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  • 1
    Monograph available for loan
    Monograph available for loan
    Cambridge : Cambridge University Press
    Call number: PIK 24-95731
    Type of Medium: Monograph available for loan
    Pages: xviii, 270 Seiten , Illustrationen, Diagramme, Karten , 25 cm
    Edition: Third edition
    ISBN: 9781108793872 , 9781108840187
    Language: English
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 2
    Publication Date: 2024-06-06
    Description: Ocean acidification and warming are challenging marine organisms and ecosystems around the world. The synergetic effects of these two climate change stressors on jellyfish remain still understudied. Here, we examine the independent and combined effects of these two environmental variables on polyp population dynamics of the Mediterranean jellyfish Cotylorhiza tuberculata. An experiment was conducted to examine asexual reproduction by budding and strobilation considering current and ca. 2100 winter (Trial 1, 36 days) and summer (Trial 2, 36 days) conditions under the RCP8.5 (IPCC 2013). In Trial 1, a temperature of 18°C and two pH levels (current: 7.9 and, reduced: 7.7) were tested. Trial 2 considered two temperature levels 24°C and 30°C, under current and reduced acidification conditions (8.0 and 7.7, respectively). Ephyrae size and statolith formation of released ephyrae from polyps exposed to summer temperatures under both acidification treatment was also analyzed. Zooxanthellae density inside the polyps throughout the experiment was measured. C. tuberculata polyps could cope with the conditions mimicked in all experimental treatments and no significant effect of pH, temperature, or the combination of both variables on the abundance of polyps was observed. At 18°C, strobilation was reduced under high PCO2 conditions. Under summer treatments (24°C and 30°C), percentage strobilation was very low and several released ephyrae suffered malformations and reduced size, as a consequence of reduced pH and elevated temperatures, separately. The number of statoliths was not affected by pH or temperature, however, bigger statoliths were formed at elevated temperatures (30°C). Finally, zooxanthellae density was not affected by experimental conditions, even if, the duration of the experiment significantly affected symbiont concentration. Our results show that even though polyps of C. tuberculata would thrive the future worst scenario predicted for the Mediterranean Sea, their capacity to undergo a proper strobilation and to produce healthy ephyrae will be more vulnerable to climate induced environmental conditions, thereby affecting medusae recruitment and, therefore, population dynamics of the species.
    Keywords: Alkalinity, total; Alkalinity, total, standard error; Animalia; Aragonite saturation state; Arms; Bicarbonate ion; Bottle number; Bottles or small containers/Aquaria (〈20 L); 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; Cotylorhiza tuberculata; Day of experiment; Diameter; Ephyra size; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Identification; Laboratory experiment; Laboratory strains; Nekton; Nitrate; Nitrate, standard error; Not applicable; Number; OA-ICC; Ocean Acidification International Coordination Centre; Oxygen, dissolved; Oxygen, dissolved, standard error; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Partial pressure of carbon dioxide (water) at sea surface temperature (wet air), standard error; Pelagos; pH; pH, standard error; Polyp number; Potentiometric titration; Registration number of species; Reproduction; Salinity; Silicate, standard error; Silicate [SiO3]2-; Single species; Species; Spectrophotometric; Statolith, length; Statolith, number; Statolith, volume; Statolith, width; Symmetry index; Temperature; Temperature, water; Temperature, water, standard error; Time in days; Treatment; Treatment: temperature; Type; Uniform resource locator/link to reference; Zooxanthellae
    Type: Dataset
    Format: text/tab-separated-values, 71985 data points
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  • 3
    Publication Date: 2024-06-06
    Description: The values of carbon remineralisation were measured in juveniles/adults of 5 non-migratory bristlemouth fishes (Cyclothone spp.) and partial migrator (Argyropelecus hemigymnus) sampled during the BATHYPELAGIC cruise (North Atlantic, June 2018). This dataset contains the values of numerical abundance, biomass, specific ETS activity, specific respiraton and respiration flux data analyzed from Northwest Africa (20° N, 20° W) to the South of Iceland. A. hemigymnus specimens were collected using a ''Mesopelagos” net (5 x7 m mouth opening, 58 m total length) equipped with graded-mesh netting (starting with 30 mm and ending with 4 mm) and a multi-sampler for collecting samples from 5 different depth layers (Olivar et al., 2017). However, Cyclothone specimens were collected using the Multiple Opening/Closing Net and Environmental Sensing System (MOCNESS-1 m²) zooplankton net (Wiebe et al., 1985) with a 0.2 mm mesh size and with several nets for collecting samples from 8 different depth layers. The Mesopelagos catches were sorted out and identified on board to the lowest possible taxon, and specimens selected for Electron Transfer System (ETS) analyses were immediately frozen in liquid nitrogen for later analysis in the laboratory. MOCNESS samples were preserved in 5% buffered formalin, and specimens were sorted out later in the laboratory. Stomiiforms respiration in the meso- and bathypelagic zones of the ocean were estimated along the transect. Abundance, biomass, specific ETS activity, specific respiration and respiration are given by layer.
