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  • 1
    Publication Date: 2023-03-14
    Keywords: Alkalinity, total; Ammonium; Atomic absorption spectrometry (AAS); Bottle, Niskin 5-L; Carbon, inorganic, dissolved; Date/Time of event; DEPTH, sediment/rock; DIVER; ECO2; ECO2-8; ECO2-8-NIS-2; ECO2-8-NIS-4; ECO2-8-NIS-6; ECO2-8-PW-1; ECO2-8-PW-10; ECO2-8-PW-11; ECO2-8-PW-12; ECO2-8-PW-13; ECO2-8-PW-14; ECO2-8-PW-15; ECO2-8-PW-16; ECO2-8-PW-17; ECO2-8-PW-18; ECO2-8-PW-19; ECO2-8-PW-2; ECO2-8-PW-20; ECO2-8-PW-21; ECO2-8-PW-3; ECO2-8-PW-4; ECO2-8-PW-5; ECO2-8-PW-6; ECO2-8-PW-7; ECO2-8-PW-8; ECO2-8-PW-9; ECO2-8-PW-S1; ECO2-8-PW-S2; ECO2-8-PW-S3; ECO2-8-PW-S4; ECO2-8-PW-S5; ECO2-8-PW-S6; ECO2-8-PW-S7; ECO2-8-PW-S8; ECO2-8-PW-S9; Elevation of event; Event label; Flow injection analysis (Hall and Aller 1992); Gas chromatography; Iron; Latitude of event; Longitude of event; Manganese; Methane; NIS_5L; Nitrate and Nitrite; Nitrite; Panarea; pH; pH meter (Mettler Toledo InLab Semi-Micro); Phosphate; Photometer, methylene blue (Cline 1969); Refractometer; Salinity; Sampling by diver; Seawater analysis after Grasshoff et al., 1983 (Verlag Chemie GmbH Weinheim); Silicate; Sub-seabed CO2 Storage: Impact on Marine Ecosystems; Sulfide; Two-point titration (Edmond 1970); Zodiac
    Type: Dataset
    Format: text/tab-separated-values, 1805 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-02-12
    Description: Samples in this dataset were collected at the long-term ecological research (LTER) site HAUSGARTEN in Fram Strait, and the central Arctic Ocean. On board, the samples were fixed with formalin in a final concentration of 2% for 10 – 12 hours, then filtered onto 0.2 µm polycarbonate Nucleopore Track-Etched filters, and stored at -20°C for further analysis. Cell abundances of the groups Alteromonas, Bacteroidia, Polaribacter, Gammaproteobacteria and the SAR11 clade were asses using CAtalyzed reporter deposition Fluorescence In Situ Hybridization (CARD-FISH) following the protocol established by (Pernthaler et al., 2002). The filters were evaluated microscopically under an automated microscope (Zeder et al., 2011). Cell enumeration was performed with the software Automated Cell Measuring and Enumeration Tool (ACMETool3, 2018-11-09; Zeder et al., 2011). Cells were counted as objects according to manually defined parameters separately for the DAPI and FISH channels.
    Keywords: 2-(4-Amidinophenyl)-1H-indole-6-carboxamidine; Alteromonas; Alteromonas, cells; ARK-XXX/1.2; Bacteroidetes; Bacteroidetes, cells; CARD-FISH; cell counts; CTD/Rosette with Underwater Vision Profiler; CTD-RO_UVP; DEPTH, ice/snow; DEPTH, water; EG_I; EG_IV; Event label; Fram Strait; Gammaproteobacteria; Gammaproteobacteria, cells; Giant box corer; GKG; ICE; Ice station; North Greenland Sea; Polaribacter; Polaribacter, cells; Polarstern; PS99/043-3; PS99/048-15; PS99/051-2; PS99/053-8; PS99.2; SAR11 clade; Type
    Type: Dataset
    Format: text/tab-separated-values, 48 data points
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2023-02-24
    Keywords: Dissolution rate; DIVER; ECO2; ECO2-8; ECO2-8-Marble-1; ECO2-8-Marble-2b; Elevation of event; Event label; Latitude of event; Longitude of event; Panarea; Sample ID; Sampling by diver; Sub-seabed CO2 Storage: Impact on Marine Ecosystems; Zodiac
    Type: Dataset
    Format: text/tab-separated-values, 108 data points
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2023-02-24
    Keywords: Date/Time of event; DEPTH, sediment/rock; ECO2; ECO2-8; ECO2-8-PUC-10a; ECO2-8-PUC-10b; ECO2-8-PUC-10c; ECO2-8-PUC-11a; ECO2-8-PUC-11b; ECO2-8-PUC-12a; ECO2-8-PUC-12b; ECO2-8-PUC-12c; ECO2-8-PUC-16a; ECO2-8-PUC-16b; ECO2-8-PUC-2a; ECO2-8-PUC-6a; ECO2-8-PUC-6b; ECO2-8-PUC-7a; ECO2-8-PUC-7b; ECO2-8-PUC-7c; ECO2-8-PUC-8a; ECO2-8-PUC-8b; ECO2-8-PUC-9a; ECO2-8-PUC-9b; ECO2-8-PUC-9c; Elevation of event; Epifluorescence microscopy (Boetius et al. 2000); Event label; Latitude of event; Longitude of event; Panarea; Prokaryotes, abundance as single cells; PUC; Push corer; Sample type; Sub-seabed CO2 Storage: Impact on Marine Ecosystems; Zodiac
