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  • 11
    Publication Date: 2024-03-18
    Keywords: 2,6,10,14-Tetramethyl-7-(3-methylpent-4-enyl)pentadecane per unit sediment mass; Age; AGE; Barents Sea; BASICC_1; BASICC_43; BASICC_8; Classification tree (CT) model; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Event label; Fram Strait; Giant box corer; GKG; Highly branched isoprenoids per unit sediment mass; Ice Proxy for the Southern Ocean with 25 carbon atoms per unit sediment mass; Latitude of event; Longitude of event; Maria S. Merian; MSM05/5; MSM05/5_712-1; PC; Phytoplankton biomarker C25 HBI (Z) triene IP25 index; Piston corer; Sea ice concentration; Sea ice type
    Type: Dataset
    Format: text/tab-separated-values, 639 data points
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  • 12
    Publication Date: 2024-03-18
    Keywords: 2,6,10,14-Tetramethyl-7-(3-methylpent-4-enyl)pentadecane per unit sediment mass; ARK-VIII/2; Barents_04GC; Barents_10BC; Barents_12GC; Barents_13GC; Barents_15GC; Barents_26GC; Barents_28GC; Barents_33GC; Barents_625; Barents_627; Barents_629; Barents_631; Barents_633; Barents_635; Barents_639; Barents_643; Barents_645; Barents_647; Barents_649; Barents_651; Barents_653; Barents_655; Barents_657; Barents_659; Barents_661; Barents_663; Barents_665; Barents_667; Barents_669; Barents_671; Barents_673; Barents_675; Barents_677; Barents_679; Barents_681; Barents_690; Barents_692; Barents_GC14; Barents_GC15; Barents_GC17; Barents_St01; Barents_St02; Barents_St03; Barents_St04; Barents_St05; Barents_St06; Barents_St07; Barents_St08; Barents_St09; Barents_St11; Barents_St12; Barents_St13; Barents_St14; Barents_St16; Barents_St17; Barents_St18; Barents_St19; Barents_St20; Barents_St21; Barents_St22; Barents_St23; Barents_St34; Barents_St35; Barents_St36; Barents_St37; Barents_St38; Barents_St39; Barents_St40; Barents_St42; Barents_St43; Barents_St45; Barents Sea; BC; Box corer; CAGE15-2914GC; CAGE15-2921GC; CAGE15-2932MC; CAGE16-51036GC; CAGE16-51048GC; CAGE16-51069GC; CAGE16-51070GC; CAGE16-51081GC; CAGE16-51082GC; Classification tree (CT) model; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Event label; GC; Giant box corer; GKG; Gravity corer; Highly branched isoprenoids per unit sediment mass; Ice Proxy for the Southern Ocean with 25 carbon atoms per unit sediment mass; James Clark Ross; JR142; JR142-GC10; JR142-GC12; JR142-GC13; JR142-GC19; JR142-GC20; JR142-GC21; JR142-GC22; JR142-GC23; JR142-GC4; JR142-GC5; JR142-GC6; JR142-GC7; JR142-GC8; JR142-GC9; JR20060728; Latitude of event; Longitude of event; MUC; MultiCorer; Norwegian Sea; Polarstern; PS19/040; PS19/045; PS19/055; PS19/102; PS19/116; PS19/119; PS19/126; PS19/132; PS19/134; PS19/136; PS19/143; PS19 EPOS II; PS2111-2; PS2113-1; PS2115-1; PS2131-1; PS2142-3; PS2144-3; PS2148-1; PS2149-1; PS2150-1; PS2151-1; PS2153-1; R100MC010; R104MC011; R1080BX010; R1096MC002; R10MC96; R1114MC003; R1119MC004; R111MC004; R1129MC005; R112MC007; R1133MC006; R1139MC010; R1146MC011; R1165MC012; R1174MC013; R117MC005; R1180MC014; R1186MC015; R11MC105; R1200MC016; R1205MC017; R1213MC018; R1257GR681; R1261MC020; R1271MC021; R1284MC027; R14MC94; R178MC010; R184BX065; R18MC98; R1MC85; R209MC003; R223MC005; R223MC006; R229MC007; R231MC008; R232MC009; R243GR037; R248GR039; R248MC010; R259GR041; R259MC011; R276BX049; R280AMC016; R280BMC018; R291MC020; R291MC022; R297BX056; R301MC023; R311BX059; R351BX065; R359BX067; R35MC114; R35MC118; R367MC026; R37MC115; R3MC110; R405MC031; R406MC032; R421MC033; R431MC035; R49MC128; R4MC107; R68AMC136; R68MC149; R754MC021; R776MC004; R77MC001; R782MC007; R80MC004; R81MC002; R87MC006; R889MC025; R911MC022; R932BX029-1; R942BX026-1; R949MC028; R961MC024; R96MC008; R973BX025-1; Sample code/label; Satellite derived; Sea ice concentration; Sea ice type; Svalbard; Svalbard Shelf
