress parameters that differed between genera and species. Acropora spp. showed elevated cellular stress and Pocillopora spp. showed changes in maintenance-associated parameters, while both genera largely maintained growth under low pH. Conversely, Porites spp. experienced the largest decreases in volume growth but showed no major changes in parameters related to maintenance or cellular stress. Our findings indicate that growth- and calcification-related responses alone may not fully reflect coral susceptibility to OA. They may also contribute to a better understanding of the complex physiological processes leading to differential growth changes of reef-building corals in response to low pH conditions.
    Keywords: Acropora humilis; Acropora millepora; Alkalinity, total; Alkalinity, total, standard deviation; Animalia; Apoptotic activity, per protein; Apoptotic activity, per protein, standard deviation; Aragonite saturation state; Aragonite saturation state, standard deviation; Benthic animals; Benthos; Bicarbonate ion; Calcification/Dissolution; Calcification rate, standard deviation; Calcification rate of calcium carbonate per month; Calcite saturation state; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Cnidaria; Coast and continental shelf; Containers and aquaria (20-1000 L or 〈 1 m**2); Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Growth/Morphology; Growth rate; Growth rate, standard deviation; Growth rate, volume per surface area; Laboratory experiment; Lipids, per ash free dry mass; Lipids, standard deviation; OA-ICC; Ocean Acidification International Coordination Centre; Other studied parameter or process; Partial pressure of carbon dioxide, standard deviation; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; pH, standard deviation; Pocillopora damicornis; Pocillopora verrucosa; Porites cylindrica; Porites lutea; Proteins, per ash free dry mass; Proteins, standard deviation; Replicates; Respiration; Salinity; Salinity, standard deviation; Single species; South Pacific; Species, unique identification; Species, unique identification (Semantic URI); Species, unique identification (URI); Temperature, water; Temperature, water, standard deviation; Tissue biomass; Tissue biomass, standard deviation; Treatment; Tropical; Type
    Type: Dataset
    Format: text/tab-separated-values, 600 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 3
    Publication Date: 2024-07-11
    Description: This dataset includes a global compilation of new and published 14C measurements of benthic foraminifera and deep-sea corals (from 0-to 49872 years BP). We synthesized this new dataset into basin-average 14C ventilation age values over the 25,000 years, along density surfaces associated with the upper and lower cells of global ocean overturning circulation (27.5 and 28 kg m^-3, respectively). The published datasets are from all ocean basins, even those not utilized in our synthesis. We also provide the basin-average estimates for the Atlantic, Southern, and Pacific Oceans as produced by the Rafter et al. 2022 study.
    Keywords: 0050PG; 0066PG; 145-883; 145-887; 146-893A; 167-1019A; 202-1240; 202-1242A; 341-U1419; 35MF20120125, OISO_21, INDIEN SUD 2; 47396B; 50-37KL; 64-480; 90b; AII125-8-55; AII125-8-56; Akademik M.A. Lavrentyev; ALV-3887-1549-004-007; ALV-3887-1549-004-009; ALV-3887-1549-004-012; ALV-3890-1407-003-001; ALV-3891-1459-003-002; ALV-3891-1758-006-003; AMOCINT, IMAGES XVII; ANT-XI/4; ANT-XXIII/9; ANT-XXVI/2; Argentine Basin; ARK-II/5; ARK-X/2; Azores; B34-91; BC; Bering Sea; Binary Object; BO04-PC11; Box corer; Brazil Basin; Burdwood_Bank; CALYPSO; CALYPSO2; Calypso Corer; Calypso Corer II; Calypso square corer; Calypso Square Core System; Canarias Sea; Cape_Horn; Caribbean Sea; CASQ; CASQS; CD159; CD159-10; CD159-15; CD159-17; CD38-17P; Celtic Sea; Cenderawasih Bay; Central Pacific; CH84-14; Charles Darwin; CHAT_10k; CHAT_16k; CHAT-3K; CHAT-5K; Chatham Rise; COMPCORE; Composite Core; Conrad