    Keywords: 1; 10; 2; 29SG20180524; 3; 4; 5; 6; 7; Abundance per area; bathypelagic; BATHYPELAGIC; BATHYPELAGIC_01_D-3; BATHYPELAGIC_01_N-2; BATHYPELAGIC_01_N-3; BATHYPELAGIC_02_D-2; BATHYPELAGIC_02_N-2; BATHYPELAGIC_03_D-2; BATHYPELAGIC_03_D-3; BATHYPELAGIC_03_N-2; BATHYPELAGIC_03_N-3; BATHYPELAGIC_04_D-3; BATHYPELAGIC_04_N-2; BATHYPELAGIC_04_N-3; BATHYPELAGIC_05_D-2; BATHYPELAGIC_05_D-3; BATHYPELAGIC_05_N-2; BATHYPELAGIC_05_N-3; BATHYPELAGIC_06_D-2; BATHYPELAGIC_06_D-3; BATHYPELAGIC_06_N-2; BATHYPELAGIC_06_N-3; BATHYPELAGIC_07_D-2; BATHYPELAGIC_07_D-3; BATHYPELAGIC_07_N-2; BATHYPELAGIC_07_N-3; BATHYPELAGIC_10_D-3; BATHYPELAGIC_10_N-3; biological carbon pump; Biomass and Active Flux in the Bathypelagic Zone; Calculated; Carbon; Date/Time of event; Depth, bathymetric; DEPTH, water; Electron transport system activity of oxygen per mass; Event label; fish; ICM_Excellence_Centre; Latitude of event; Longitude of event; mesopelagic; Mesopelagos; Micronekton, biomass as carbon; Midwater trawl, Mesopelagos (Meillat, 2012); MOC1; MOCNESS opening/closing plankton net 1 sqm; North Atlantic; Northeast Atlantic; Optional event label; remineralization; Respiration; respiration flux; Respiration rate, carbon; Sarmiento de Gamboa; Severo Ochoa Centre of Excellence; Species, unique identification; Species, unique identification (Semantic URI); Species, unique identification (URI); SUMMER; Sustainable Management of Mesopelagic Resources; Temperature, water, mean; Tetrazolium reduction technique according to Packard (1971); Time of day; TRIATLAS; Tropical and South Atlantic climate-based marine ecosystem predictions for sustainable management; VID; Visual identification
    Type: Dataset
    Format: text/tab-separated-values, 856 data points
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  • 4
    Publication Date: 2024-06-06
    Description: Physical oceanography variables and carbon remineralisation (juveniles/adults of Cyclothone species and Argyropelecus hemigymnus) were analysed during the BATHYPELAGIC cruise (North Atlantic, June 2018). This dataset contains the depth, temperature, and conductivity which were recorded from surface to a maximum depth of 2000 m using a SeaBird SBE 25plus CTD equipped with a Seabird-43 Dissolved Oxygen sensor and a Seapoint Fluorometer. Values of numerical abundance, biomass, specific ETS activity, specific respiraton and respiration flux data analyzed from Northwest Africa (20° N, 20° W) to the South of Iceland are presented. A. hemigymnus specimens were collected using a ''Mesopelagos” net (5 x7 m mouth opening, 58 m total length) equipped with graded-mesh netting (starting with 30 mm and ending with 4 mm) and a multi-sampler for collecting samples from 5 different depth layers. However, Cyclothone specimens were collected using the Multiple Opening/Closing Net and Environmental Sensing System (MOCNESS-1 m²) zooplankton net with a 0.2 mm mesh size and with several nets for collecting samples from 8 different depth layers. The Mesopelagos catches were sorted out and identified on board