    Type: Dataset
    Format: text/tab-separated-values, 2594 data points
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  • 13
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    In:  Supplement to: Köseoğlu, Denizcan; Belt, Simon T; Smik, Lukas; Yao, Haoyi; Panieri, Giuliana; Knies, Jochen (2018): Complementary biomarker-based methods for characterising Arctic sea ice conditions: A case study comparison between multivariate analysis and the PIP25 index. Geochimica et Cosmochimica Acta, 222, 406-420, https://doi.org/10.1016/j.gca.2017.11.001
    Publication Date: 2024-03-18
    Description: We investigated the potential for classification tree (CT) models to provide a further approach to paleo Arctic sea ice reconstruction through analysis of a suite of six highly branched isoprenoid (HBI) biomarkers in 198 surface sediments from the Barents Sea. The four CT models representing modern sea ice conditions were then applied to four downcore records within the study area (cores BASICC 1, 8, 43, and core MSM5/5-712-1) in order to reconstruct sea ice conditions over the last 300 years. The current dataset includes the absolute HBI concentrations in all sediment samples (ng/g dry sed.), as well as CT model outcomes for all samples, which were classified as having experienced marginal, intermediate, or extensive overlying sea ice cover (further details are available in the manuscript associated with these data).
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 14
    Publication Date: 2020-01-21
    Description: The HACON cruise is a major component of the FRINATEK HACON project, which aims at investigating the role of the Gakkel Ridge and Arctic Ocean in biological connectivity amongst ocean basins and global biogeography of chemosynthetic ecosystems. The HACON study area is centered in the Aurora seamount and Aurora vent field.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Miscellaneous , notRev
    Format: application/pdf
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  • 15
    Publication Date: 2022-05-25
    Description: © The Author(s), 2018. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Scientific Reports 8 (2018): 10610, doi:10.1038/s41598-018-28871-3.
    Description: Foraminifera in sediments exposed to gas-hydrate dissociation are not expected to have cellular adaptations that facilitate inhabitation of chemosynthesis-based ecosystems because, to date, there are no known endemic seep foraminifera. To establish if foraminifera inhabit sediments impacted by gas-hydrate dissociation, we examined the cellular ultrastructure of Melonis barleeanus (Williamson, 1858) from the Vestnesa gas hydrate province (Arctic Ocean, west of Svalbard at ~79 °N; ~1200-m depth; n = 4). From sediments with gas hydrate indicators, living M. barleeanus had unusual pore plugs composed of a thick, fibrous meshwork; mitochondria were concentrated at the cell periphery, under pore plugs. While there was no evidence of endosymbioses with prokaryotes, most M. barleeanus specimens were associated with what appear to be Type I methanotrophic bacteria. One foraminifer had a particularly large bolus of these microbes concentrated near its aperture. This is the first documented instance of bona fide living M. barleeanus in gas-hydrate sediments and first documentation of a foraminifer living in close association with putative methanotrophs. Our observations have implications to paleoclimate records utilizing this foundational foraminiferal species.
    Description: JMB was funded by a WHOI Independent Study Award (Mellon Grant), with partial support from NSF grant OCE-1634469. GP and CAGE 15-2 cruise were supported by the Research Council of Norway through CAGE Center for Excellence in Arctic Gas Hydrate Environment and Climate project 223259 and NORCRUST (project number 255150).