Rise; Core; CORE; Core1471; Core2088; Core21210009; Core2307; Core2631; Core2657; Core2706; Core2774; Core47396; Core654; Core660; Core936; Corner Rise; Denmark Strait; Drake Passage; DRILL; Drilling/drill rig; Eastern Equatorial Pacific; Eastern slope of Kurile Basin; East Pacific; Emperor Seamounts; EN06601; EN066-39GGC; Endeavor; Equatorial East Pacific; ESTASE1; EW0408; EW0408-26JC; EW0408-85JC; EW0408-87JC; Exp341; F2-92-P3; F8-90-G21; File content; Galapagos; Galápagos Islands; GC; GC_POI; GeoB1503-1; GeoB2104-3; GeoB7149-2; GeoB7162-6; GeoB7163-7; GeoB7167-6; GGC; GGC5; gh02-1030; Giant box corer; Giant gravity corer; Giant piston corer; GIK17940-1; GIK23243-2 PS05/431; GKG; Glomar Challenger; GPC; Gravity corer; Gravity corer (Kiel type); Gravity corer (POI); GS07-150-17/1GC-A; GS07-150-20/2A; Gulf of Alaska; Gulf of California; H209; H213; HH12-946MC; HU72-021-7; HU89038-8PC; IMAGES III - IPHIS; IMAGES IV-IPHIS III; IMAGES V; IMAGES VIII - MONA; IMAGES VII - WEPAMA; IMAGES XII - MARCO POLO; IMAGES XV - Pachiderme; Indian Ocean; INOPEX; Interim_Seamount; Japan Trench; Jean Charcot; JM-FI-19PC; Joides Resolution; JPC; JPC30; JT96-09; JT96-09PC; Jumbo Piston Core; KAL; KALMAR II; Kasten corer; KL; KN_USA; KN11002; KN159-5; Knorr; KNR073-04-003; KNR110-50; KNR110-66; KNR110-82a; KNR110-82GGC; KNR140; KNR140-01JPC; KNR140-02JPC; KNR140-12JPC; KNR140-2-12JPC; KNR140-2-22JPC; KNR140-22JPC; KNR140-2-30GGC; KNR140-2-51GGC; KNR140-26GGC; KNR140-30GGC; KNR140-37JPC; KNR140-39GGC; KNR140-43GGC; KNR140-50GGC; KNR140-51GGC; KNR140-56GGC; KNR140-66GGC; KNR159-5; KNR159-5-36GGC; KNR159-5-78GGC; KNR176-17GC; KNR178; KNR178-2GGC; KNR178-32JPC; KNR195-5-CDH23; KNR195-5-CDH26; KNR195-5-CDH41; KNR195-5-GGC43; KNR197-10; KNR197-10CDH42; KNR197-10-CDH42; KNR197-10-CDH46; KNR197-10-GGC17; KNR197-10-GGC36; KNR197-10-GGC5; KNR198-CDH36; KNR198-GGC15; KNR31GPC5; KNR733P; KNR734P; KNR736P; KOL; KOMEX; KOMEX II; KR02-15-PC06; Kronotsky Peninsula; KT89-18-P4; Lakshadweep Sea; Laurentian fan; Leg145; Leg146; Leg167; Leg202; Leg64; Le Suroît; LPAZ21P; LV27/GREGORY; LV27-2-4; LV29-114-3; LV29-2; M16/2; M23/2; Marion Dufresne (1972); Marion Dufresne (1995); Maurice Ewing; Mazatlan; MCSEIS; MD012378; MD01-2378; MD012386; MD01-2386; MD012416; MD01-2416; MD012420; MD01-2420; MD022489; MD02-2489; MD022519; MD02-2519; MD03-2697; MD03-2707; MD052896; MD05-2896; MD052904; MD05-2904; MD07-3076; MD07-3076Q; MD07-3088; MD08-3169; MD08-3180; MD09-3256; MD09-3256Q; MD09-3257; MD106; MD111; MD114; MD122; MD12-3396Cq; MD126; MD13; MD134; MD147; MD159; MD168; MD173; MD189; MD77-176; MD972106; MD97-2106; MD972120; MD97-2120; MD972121; MD97-2121; MD972138; MD97-2138; MD982165; MD98-2165; MD982181; MD98-2181; MD99-2334; ME0005A; ME0005A-24JC; ME0005A-43JC; Melville; Meteor (1986); ML1208-01PC; MONITOR MONSUN; MR01-K03; MR06-04_PC04A; MUC; Multichannel seismics; MultiCorer; MV99-GC38; MV99-MC17/GC32/PC10; MV99-MC19/GC31/PC08; NEMO; Nesmeyanov25-1-GGC15; Nesmeyanov25-1-GGC18; Nesmeyanov25-1-GGC20; Nesmeyanov25-1-GGC27; New_England_Seamounts; North Atlantic; North Greenland Sea; North Pacific/Gulf of California/BASIN; North Pacific Ocean; Northwest Atlantic; Norwegian Sea; OCE326-GGC14; OCE326-GGC26; OCE326-GGC5; off Chile; off Nova Scotia; OSIRIS III; Pacific Ocean; PALEOCINAT; PC; Philippine Sea; PICABIA; Piston corer; Piston corer (BGR type); Piston corer (Kiel type); PLDS-007G; PLDS-1; Pleiades; Polarstern; PS05; PS1243-2; PS2606-6; PS2644-2; PS30; PS30/144; PS31; PS31/160; PS69; PS69/907-2; PS69/912-3; PS69/912-4; PS75/059-2; PS75/100-4; PS75/104-1; PS75 BIPOMAC; PUCK; RAPiD-10-1P; RAPiD-15-4P; RAPiD-17-5P; RBDASS05; RC24; RC24-8GC; RC27; RC27-14; RC27-23; Remote operated vehicle; RETRO-2; RNDB-GGC15; RNDB-GGC5; RNDB-PC11; RNDB-PC13; Robert Conrad; ROV; RR0503-36JPC; RR0503-41JPC; RR0503-64JPC; RR0503-79JPC; RR0503-831C; RR0503-83GC; S67-FFC15; S794; S931; Sakhalin shelf and slope; Sars_Seamount; Scotia Sea; Sea of Okhotsk; SEDCO; Sediment corer; Shackleton_Fracture_Zone; SHAK03-6K; SHAK05-3K; SHAK06-4K; SHAK06-5K; SHAK10-10K; SHAK14-4G; Shirshov