    Type: Dataset
    Format: text/tab-separated-values, 90 data points
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2023-02-24
    Keywords: Aluminium; Antimony; Arsenic; Barium; Beryllium; Bismuth; Boron; Bromine; Cadmium; Caesium; Calcium; Cerium; Chromium; Cobalt; Copper; Date/Time of event; DEPTH, sediment/rock; Dysprosium; ECO2; ECO2-2; ECO2-2-PUC-1a; ECO2-2-PUC-2b; Erbium; Europium; Event label; Gadolinium; Gallium; Gold; Holmium; Indium; Inductively coupled plasma - mass spectrometry (ICP-MS); Iodine; Iron; Lanthanum; Latitude of event; Lead; Lithium; Longitude of event; Lutetium; Magnesium; Manganese; Molybdenum; Neodymium; Nickel; Panarea; Phosphorus; Potassium; Praseodymium; PUC; Push corer; Rubidium; Samarium; Scandium; Selenium; Silicon; Silver; Sodium; Strontium; Sub-seabed CO2 Storage: Impact on Marine Ecosystems; Sulfur, total; Tellurium; Terbium; Thallium; Thorium; Thulium; Tin; Uranium; Vanadium; Ytterbium; Yttrium; Zinc
    Type: Dataset
    Format: text/tab-separated-values, 114 data points
    Location Call Number Limitation Availability
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  • 6
    Publication Date: 2023-02-24
    Description: The amount of total carbon and nitrogen were assessed for sediments profile (0 to 10 cm depth) collected at CO2-impacted sites and reference site in 2012 and 2013.
    Keywords: Carbon, organic, total; Date/Time of event; DEPTH, sediment/rock; ECO2; ECO2-3; ECO2-3-PUC-10a; ECO2-3-PUC-13d; ECO2-3-PUC-14b; ECO2-3-PUC-17b; ECO2-3-PUC-17d; ECO2-3-PUC-3c; ECO2-3-PUC-6b; ECO2-3-PUC-7b; ECO2-3-PUC-9b; ECO2-8; ECO2-8-PUC-10b; ECO2-8-PUC-10c; ECO2-8-PUC-12a; ECO2-8-PUC-16b; ECO2-8-PUC-6b; ECO2-8-PUC-7a; ECO2-8-PUC-8a; ECO2-8-PUC-8b; ECO2-8-PUC-9a; Elevation of event; Event label; HCL acidification; Latitude of event; Longitude of event; Nitrogen, organic; Panarea; PUC; Push corer; Sub-seabed CO2 Storage: Impact on Marine Ecosystems; Zodiac
    Type: Dataset
    Format: text/tab-separated-values, 178 data points
    Location Call Number Limitation Availability
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  • 7
    Publication Date: 2023-02-24
    Description: Sediment bacterial community at natural CO2 vents as described applying molecular fingerprint technique Automated Ribosomal Intergenic Spacer Analysis (ARISA) on sandy sediment samples collected in 2011, 2012 and 2013 collected at Basiluzzo Islet (Panarea Island). Automated ribosomal intergenic spacer analysis (ARISA) is a quantitative fingerprinting approach for estimating the abundance of Operation Taxonomic Units (OUT) in natural microbial communities. A detailed description of this molecular method is provided in Ramette (2009)*. Briefly PCR-amplified fragments, obtained using primes that yield peaks in the range 100 to 1,000 bp, were separated via capillary electrophoresis and then raw profiles were checked for stable baselines and voltage, and peak sizes and absolute areas were determined by using GeneMapper software v 3.7 (Applied Biosystems) with minimum peak heights of 50 fluorescence units for all dyes. Here the GeneMapper output table is provided. In Molari et al. (XXXX) samples-by-binned-OUT tables was obtained by calculating relative fluorescence intensity (RFI), considering fragments above a threshold of 50 fluorescence units and between 100–1000 bp length, and applying a binning strategy with a bin size of 2 bp. *Ramette, Alban (2009). Quantitative Community Fingerprinting Methods for Estimating the Abundance of Operational Taxonomic Units in Natural Microbial Communities. Applied and Environmental Microbiology, 75(8): 2495−2505.