to the lowest possible taxon, and specimens selected for Electron Transfer System (ETS) analyses were immediately frozen in liquid nitrogen for later analysis in the laboratory. MOCNESS samples were preserved in 5% buffered formalin, and specimens were sorted out later in the laboratory. Stomiiforms respiration in the meso- and bathypelagic zones of the ocean were estimated along the transect. Abundance, biomass, specific ETS activity, specific respiration and respiration are given by layer between e.g. 100 m and 1000 m depth (MOCNESS net, 1900–1600 m, 1600–1300 m, 1300–1000 m, 1000–700 m, 700–400 m, 400–200 m, 200–100 m and 100–0 m; Mesopelagos, 1900–1200 m, 1200–800 m, 800–500 m, 500–200 m and 200–0 m).
    Keywords: bathypelagic; BATHYPELAGIC; biological carbon pump; Biomass and Active Flux in the Bathypelagic Zone; Carbon; fish; ICM_Excellence_Centre; mesopelagic; Northeast Atlantic; remineralization; respiration flux; Severo Ochoa Centre of Excellence; SUMMER; Sustainable Management of Mesopelagic Resources; TRIATLAS; Tropical and South Atlantic climate-based marine ecosystem predictions for sustainable management
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 5
    Publication Date: 2024-06-06
    Description: These datasets provide sedimentological data partly at annual resolution and an age model for the lateglacial part of (1) the ICDP sediment core 5017-1-A retrieved from the deep northern Dead Sea basin in 2010/11, and (2) for the Masada outcrop located at the southwestern shore of the Dead Sea sampled in 2018. The here investigated two sediment sections cover the last glacial-interglacial transition (ca. 17-11.5 ka BP) in the hydroclimatically sensitive Levant, when the water level of Lake Lisan – the precursor of the Dead Sea – dropped dramatically from its glacial high-stand to the Holocene low levels. Here, we analyze the interval between the last two gypsum units – the Upper Gypsum Unit (UGU) and the Additional Gypsum Unit (AGU) – which were also used to correlate the two sites. In the ICDP core this section is located between ~101 and 88.5 m sediment depth below lake floor and at Masada it encompasses the uppermost ~3.8 m sediments of the Lisan Formation, which form the terminal deposit at this site. Due to the lake level decline, the complete transition into the Holocene is only recorded in the ICDP core, while sedimentation at Masada terminates earlier. The microfacies was investigated by continuous thin section microscopy, while additional macroscopic information is provided from over- and underlying sediment sections. A revised chronology using age modelling in OxCal (Ramsey 2008; Ramsey 2009; Ramsey and Lee 2013) was developed for the ICDP core and a floating varve chronology was constructed at Masada. Using these new microfacies data from marginal (Masada) and deep-water (ICDP core) sediments, the hydroclimatic variability during the final stage of Lake Lisan can be reconstructed, which could provide important insights into the development of human sedentism in the region at this time.