Ridge; SK129-CR2; SL; Smithsonian_48735.1; SO156/2; SO156/3; SO161/3; SO161/3_22; SO178; SO178-13-6; SO201/2; SO201-2-101; SO201-2-12KL; SO201-2-77; SO201-2-85; SO202/1; SO202/1_18-6; SO213/2; SO213/2_76-2; SO213/2_79-2; SO213/2_82-1; SO213/2_84-1; SO95; Sonne; SOPATRA; South Atlantic; South Atlantic Ocean; South China Sea; Southern Alaska Margin: Tectonics, Climate and Sedimentation; South of Iceland; South Pacific Ocean; South Tasman Rise; Southwest Pacific Ocean; SPOC; Station 6, MD189-3396; SU90-08; Thomas G. Thompson (1964); Thomas Washington; Timor Sea; TNO57-21; TR163-22; TR163-23; TR163-31; TT154-10; TTN13-18; TTXXX; U938; V34; V34-98; V35; V35-5; V35-6; Vema; Vigo; VINO19-4-GGC17; VINO19-4-GGC37; VM21-29; VM21-30; VM23-81; VM28-122; VM28-238; VNTR01; VNTR01-10GC; W8709A; W8709A-13; Wecoma
    Type: Dataset
    Format: text/tab-separated-values, 8 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 4
    Publication Date: 2023-06-14
    Description: Abstract
    Description: We present an outstanding record of local, dense Large-N seismic and distributed acoustic sensor observations of a meteoroid from July 2, 2021 in Iceland. Our dataset includes high-quality observations from seven small aperture arrays of few hundred meters, an infrasound array, and a rotational station, all located within the distance range of 300 km. The high-frequency data show a variety of different phases associated with the source process along the atmospheric trajectory, including impulsive negative 1 first ground motions, a complex coda wave train about 2.5 s long thereafter, an azimuth-dependent stopping phase with reversed polarity between 1-25 s after the first arrival, which is resolved over only a few kilometers. The ground motion amplitude between the first and last arrivals is generally elevated. We associate the waveform in the 2.5 s coda with meteor-atmosphere interactions and nonlinear plasma processes that produce an oscillating shock-wave source pulse. Our data suggest a small azimuth-dependent deflection or dispersion of this source pulse, which may be related to the meteoroid’s deceleration in the atmosphere. We present a finite-length kinematic line-source pulse model that consistently explains the different phases inside and outside the Mach cone segment of our images, their wave amplitude variations, and a polarity change between the first phase and the terminating phase. The previously undiscovered rich directivity effects can also explain seemingly contradictory, time-dependent wave energy beam-directions at the various small aperture arrays and along the DAS cable. A combination of conventional locations and a Bayesian inversion of first and stopping phase arrivals led to a precise localization of the meteor trajectory.
    Keywords: Large-N seismometers networks ; Distributed fibre optic sensing ; EARTH SCIENCE 〉 SOLID EARTH 〉 ROCKS/MINERALS/CRYSTALS 〉 METEORITES ; EARTH SCIENCE 〉 SOLID EARTH 〉 ROCKS/MINERALS/CRYSTALS 〉 METEORITES 〉 METEORITE ORIGIN
    Type: Dataset , Dataset
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 5
    Publication Date: 2023-03-04
    Description: A total of 125 aerosol samples were analysed for their lithium concentrations and deposition flux. Daily aerosol samples were collected from the Pacific Ocean during CLIVAR-CO2 Repeat Hydrography Sections P16 and P2. The P16 section follows 150°-152°W and was divided into two legs, a southern leg from 17°S to 71°S in January-February 2005, and a northern leg from 16°S to 56°N in February-March 2006. CLIVAR-CO2 section P2 from Japan to San Diego, along 30°N, was visited in June-August 2004. The aerosol data from both CLIVAR-CO2 sections include aerosol lithium concentration measured following digestion in HF:HNO3:HCl mixture and corrected for sea-salt contributions (Li xs total), the P16 data also includes aerosol lithium extracted with ultrapure deionised water (≥18 MΩ) by pulling 100 mL of deionised water within ten seconds through the filter (Li xs MQ). Aerosol lithium deposition flux was calculated based on the local rain rate.