    Keywords: Base pair size; Date/Time of event; ECO2; ECO2-2; ECO2-2-FT-1; ECO2-2-FT-11; ECO2-2-FT-12; ECO2-2-FT-2; ECO2-2-FT-27; ECO2-2-FT-28; ECO2-2-FT-29; ECO2-2-FT-3; ECO2-2-FT-30; ECO2-2-FT-31; ECO2-2-FT-32; ECO2-2-FT-33; ECO2-2-FT-34; ECO2-2-FT-35; ECO2-2-FT-36; ECO2-2-FT-37; ECO2-2-FT-38; ECO2-2-FT-4; ECO2-2-FT-5; ECO2-2-FT-53; ECO2-2-FT-54; ECO2-2-FT-55; ECO2-2-FT-56; ECO2-2-FT-57; ECO2-2-FT-58; ECO2-2-FT-59; ECO2-2-FT-6; ECO2-2-FT-60; ECO2-2-FT-61; ECO2-2-FT-62; ECO2-2-FT-63; ECO2-2-FT-64; ECO2-2-FT-7; ECO2-2-FT-8; ECO2-2-PUC-1a; ECO2-2-PUC-1b; ECO2-2-PUC-1c; ECO2-2-PUC-2a; ECO2-2-PUC-2b; ECO2-2-PUC-2c; ECO2-3; ECO2-3-FT-1; ECO2-3-FT-10; ECO2-3-FT-11; ECO2-3-FT-12; ECO2-3-FT-13; ECO2-3-FT-14; ECO2-3-FT-15; ECO2-3-FT-16; ECO2-3-FT-18; ECO2-3-FT-19; ECO2-3-FT-2; ECO2-3-FT-20; ECO2-3-FT-3; ECO2-3-FT-36; ECO2-3-FT-37; ECO2-3-FT-38; ECO2-3-FT-39; ECO2-3-FT-4; ECO2-3-FT-40; ECO2-3-FT-41; ECO2-3-FT-42; ECO2-3-FT-43; ECO2-3-FT-44; ECO2-3-FT-45; ECO2-3-FT-46; ECO2-3-FT-47; ECO2-3-FT-48; ECO2-3-FT-49; ECO2-3-FT-5; ECO2-3-FT-50; ECO2-3-FT-51; ECO2-3-FT-52; ECO2-3-FT-53; ECO2-3-FT-54; ECO2-3-FT-55; ECO2-3-FT-6; ECO2-3-FT-7; ECO2-3-FT-71; ECO2-3-FT-72; ECO2-3-FT-73; ECO2-3-FT-74; ECO2-3-FT-75; ECO2-3-FT-76; ECO2-3-FT-77; ECO2-3-FT-78; ECO2-3-FT-79; ECO2-3-FT-8; ECO2-3-FT-80; ECO2-3-FT-81; ECO2-3-FT-82; ECO2-3-FT-83; ECO2-3-FT-84; ECO2-3-FT-85; ECO2-3-FT-86; ECO2-3-FT-87; ECO2-3-FT-88; ECO2-3-FT-89; ECO2-3-FT-9; ECO2-3-FT-90; ECO2-3-PUC-10c; ECO2-3-PUC-11b; ECO2-3-PUC-12d; ECO2-3-PUC-13d; ECO2-3-PUC-13f; ECO2-3-PUC-16c; ECO2-3-PUC-17a; ECO2-3-PUC-1a; ECO2-3-PUC-2a; ECO2-3-PUC-2b; ECO2-3-PUC-2d; ECO2-3-PUC-3a; ECO2-3-PUC-3b; ECO2-3-PUC-3c; ECO2-3-PUC-4a; ECO2-3-PUC-4b; ECO2-3-PUC-4c; ECO2-3-PUC-5a; ECO2-3-PUC-5b; ECO2-3-PUC-6a; ECO2-3-PUC-6c; ECO2-3-PUC-6f; ECO2-3-PUC-7a; ECO2-3-PUC-8c; ECO2-3-PUC-8e; ECO2-3-PUC-9a; ECO2-3-PUC-9b; ECO2-8; ECO2-8-FT-1; ECO2-8-FT-10; ECO2-8-FT-11; ECO2-8-FT-12; ECO2-8-FT-13; ECO2-8-FT-14; ECO2-8-FT-15; ECO2-8-FT-16; ECO2-8-FT-17; ECO2-8-FT-18; ECO2-8-FT-19; ECO2-8-FT-2; ECO2-8-FT-20; ECO2-8-FT-21; ECO2-8-FT-22; ECO2-8-FT-23; ECO2-8-FT-24; ECO2-8-FT-25; ECO2-8-FT-26; ECO2-8-FT-27; ECO2-8-FT-28; ECO2-8-FT-29; ECO2-8-FT-3; ECO2-8-FT-30; ECO2-8-FT-31; ECO2-8-FT-32; ECO2-8-FT-33; ECO2-8-FT-34; ECO2-8-FT-35; ECO2-8-FT-36; ECO2-8-FT-37; ECO2-8-FT-38; ECO2-8-FT-39; ECO2-8-FT-4; ECO2-8-FT-40; ECO2-8-FT-41; ECO2-8-FT-42; ECO2-8-FT-43; ECO2-8-FT-44; ECO2-8-FT-45; ECO2-8-FT-46; ECO2-8-FT-47; ECO2-8-FT-48; ECO2-8-FT-49; ECO2-8-FT-5; ECO2-8-FT-50; ECO2-8-FT-51; ECO2-8-FT-52; ECO2-8-FT-53; ECO2-8-FT-54; ECO2-8-FT-55; ECO2-8-FT-56; ECO2-8-FT-57; ECO2-8-FT-58; ECO2-8-FT-59; ECO2-8-FT-6; ECO2-8-FT-60; ECO2-8-FT-7; ECO2-8-FT-8; ECO2-8-FT-9; ECO2-8-PUC-10a; ECO2-8-PUC-10b; ECO2-8-PUC-10c; ECO2-8-PUC-11a; ECO2-8-PUC-11b; ECO2-8-PUC-12a; ECO2-8-PUC-12b; ECO2-8-PUC-12c; ECO2-8-PUC-16a; ECO2-8-PUC-16b; ECO2-8-PUC-2a; ECO2-8-PUC-6a; ECO2-8-PUC-6b; ECO2-8-PUC-7a; ECO2-8-PUC-7b; ECO2-8-PUC-7c; ECO2-8-PUC-8a; ECO2-8-PUC-8b; ECO2-8-PUC-9a; ECO2-8-PUC-9b; ECO2-8-PUC-9c; Elevation of event; Event label; Hand push corer; HSR; Latitude of event; Longitude of event; Panarea; Peak area; PUC; Push corer; Sample code/label; Sub-seabed CO2 Storage: Impact on Marine Ecosystems; Zodiac