    Keywords: Dead Sea; Eastern Mediterranean; ICDP; International Continental Scientific Drilling Program; Lateglacial; microfacies analyses; Paleoclimate; varve chronology
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 6
    Publication Date: 2024-06-06
    Description: This dataset provides the results from Bayesian age depth modelling in OxCal for ICDP core 5017-1-A, retrieved from the deep northern Dead Sea basin in 2010/11, for the last glacial-interglacial transition between ~101 and 88.5 m sediment depth below lake floor (ca. 17-11.5 ka BP). The model was performed in OxCal v.4.4 using a P_Sequence (1,1,C(-2,2)) (Ramsey 2008; Ramsey 2009; Ramsey and Lee 2013) and includes three tephrochronological ages from Neugebauer et al. (2021) and three radiocarbon ages from Kitagawa et al. (2017).
    Keywords: AGE; Age, uncertainty maximum/old; Age, uncertainty minimum/young; CDRILL; Core drilling; Dead Sea; Dead Sea Basin, Israel; DEPTH, sediment/rock; DSDDP_5017-1-A; Eastern Mediterranean; ICDP; International Continental Scientific Drilling Program; Lateglacial; microfacies analyses; Paleoclimate; varve chronology
    Type: Dataset
    Format: text/tab-separated-values, 5636 data points
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  • 7
    Publication Date: 2024-06-06
    Description: This dataset contains measurements of global radiation, precipitation, air temperature, relative humidity, air pressure, wind speed and wind direction from the study area of the project Dendromass4Europe. The aim of the study was to determine the influence of meteorological and soil-related site conditions on tree transpiration rates in poplar short rotation coppices plantations. In June 2018 a meteorological station was installed. The measurements started in June 2018 with a resolution of 30 minutes until end of May 2022 (31.05.2022). Three poplar SRC stands were selected according to a gradient of groundwater accessibility: S5-N (higher groundwater level), S4-D (low groundwater level), and S2-F (fluctuating groundwater level). On each of the selected sites one soil profile was excavated and prepared for the installation of soil sensors. The meteorological station was located southwest from the experimental sites. The distance from the meteorological station to the experimental sites was: 9.56 km to site S5-N (higher groundwater table), 9.82 km to site S4-D (low groundwater level), and 6.57 km to site S2-F (fluctuating groundwater table).
    Keywords: D4EU-Dendromass4Europe; DATE/TIME; HEIGHT above ground; Humidity, relative; Kalyx Rain Gauge (EML Ltd.), receiver tank area 127 cm2 and a resolution of 0.2 mm per tip; Kopcany2018-2022; MON; Monitoring; Precipitation; Pyranometer Sensor, SP-110 Apogee; Sampling on land; Securing Sustainable Dendromass Production with Poplar Plantations in European Rural Areas; Short-wave downward (GLOBAL) radiation; SK-Land-2018-2022_Kopcany; Station pressure; Temperature, air; Wind direction; Wind speed, hourly mean; WS500-UMB Smart Weather Sensor
    Type: Dataset
    Format: text/tab-separated-values, 207350 data points
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  • 8
    Publication Date: 2024-06-06
    Description: Depth, temperature, and conductivity were recorded during the Bathypelagic cruise (from 24th May to 23rd June 2018,) using a SeaBird SBE 25plus CTD, the dissolved oxygen with a Seabird-43 sensor both attached to an oceanographic rosette from surface to a maximum depth of 2000 m, and the fluorometer with a Seapoint sensor in the upper 200 m depth.