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 16
    Publication Date: 2022-01-04
    Description: The recent expansion of Atlantic waters into the Arctic Ocean represents undisputable evidence of the rapid changes occurring in this region. Understanding the past variability of this “Atlantification” is thus crucial in providing a longer perspective on the modern Arctic changes. Here, we reconstruct the history of Atlantification along the eastern Fram Strait during the past 800 years using precisely dated paleoceanographic records based on organic biomarkers and benthic foraminiferal data. Our results show rapid changes in water mass properties that com-menced in the early 20th century—several decades before the documented Atlantification by instrumental records. Comparison with regional records suggests a poleward expansion of subtropical waters since the end of the Little Ice Age in response to a rapid hydrographic reorganization in the North Atlantic. Understanding of this mechanism will require further investigations using climate model simulations.INTRODUCTIONClimate reconstructions of the Common Era are fundamental bench-marks to place human-induced changes into the context of natural climatic change (1, 2). This is particularly relevant for the Arctic, which is currently warming faster than any other region (3). Arctic warming has been associated with rapid sea ice decline and expan-sion of Atlantic waters (AWs) into the Arctic basin (4, 5) — a phenomenon commonly referred to as “Atlantification” (6). While in situ observations and satellite images provide high-resolution records of anomalies in water mass properties and sea ice since the 1930s and 1980s (4, 7–10), respectively, little is known about this phenomenon in pre- and early-industrial times. Because natural archives preserve evidence of past climate variability, they can offer a longer-term perspective on Atlantification in this region.The Fram Strait represents an important oceanographic gateway that allows the exchange of Arctic and AW masses (11). Low-resolution paleoceanographic records suggest that the summer temperatures of the AW inflow moving along the eastern Fram Strait may have increased before the instrumental record (12). Although this change in AW properties hints at a possible early sign of Atlantification, the lack of a reliable chronology for these records limits the integration with regional high-resolution proxy reconstructions to determine the physical mechanisms at play. Recently, it has been argued that the Atlantic subpolar gyre (SPG) has weakened since the 20th century (13). This, in turn, might have conditioned the water masses routed toward the Arctic. However, a survey of the recent literature shows that our
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 17
    Publication Date: 2022-01-11
    Description: Immersive virtual reality can potentially open up interesting geological sites to students, academics and others who may not have had the opportunity to visit such sites previously. We study how users perceive the usefulness of an immersive virtual reality approach applied to Earth Sciences teaching and communication. During nine immersive virtual reality-based events held in 2018 and 2019 in various locations (Vienna in Austria, Milan and Catania in Italy, Santorini in Greece), a large number of visitors had the opportunity to navigate, in immersive mode, across geological landscapes reconstructed by cutting-edge, unmanned aerial system-based photogrammetry techniques. The reconstructed virtual geological environments are specifically chosen virtual geosites, from Santorini (Greece), the North Volcanic Zone (Iceland), and Mt. Etna (Italy). Following the user experiences, we collected 459 questionnaires, with a large spread in participant age and cultural background. We find that the majority of respondents would be willing to repeat the immersive virtual reality experience, and importantly, most of the students and Earth Science academics who took part in the navigation confirmed the usefulness of this approach for geo-education purposes.
    Description: This research has been provided in the framework of the following projects: (i) the MIUR project ACPR15T4_00098–Argo3D (http://argo3d.unimib.it/ (accessed on 26 November 2021)); (ii) 3DTeLC Erasmus + Project 2017-1-UK01-KA203-036719 (http://www.3dtelc.com (accessed on 26 November 2021)); (iii) EGU 2018 Public Engagement Grant (https://www.egu.eu/outreach/peg/ (accessed on 26 November 2021)). Agisoft Metashape is acknowledged for photogrammetric data processing. This article is also an outcome of Project MIUR–Dipartimenti di Eccellenza 2018–2022. Finally, this paper is an outcome of the Virtual Reality lab for Earth Sciences—GeoVires lab (https://geovires.unimib.it/ (accessed on 26 November 2021)). The work supports UNESCO IGCP 692 ‘Geoheritage for Resilience’.
    Description: Published
    Description: 9
    Description: 1TM. Formazione
    Description: JCR Journal
    Keywords: immersive virtual reality ; geology; ; photogrammetry; ; education; ; Iceland; ; Santorini ; Etna ; 04.04. Geology ; 05.03. Educational, History of Science, Public Issues ; 05.04. Instrumentation and techniques of general interest ; 04.08. Volcanology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 18
    Publication Date: 2023-03-08
    Description: © The Author(s), 2022. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Schmidt, C., Geslin, E., Bernhard, J. M., LeKieffre, C., Svenning, M. M., Roberge, H., Schweizer, M., & Panieri, G. Deposit-feeding of Nonionellina labradorica (foraminifera) from an Arctic methane seep site and possible association with a methanotroph. Biogeosciences, 19(16), (2022): 3897–3909, https://doi.org/10.5194/bg-19-3897-2022.