    Type: Dataset
    Format: text/tab-separated-values, 1071480 data points
    Location Call Number Limitation Availability
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  • 8
    Publication Date: 2023-05-12
    Keywords: Alkalinity, total; Ammonium; Benthic Chamber; Carbon, inorganic, dissolved; CHAM; Date/Time of event; DEPTH, sediment/rock; ECO2; ECO2-8; ECO2-8-CHAM-1a; ECO2-8-CHAM-1b; ECO2-8-CHAM-1c; ECO2-8-CHAM-2a; ECO2-8-CHAM-2b; ECO2-8-CHAM-2c; ECO2-8-CHAM-3a; ECO2-8-CHAM-3b; ECO2-8-CHAM-3c; ECO2-8-CHAM-4a; ECO2-8-CHAM-4b; ECO2-8-CHAM-4c; ECO2-8-CHAM-5a; ECO2-8-CHAM-5b; ECO2-8-CHAM-5c; ECO2-8-CHAM-6a; ECO2-8-CHAM-6b; ECO2-8-CHAM-6c; Elevation of event; Event label; Flow injection analysis (Hall and Aller 1992); Incubation duration; Latitude of event; Longitude of event; Nitrate and Nitrite; Nitrite; Oxygen; Panarea; pH; pH meter; Phosphate; Photometer, methylene blue (Cline 1969); Refractometer; Salinity; Seawater analysis after Grasshoff et al., 1983 (Verlag Chemie GmbH Weinheim); Silicate; Sub-seabed CO2 Storage: Impact on Marine Ecosystems; Sulfide; Time point, descriptive; Titration, Winkler; Two-point titration (Edmond 1970); Volume; Zodiac
    Type: Dataset
    Format: text/tab-separated-values, 793 data points
    Location Call Number Limitation Availability
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  • 9
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    Unknown
    PANGAEA
    In:  Supplement to: Molari, Massimiliano; Guilini, Katja; Lott, Christian; Weber, Miriam; de Beer, Dirk; Meyer, Stefanie; Ramette, Alban; Wegener, Gunter; Wenzhöfer, Frank; Martin, Daniel; Cibic, Tamara; De Vittor, Cinzia; Vanreusel, Ann; Boetius, Antje (2018): CO2 leakage alters biogeochemical and ecological functions of submarine sands. Science Advances, 4(2), eaao2040, https://doi.org/10.1126/sciadv.aao2040
    Publication Date: 2023-05-12
    Description: Subseabed CO2 storage is considered a future climate change mitigation technology. We investigated the ecological consequences of CO2 leakage for a marine benthic ecosystem. For the first time with a multidisciplinary integrated study, we tested hypotheses derived from a meta-analysis of previous experimental and in situ high-CO2 impact studies. For this, we compared ecological functions of naturally CO2-vented seafloor off the Mediterranean island Panarea (Tyrrhenian Sea, Italy) to those of nonvented sands, with a focus on biogeochemical processes and microbial and faunal community composition. High CO2 fluxes (up to 4 to 7 mol CO2 m−2 hour−1) dissolved all sedimentary carbonate, and comigration of silicate and iron led to local increases of microphytobenthos productivity (+450%) and standing stocks (+300%). Despite