    Keywords: 1; 10; 2; 29SG20180524; 3; 4; 5; 6; 7; 8; 9; bathypelagic; BATHYPELAGIC; BATHYPELAGIC_01-1; BATHYPELAGIC_02-1; BATHYPELAGIC_03-1; BATHYPELAGIC_04-1; BATHYPELAGIC_05-1; BATHYPELAGIC_06-1; BATHYPELAGIC_07-1; BATHYPELAGIC_08-1; BATHYPELAGIC_09-1; BATHYPELAGIC_10-1; biological carbon pump; Biomass and Active Flux in the Bathypelagic Zone; Carbon; Chlorophyll a; Chlorophyll fluorometer, Seapoint, Seapoint chlorophyll fluorometer; CTD, Sea-Bird, SBE 25plus; Date/Time of event; DEPTH, water; Event label; fish; ICM_Excellence_Centre; Latitude of event; Longitude of event; mesopelagic; North Atlantic; Northeast Atlantic; Optional event label; Oxygen, dissolved; Oxygen sensor, SBE 43; remineralization; respiration flux; Salinity; Sarmiento de Gamboa; Severo Ochoa Centre of Excellence; SUMMER; Sustainable Management of Mesopelagic Resources; Temperature, water; TRIATLAS; Tropical and South Atlantic climate-based marine ecosystem predictions for sustainable management
    Type: Dataset
    Format: text/tab-separated-values, 61749 data points
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  • 9
    Publication Date: 2024-06-05
    Description: The high surface productivity triggered by nutrient-rich Benguela upwelled waters results in significant enrichment of organic carbon in the sub-surface waters due to enhanced mineralization in the water column and benthic fluxes. Hence, microbial O2-consuming processes are promoted, driving oxygen depletion that favors trace gases i.e. methane (CH4) and nitrous oxide (N2O) production at relatively shallow depths. During upwelling, gas-rich subsurface waters are also transported towards the surface waters, enhancing trace gas sea-air fluxes. We investigate the variability of these fluxes on seasonal and shorter timescales to understand the intensity of the Benguela upwelling system in gas emissions. The data might serve as a base for projections under a changing climate. The fieldwork took place during the cruise M157 (August 4th – September 16th, 2019) onboard the R/V METEOR, which encompassed close-coastal and open ocean regions between Mindelo (Cape Verde) and Walvis Bay. The main transect lines around 18, 23 and 25°S represents the Angola-Benguela frontal zone, Walvis Bay and Lüderitz upwelling cells respectively, which are suggested to represent some regional hotspots of trace gas emissions to the atmosphere, in particular in the vicinity of the upwelling cells. The partial pressures of CH4, N2O, and CO2 as well as oxygen saturation in surface water were determined using IOW's self-built Mobile Equilibrator Sensor System (MESS). The system was described in details elsewhere (Sabbaghzadeh et al., 2021) but in brief, it consists of a custom-built equilibrator (combined shower-head/bubble type) with a water flow rate of about 5 l min-1 and an airflow rate of ~ 4 l min-1, which is linked to two off-axis integrated cavity output laser spectrometers (oa-ICOS, Los Gatos Instruments) for the detection of CH4 / CO2 and N2O / CO. Seawater was supplied by a pump installed at a water depth of about 6 m in the moon pool on board of RV METEOR. oa-ICOS sensors combine a highly specific infrared band laser with a set of reflective mirrors and achieve an effective absorption path length of several kilometers. This enables the detection of the trace gases with high accuracy. Three standard gases, provided by the central calibration lab of the European Integrated Carbon Observation System Research Infrastructure (ICOS RI) were used to calibrate the sensors almost daily throughout the entire expedition. To estimate sea-air gas fluxes, the atmospheric concentration of trace gases was also measured at several positions during the cruise using a tube with the inlet positioned to minimize ship contamination. All other ancillary parameters out of the MESS system were synchronized with D-ship data with a simultaneous data reduction to one-minute intervals.