    Keywords: aerosol; Cruise/expedition; DATE/TIME; Indian Ocean; LATITUDE; Lithium; Lithium, flux; Lithium, soluble; LONGITUDE; Pacific Ocean; Precipitation, annual, mean; Sinking velocity
    Type: Dataset
    Format: text/tab-separated-values, 999 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 6
    Publication Date: 2023-01-13
    Description: Rock samples for TOC were dried at 40 ºC and then grounded to a fine powder with subsequent carbonate dissolution with HCl and organic-carbon combustion using a LECO WR 112 Carbon Analyser.
    Keywords: Carbon, organic, total; Carbon analyser, LECO; Depth, well; Espirito_Santo_Basin; Late Cretaceous; Milankovitch forcing; orbital tuning; South Atlantic; western South Atlantic
    Type: Dataset
    Format: text/tab-separated-values, 1026 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 7
    Publication Date: 2023-01-13
    Description: Well-log data was acquired in a Late Cretaceous section of the Espírito Santo basin (western South Atlantic). Cyclostratigraphic techniques were used to explore the eventual pacing of orbital cycles in the deposition of sequences. The frequency ratio method was used to interpret the orbital cycles and based on this a long-eccentricity signal was interpreted and extracted to create a floating time-scale. Using a seismic horizon associated Cretaceous-Paleogene transition, a strong shift in the natural gamma-ray data was anchored to an age of 66.0 Ma producing an anchored astronomical time-scale placed between late Albian and early Ypresian.
    Keywords: Late Cretaceous; Milankovitch forcing; orbital tuning; South Atlantic
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 8
    Publication Date: 2023-01-30
    Description: The Paleocene-Eocene Thermal Maximum (PETM) is the most pronounced climate event of the early Paleogene. It is characterized by negative δ18O and δ13C excursions recorded in sedimentary archives and a transient disruption of the marine biosphere. Bulk carbonate and foraminiferal δ13C records from Paleocene-Eocene core sections from the U.S. Atlantic Coastal Plain show an additional small, but distinct δ13C excursion below the onset of the PETM, coined the “pre-onset excursion” (POE). This study focuses on the South Dover Bridge (SDB) core in Maryland, where the Paleocene-Eocene transition is stratigraphically constrained by calcareous nannoplankton and stable isotope data, and in which the POE is well-expressed. The site was situated in a shallow marine shelf setting near a major outflow of the paleo-Potomac River system (38°44′49″N latitude, 76°00′25″W longitude, Talbot County). We generated high-resolution benthic foraminiferal assemblage, stable isotope, trace-metal, grain size and clay mineralogy data. Data collection was done via core-sampling, and successive preparation of the samples according to each proxy. Foraminifera underwent wet sieving (〉63 μm), picking and mounting on Plummer slides. For geochemistry analysis Cibicidoides alleni (Paleocene) and Anomalinoides acutus (PETM) were used. Grain size data was collected with a Laser Diffraction Particle Analyzer. Stable isotope samples were analyzed with a Kiel Mat 253 gas source mass spectrometer system. All carbon isotope values are given in δ13C notation, relative to the PeeDee belemnite Standard (PDB). Trace elemental analyses were carried out on a Thermo Scientific Element XR Sector Field Inductively Coupled Plasma Mass Spectrometer (SF-ICP-MS). For clay mineral analysis, after Jackson treatment, a Philips PW 1380 diffractometer equipped with CuKalpha radiation, 45kV and 30mA graphite monochromator and was quantified through Rietveld Refinement for clay content.