the higher food availability, faunal biomass (−80%) and trophic diversity were substantially lower compared to those at the reference site. Bacterial communities were also structurally and functionally affected, most notably in the composition of heterotrophs and microbial sulfate reduction rates (−90%). The observed ecological effects of CO2 leakage on submarine sands were reproduced with medium-term transplant experiments. This study assesses indicators of environmental impact by CO2 leakage and finds that community compositions and important ecological functions are permanently altered under high CO2.
    Keywords: ECO2; Sub-seabed CO2 Storage: Impact on Marine Ecosystems
    Type: Dataset
    Format: application/zip, 43 datasets
    Location Call Number Limitation Availability
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  • 10
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    Unknown
    PANGAEA
    In:  Supplement to: Schmid, Florian; Molari, Massimiliano; Schlindwein, Vera; Kaul, Norbert; Bach, Wolfgang; Vogt, Martin; Jöns, Niels; Hansen, Christian T; Walter, Maren; Damm, Ellen; Boetius, Antje (submitted): Lithospheric strength, thermal structure, diffusive geochemical fluxes and microbial activity in the ultraslow spreading Southwest Indian Ridge axial valley. Geochemistry, Geophysics, Geosystems
    Publication Date: 2023-09-01
    Description: The relation of tectonics and geochemical cycling at magma-starved ultraslow spreading ridges are hardly understood. Here we present yield-strength profiles, heat flow determinations, geochemical- and microbiological results from the axial valley of the Oblique Supersegment at the Southwest Indian Ridge. Our results report a rheologically weak lithosphere down to 18 km and a very low heat flow of 63.4 - 82.5 mW/m² at the brittle-ductile transition. This is best explained by serpentinization possibly focused in shear zones of deep reaching boundary faults. The axial valley sediments, especially in the deepest areas, are enriched in organic carbon due to high primary productivity and efficient downslope sediment transportation. The microbial activity is comparable inside and outside the valley and appears strongest at a site where we discovered a bivalve that is endemic to hydrothermal- or reducing habitats. We did not find any site of active hydrothermal discharge. Pore water geochemical profiles are contrary to the local temperature and heat flow values and show high diffusive upward fluxes at sites of low heat flow and vice versa. Biogeochemical processes in the axial valley sediments appear strongly influenced by the accumulation and subsequent remineralization of organic matter. Increasing flux rates towards the boundary faults indicate a diffuse, sluggish fluid circulation in these fault zones.
    Type: Dataset
    Format: application/zip, 64 datasets
    Location Call Number Limitation Availability
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