    Keywords: Benguela Upwelling System; BUSUC 1; Carbon dioxide, dry air; Carbon monoxide, dry air; CT; DATE/TIME; EVAR; M157; M157-track; Meteor (1986); Methane, dry air; Namibia; Nitrous oxide, dry air; oxygen deficient zones; Ship speed; The Benguela Upwelling System under climate change – Effects of VARiability in physical forcing on carbon and oxygen budgets; Threshold; trace gases; Underway cruise track measurements; Wind direction, relative; Wind speed, relative
    Type: Dataset
    Format: text/tab-separated-values, 260 data points
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  • 10
    Publication Date: 2024-06-05
    Description: The high surface productivity triggered by nutrient-rich Benguela upwelled waters results in significant enrichment of organic carbon in the sub-surface waters due to enhanced mineralization in the water column and benthic fluxes. Hence, microbial O2-consuming processes are promoted, driving oxygen depletion that favors trace gases i.e. methane (CH4) and nitrous oxide (N2O) production at relatively shallow depths. During upwelling, gas-rich subsurface waters are also transported towards the surface waters, enhancing trace gas sea-air fluxes. We investigate the variability of these fluxes on seasonal and shorter timescales to understand the intensity of the Benguela upwelling system in gas emissions. The data might serve as a base for projections under a changing climate. The fieldwork took place during the cruise M157 (August 4th – September 16th, 2019) onboard the R/V METEOR, which encompassed close-coastal and open ocean regions between Mindelo (Cape Verde) and Walvis Bay. The main transect lines around 18, 23 and 25°S represents the Angola-Benguela frontal zone, Walvis Bay and Lüderitz upwelling cells respectively, which are suggested to represent some regional hotspots of trace gas emissions to the atmosphere, in particular in the vicinity of the upwelling cells. To explore further, nearly 300 discrete water samples were collected from the Niskin bottles at different stations for determination of the concentrations of CH4, N2O, and total inorganic carbon (CT). Analysis for CH4 and N2O was performed using an in-house designed purge and trap system with a dynamic headspace. In brief, a subsample of the water is purged with an inert ultrapure carrier gas of Helium, and the gases are focused on a cryo-trap operated at about -120°C. The volatile compounds are desorbed by rapid heating and analyzed by a gas chromatograph (Agilent 7890 B), equipped with a Flame Ionization Detector for CH4 and an Electron Capture Detector for N2O measurements, respectively. Samples for CT were taken to investigate the carbonate system. CT was measured using an automated Infra-Red Inorganic Carbon Analyzer (AIRICA) system (Marianda e.K., 24145 Kiel) from discrete 250 ml samples. In brief, a subsample is drawn into a volume-calibrated syringe and injected into a purge vessel, where the discrete sample is acidified. All species of the inorganic carbon system are converted to CO2, which is purged from the water using a carrier gas that streams through the acidified probe. Then the gas flows through a Peltier cooler and a NAFION dryer to be dried. The concentration of CO2 is then measured by an infrared detector (LICOR 7000), which integrates the peak of the purged sample. The integrated signal is directly proportional to the carbon released, allowing the CT concentration to be calculated with high precision. Certified reference material (CRM) of known CT-concentration is used for standardization and to account for drift of the sensor response.
    Keywords: Benguela Upwelling System; BUSUC 1; Carbon dioxide; CTD/Rosette; CTD-RO; DEPTH, water; EVAR; Event label; Gas chromatography, Agilent 7820B, coupled with a flame ionization detector and an Electron Capture Detector; Infrared detector LICOR 7000; LATITUDE; LONGITUDE; M157; M157_10-7; M157_11-4; M157_12-2; M157_14-2; M157_15-14; M157_16-3; M157_17-2; M157_24-1; M157_25-1; M157_26-2; M157_27-1; M157_2-8; M157_28-1; M157_31-1; M157_34-4; M157_36-2; M157_38-2; M157_39-2; M157_40-2; M157_41-14; M157_42-2; M157_43-2; M157_44-2; M157_45-2; M157_46-3; M157_49-3; M157_6-1; M157_8-2; M157_9-2; Meteor (1986); Methane; Namibia; Nitrous oxide; oxygen deficient zones; Station label; The Benguela Upwelling System under climate change – Effects of VARiability in physical forcing on carbon and oxygen budgets; trace gases
    Type: Dataset
    Format: text/tab-separated-values, 1370 data points
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