    Keywords: Benthic foraminifera; CaCO3 content; grainsize; kaolinite; Maryland; Mg/Ca; Mg/Ca paleothermometry; Paleocene; Paleocene-Eocene Thermal Maximum; PETM; POE; Pre-onset excursion; South Dover Bridge; Stable isotope; Taxonomy; U.S. Atlantic Coastal Plains
    Type: Dataset
    Format: application/zip, 10 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 9
    Publication Date: 2023-01-30
    Description: Sediment core LV53-27 (41° 54′ N, 132° 33′ E) was retrieved in the northwestern Sea of Japan (Pervenets Seamount) at 1698 m depth during a joint Russian-Chinese expedition LV53 on RV “Akademik M.A. Lavrentyev” in 2010-11-10T23:39:00. The 757-cm long core was characterized by clay/silty clay sediments with alternating dark and light layers. in order to investigate millenial-scale climate changes with ultra-high resolution digital image of this sediment core was processed. Sediment core LV53-27 recovered about 120 kyr according to age model (Gorbarenko et al., submitted to Global and Planetary Changes). Age model was based on correlation of magnetic susceptibility, chlorin content and lightness records with similar records of well-dated sediment core MD01-2407. The magnetic susceptibility (MS) of the sediments was measured in cube samples throughout the core at 2-cm intervals using an AGICO Kappabridge MFK1-FA. These measurements were performed at the Laboratory of Cenozoic Geology and Paleomagnetism of the North-East Interdisciplinary Scientific Research Institute in Magadan, Russia. Data presented as natural logarithm of units SI (International System of Units) Chlorin content was measured with pretreatment procedures and analytical reagents, as proposed by Harris et al. (1996), using a Shimadzu UV-1650PC spectrophotometer at 1 cm resolution. Color lightness (CL) of the sediments was measured using the original photocolorimeter based on a Canon 50D digital camera. One-meter core sections with 14 cm diameter were split into two halves, while performing surface smoothing. Two flash units with soft boxes were used for creating an even and diffused illumination of the sediment surface. Camera shooting was performed with the following settings: ISO 100, 1/100'' exposure, and 8.0 focal ratio. Every image covered approximately 40 cm of the core section with approximately 11 pixels per 1 mm stratigraphic resolution. The X-rite Color Checker was used for calibrating the white balance of each image. Digital images were processed with the RTImageProc software for calculating the CL data from black (0) to white (255) with 1-pixel resolution and averaged with 1 mm step. Need to note that the width of the analyzed window of each image (80 mm) in the studied core allow to significantly reduce the possible effect of the sediment bioturbation by organisms several millimeters in diameter.
    Keywords: chlorin content; color lightness; LV53-27; magnetic susceptibility; Sea of Japan
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 10
    Publication Date: 2023-01-30
    Description: Makrozoobenthic communties were collected at multiple at different depth of wind turbines. Samples were taken by scraping the organisms from the turbines into a net (scrape samples) by scuba divers to analyse the epifaunal communities. Samples were collected in three different wind farms: DanTysk (sampled in 2018, 2019) and Sandbank (2019) in the German exclusive economic zone (EEZ) and Horns Rev (2003-2005) in the Danish EEZ. Epifaunal community was evaluated for recording successional stages of growth on the wind turbines in different depth to cover the vertical zonation along the turbines. The data are part of the Danish monitoring data on offshore wind farms and the German Standard Investigation of the Impacts of Offshore Wind Turbines on the Marine Environment (StUK 4, published by BSH 2014). Data for each campaign comprise different turbines in the wind farms sampled by scuba divers using scrape samples. Biodiversity data of species include abundance (count data) and biomass (wet mass, g) per sample. Data were collected on behalf of Vattenfall in the framework of the mandatory monitoring. Thus we would like to thank Vattenfall who kindly provided the data for scientific independent research analysis and publication.
    Keywords: Area; artificial hard substrate; benthic communities; Campaign; DATE/TIME; DEPTH, water; Event label; Gear; German Bight; Habitat; HR_3_2003; HR_3_2003/HORN_T33_9.2_3/2003-T33/2003/03_9.2m_S1a; HR_3_2003/HORN_T33_9.2_3/2003-T33/2003/03_9.2m_S1b; HR_3_2003/HORN_T33_9.2_3/2003-T33/2003/03_9.2m_S1c; HR_3_2003/HORN_T33_9.2_3/2003-T33/2003/03_9.2m_S1d; HR_3_2003/HORN_T33_9.2_3/2003-T33/2003/03_9.2m_S2a; HR_3_2003/HORN_T33_9.2_3/2003-T33/2003/03_9.2m_S2b; HR_3_2003/HORN_T33_9.2_3/2003-T33/2003/03_9.2m_S2c; HR_3_2003/HORN_T33_9.2_3/2003-T33/2003/03_9.2m_S2d; HR_3_2003/HORN_T33_9.2_3/2003-T33/2003/03_9.2m_S3a; HR_3_2003/HORN_T33_9.2_3/2003-T33/2003/03_9.2m_S3b; HR_3_2003/HORN_T33_9.2_3/2003-T33/2003/03_9.2m_S3c; HR_3_2003/HORN_T33_9.2_3/2003-T33/2003/03_9.2m_S3d; HR_3_2003/HORN_T55_0.2_3/2003-T55/2003/03_0.2m_S1; HR_3_2003/HORN_T55_0.2_3/2003-T55/2003/03_0.2m_S1_; HR_3_2003/HORN_T55_0.2_3/2003-T55/2003/03_0.2m_S2; HR_3_2003/HORN_T55_0.2_3/2003-T55/2003/03_0.2m_S2_; HR_3_2003/HORN_T55_2.2_3/2003-T55/2003/03_2.2m_S1a; HR_3_2003/HORN_T55_2.2_3/2003-T55/2003/03_2.2m_S1b; HR_3_2003/HORN_T55_2.2_3/2003-T55/2003/03_2.2m_S2a; HR_3_2003/HORN_T55_2.2_3/2003-T55/2003/03_2.2m_S2b; HR_3_2003/HORN_T55_4.2_3/2003-T55/2003/03_4.2m_S1a; HR_3_2003/HORN_T55_4.2_3/2003-T55/2003/03_4.2m_S1b; HR_3_2003/HORN_T55_4.2_3/2003-T55/2003/03_4.2m_S2a; HR_3_2003/HORN_T55_4.2_3/2003-T55/2003/03_4.2m_S2b; HR_3_2003/HORN_T55_6.2_3/2003-T55/2003/03_6.2m_S1a; HR_3_2003/HORN_T55_6.2_3/2003-T55/2003/03_6.2m_S1b; HR_3_2003/HORN_T55_6.2_3/2003-T55/2003/03_6.2m_S2a; HR_3_2003/HORN_T55_6.2_3/2003-T55/2003/03_6.2m_S2b; HR_3_2003/HORN_T55_8.2_3/2003-T55/2003/03_8.2m_S1a; HR_3_2003/HORN_T55_8.2_3/2003-T55/2003/03_8.2m_S1b; HR_3_2003/HORN_T55_8.2_3/2003-T55/2003/03_8.2m_S1c; HR_3_2003/HORN_T55_8.2_3/2003-T55/2003/03_8.2m_S1d; HR_3_2003/HORN_T55_8.2_3/2003-T55/2003/03_8.2m_S1e; HR_3_2003/HORN_T55_8.2_3/2003-T55/2003/03_8.2m_S1f; HR_3_2003/HORN_T55_8.2_3/2003-T55/2003/03_8.2m_S2a; HR_3_2003/HORN_T55_8.2_3/2003-T55/2003/03_8.2m_S2b; HR_3_2003/HORN_T55_8.2_3/2003-T55/2003/03_8.2m_S2c; HR_3_2003/HORN_T55_8.2_3/2003-T55/2003/03_8.2m_S2d; HR_3_2003/HORN_T55_8.2_3/2003-T55/2003/03_8.2m_S2e; HR_3_2003/HORN_T55_8.2_3/2003-T55/2003/03_8.2m_S2f; HR_3_2003/HORN_T55_8.2_3/2003-T55/2003/03_8.2m_S3a; HR_3_2003/HORN_T55_8.2_3/2003-T55/2003/03_8.2m_S3b; HR_3_2003/HORN_T55_8.2_3/2003-T55/2003/03_8.2m_S3c; HR_3_2003/HORN_T55_8.2_3/2003-T55/2003/03_8.2m_S3d; HR_3_2003/HORN_T58_1.1_3/2003-T58/2003/03_1.1m_S1a; HR_3_2003/HORN_T58_1.1_3/2003-T58/2003/03_1.1m_S1b; HR_3_2003/HORN_T58_1.1_3/2003-T58/2003/03_1.1m_S2a; HR_3_2003/HORN_T58_1.1_3/2003-T58/2003/03_1.1m_S2b; HR_3_2003/HORN_T58_3.1_3/2003-T58/2003/03_3.1m_S1a; HR_3_2003/HORN_T58_3.1_3/2003-T58/2003/03_3.1m_S1b; HR_3_2003/HORN_T58_3.1_3/2003-T58/2003/03_3.1m_S2a; HR_3_2003/HORN_T58_3.1_3/2003-T58/2003/03_3.1m_S2b; HR_3_2003/HORN_T58_5.1_3/2003-T58/2003/03_5.1m_S1a; HR_3_2003/HORN_T58_5.1_3/2003-T58/2003/03_5.1m_S1b; HR_3_2003/HORN_T58_5.1_3/2003-T58/2003/03_5.1m_S2a; HR_3_2003/HORN_T58_5.1_3/2003-T58/2003/03_5.1m_S2b; HR_3_2003/HORN_T58_7.1_3/2003-T58/2003/03_7.1m_S1a; HR_3_2003/HORN_T58_7.1_3/2003-T58/2003/03_7.1m_S1b; HR_3_2003/HORN_T58_7.1_3/2003-T58/2003/03_7.1m_S1c; HR_3_2003/HORN_T58_7.1_3/2003-T58/2003/03_7.1m_S1d; HR_3_2003/HORN_T58_7.1_3/2003-T58/2003/03_7.1m_S1e; HR_3_2003/HORN_T58_7.1_3/2003-T58/2003/03_7.1m_S1f; HR_3_2003/HORN_T58_7.1_3/2003-T58/2003/03_7.1m_S2a; HR_3_2003/HORN_T58_7.1_3/2003-T58/2003/03_7.1m_S2b; HR_3_2003/HORN_T58_7.1_3/2003-T58/2003/03_7.1m_S2c; HR_3_2003/HORN_T58_7.1_3/2003-T58/2003/03_7.1m_S2d; HR_3_2003/HORN_T58_7.1_3/2003-T58/2003/03_7.1m_S2e; HR_3_2003/HORN_T58_7.1_3/2003-T58/2003/03_7.1m_S2f; HR_3_2003/HORN_T58_7.1_3/2003-T58/2003/03_7.1m_S3a; HR_3_2003/HORN_T58_7.1_3/2003-T58/2003/03_7.1m_S3b; HR_3_2003/HORN_T58_7.1_3/2003-T58/2003/03_7.1m_S3c; HR_3_2003/HORN_T58_7.1_3/2003-T58/2003/03_7.1m_S3d; HR_3_2003/HORN_T91_5.5_3/2003-T91/2003/03_5.5m_S1a; HR_3_2003/HORN_T91_5.5_3/2003-T91/2003/03_5.5m_S1b; HR_3_2003/HORN_T91_5.5_3/2003-T91/2003/03_5.5m_S1c; HR_3_2003/HORN_T91_5.5_3/2003-T91/2003/03_5.5m_S1d; HR_3_2003/HORN_T91_5.5_3/2003-T91/2003/03_5.5m_S2a; HR_3_2003/HORN_T91_5.5_3/2003-T91/2003/03_5.5m_S2b; HR_3_2003/HORN_T91_5.5_3/2003-T91/2003/03_5.5m_S2c; HR_3_2003/HORN_T91_5.5_3/2003-T91/2003/03_5.5m_S2d; HR_3_2003/HORN_T91_5.5_3/2003-T91/2003/03_5.5m_S3a; HR_3_2003/HORN_T91_5.5_3/2003-T91/2003/03_5.5m_S3b; HR_3_2003/HORN_T91_5.5_3/2003-T91/2003/03_5.5m_S3c; HR_3_2003/HORN_T91_5.5_3/2003-T91/2003/03_5.5m_S3d; HR_3_2003/HORN_T92_5.7_3/2003-T92/2003/03_5.7m_S1a; HR_3_2003/HORN_T92_5.7_3/2003-T92/2003/03_5.7m_S1b; HR_3_2003/HORN_T92_5.7_3/2003-T92/2003/03_5.7m_S1c; HR_3_2003/HORN_T92_5.7_3/2003-T92/2003/03_5.7m_S1d; HR_3_2003/HORN_T92_5.7_3/2003-T92/2003/03_5.7m_S2a; HR_3_2003/HORN_T92_5.7_3/2003-T92/2003/03_5.7m_S2b; HR_3_2003/HORN_T92_5.7_3/2003-T92/2003/03_5.7m_S2c; HR_3_2003/HORN_T92_5.7_3/2003-T92/2003/03_5.7m_S3a; HR_3_2003/HORN_T92_5.7_3/2003-T92/2003/03_5.7m_S3b; HR_3_2003/HORN_T92_5.7_3/2003-T92/2003/03_5.7m_S3c; HR_3_2003/HORN_T92_5.7_3/2003-T92/2003/03_5.7m_S3d; HR_3_2003/HORN_T95_0_3/2003-T95/2003/03_0m_S1a; HR_3_2003/HORN_T95_0_3/2003-T95/2003/03_0m_S1a_1_1; HR_3_2003/HORN_T95_0_3/2003-T95/2003/03_0m_S1b; HR_3_2003/HORN_T95_0_3/2003-T95/2003/03_0m_S1b_1_1; HR_3_2003/HORN_T95_0_3/2003-T95/2003/03_0m_S2a; HR_3_2003/HORN_T95_0_3/2003-T95/2003/03_0m_S2a_1_1; HR_3_2003/HORN_T95_0_3/2003-T95/2003/03_0m_S2b; HR_3_2003/HORN_T95_0_3/2003-T95/2003/03_0m_S2b_1_1; HR_3_2003/HORN_T95_1.3_3/2003-T95/2003/03_1.3m_S1a; HR_3_2003/HORN_T95_1.3_3/2003-T95/2003/03_1.3m_S1b; HR_3_2003/HORN_T95_1.3_3/2003-T95/2003/03_1.3m_S2a; HR_3_2003/HORN_T95_1.3_3/2003-T95/2003/03_1.3m_S2b; HR_3_2003/HORN_T95_3.3_3/2003-T95/2003/03_3.3m_S1a; HR_3_2003/HORN_T95_3.3_3/2003-T95/2003/03_3.3m_S1b; HR_3_2003/HORN_T95_3.3_3/2003-T95/2003/03_3.3m_S2a; HR_3_2003/HORN_T95_3.3_3/2003-T95/2003/03_3.3m_S2b; HR_3_2003/HORN_T95_5.3_3/2003-T95/2003/03_5.3m_S1a; HR_3_2003/HORN_T95_5.3_3/2003-T95/2003/03_5.3m_S1b; HR_3_2003/HORN_T95_5.3_3/2003-T95/2003/03_5.3m_S2a; HR_3_2003/HORN_T95_5.3_3/2003-T95/2003/03_5.3m_S2b; HR_3_2003/HORN_T95_7.3_3/2003-T95/2003/03_7.3m_S1a; HR_3_2003/HORN_T95_7.3_3/2003-T95/2003/03_7.3m_S1b; HR_3_2003/HORN_T95_7.3_3/2003-T95/2003/03_7.3m_S1c; HR_3_2003/HORN_T95_7.3_3/2003-T95/2003/03_7.3m_S1d; HR_3_2003/HORN_T95_7.3_3/2003-T95/2003/03_7.3m_S1e; HR_3_2003/HORN_T95_7.3_3/2003-T95/2003/03_7.3m_S1f; HR_3_2003/HORN_T95_7.3_3/2003-T95/2003/03_7.3m_S2a; HR_3_2003/HORN_T95_7.3_3/2003-T95/2003/03_7.3m_S2b; HR_3_2003/HORN_T95_7.3_3/2003-T95/2003/03_7.3m_S2c; HR_3_2003/HORN_T95_7.3_3/2003-T95/2003/03_7.3m_S2d; HR_3_2003/HORN_T95_7.3_3/2003-T95/2003/03_7.3m_S2e; HR_3_2003/HORN_T95_7.3_3/2003-T95/2003/03_7.3m_S2f; HR_3_2003/HORN_T95_7.3_3/2003-T95/2003/03_7.3m_S3a; HR_3_2003/HORN_T95_7.3_3/2003-T95/2003/03_7.3m_S3b; HR_3_2003/HORN_T95_7.3_3/2003-T95/2003/03_7.3m_S3c; HR_3_2003/HORN_T95_7.3_3/2003-T95/2003/03_7.3m_S3d; HR_3_2004; HR_3_2004/HORN_T33_9.2_3/2004-T33/2004/03_9.2m_S1a; HR_3_2004/HORN_T33_9.2_3/2004-T33/2004/03_9.2m_S1b; HR_3_2004/HORN_T33_9.2_3/2004-T33/2004/03_9.2m_S1c; HR_3_2004/HORN_T33_9.2_3/2004-T33/2004/03_9.2m_S1d; HR_3_2004/HORN_T33_9.2_3/2004-T33/2004/03_9.2m_S2a; HR_3_2004/HORN_T33_9.2_3/2004-T33/2004/03_9.2m_S2b; HR_3_2004/HORN_T33_9.2_3/2004-T33/2004/03_9.2m_S2c; HR_3_2004/HORN_T33_9.2_3/2004-T33/2004/03_9.2m_S2d; HR_3_2004/HORN_T33_9.2_3/2004-T33/2004/03_9.2m_S3a; HR_3_2004/HORN_T33_9.2_3/2004-T33/2004/03_9.2m_S3b; HR_3_2004/HORN_T33_9.2_3/2004-T33/2004/03_9.2m_S3c; HR_3_2004/HORN_T33_9.2_3/2004-T33/2004/03_9.2m_S3d; HR_3_2004/HORN_T55_0.2_3/2004-T55/2004/03_0.2m_S1a; HR_3_2004/HORN_T55_0.2_3/2004-T55/2004/03_0.2m_S1b; HR_3_2004/HORN_T55_0.2_3/2004-T55/2004/03_0.2m_S2a; HR_3_2004/HORN_T55_0.2_3/2004-T55/2004/03_0.2m_S2b; HR_3_2004/HORN_T55_2.2_3/2004-T55/2004/03_2.2m_S1a; HR_3_2004/HORN_T55_2.2_3/2004-T55/2004/03_2.2m_S1b; HR_3_2004/HORN_T55_2.2_3/2004-T55/2004/03_2.2m_S2a; HR_3_2004/HORN_T55_2.2_3/2004-T55/2004/03_2.2m_S2b; HR_3_2004/
    Type: Dataset
    Format: text/tab-separated-values, 133418 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...