    Description: Several foraminifera are deposit feeders that consume organic detritus (dead particulate organic material with entrained bacteria). However, the role of such foraminifera in the benthic food web remains understudied. Foraminifera feeding on methanotrophic bacteria, which are 13C-depleted, may cause negative cytoplasmic and/or calcitic δ13C values. To test whether the foraminiferal diet includes methanotrophs, we performed a short-term (20 h) feeding experiment with Nonionellina labradorica from an active Arctic methane-emission site (Storfjordrenna, Barents Sea) using the marine methanotroph Methyloprofundus sedimenti and analysed N. labradorica cytology via transmission electron microscopy (TEM). We hypothesised that M. sedimenti would be visible post-experiment in degradation vacuoles, as evidenced by their ultrastructure. Sediment grains (mostly clay) occurred inside one or several degradation vacuoles in all foraminifers. In 24 % of the specimens from the feeding experiment degradation vacuoles also contained bacteria, although none could be confirmed to be the offered M. sedimenti. Observations of the apertural area after 20 h incubation revealed three putative methanotrophs, close to clay particles, based on bacterial ultrastructural characteristics. Furthermore, we noted the absence of bacterial endobionts in all examined N. labradorica but confirmed the presence of kleptoplasts, which were often partially degraded. In sum, we suggest that M. sedimenti can be consumed via untargeted grazing in seeps and that N. labradorica can be generally classified as a deposit feeder at this Arctic site.
    Description: This research has been supported by the French scientific programme MOPGA (Make our Planet Great Again) managed by the National Research Agency; the Norwegian Research Council through the Centre for Arctic Gas Hydrate, Environment and Climate (project number 223259); NORCRUST (project number 255250); and by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) – 444059848.
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 19
    Publication Date: 2022-10-27
    Description: Field-based classes in geological sciences are crucial components of geoscience education and research. Owing to the COVID-19 pandemic, such activities became problematic due to limitations such as travel restrictions and lockdown periods: this motivated the geoeducational community to tailor new ways to engage people in field activities. As a result, we adopted Immersive Virtual Reality as a tool to involve students, academics, and the lay public in field exploration, thus making geological exploration accessible also to people affected by permanent or temporary motor disabilities. In particular, we evaluated how users perceive the usefulness of this approach as applied to Earth Science learning and teaching, through nine outreach events, where a total of 459 participants were involved, with different ages and cultural backgrounds. The participants explored, in an immersive mode, four geological landscapes, defined as virtual geological environments, which have been reconstructed by cutting-edge, unmanned aerial system-based photogrammetry techniques. They include: Santorini (Greece), the North Volcanic Zone (Iceland), and Mt. Etna (Italy). After the exploration, each participant filled in an anonymous questionnaire. The results show that the majority would be willing to repeat the experience, and, most importantly, the majority of the students and Earth Science academics who took part in the navigation confirmed the usefulness of this technique for geo-education purposes. Our approach can be considered as a groundbreaking tool and an innovative democratic way to access information and experiences, as well as to promote inclusivity and accessibility in geo-education, while reducing travel costs, saving time, and decreasing the carbon footprint. This work has been carried out in the framework of the following projects: i) ACPR15T4_ 00098 “Agreement between the University of Milan Bicocca and the Cometa Consortium for the experimentation of cutting-edge interactive technologies for the improvement of science teaching and dissemination” of Italian Ministry of Education, University and Research (ARGO3D - https://argo3d.unimib.it/); ii) Erasmus+ Key Action 2 2017-1-UK01-KA203- 036719 “3DTeLC – Bringing the 3D-world into the classroom: a new approach to Teaching, Learning and Communicating the science of geohazards in terrestrial and marine environments” (http://3dtelc.lmv.uca.fr/; https://www.3dtelc.com/); iii) 2018 EGU Public Engagement Grants (https://www.egu.eu/outreach/peg/).
    Description: This work has been carried out in the framework of the following projects: i) ACPR15T4_ 00098 “Agreement between the University of Milan Bicocca and the Cometa Consortium for the experimentation of cutting-edge interactive technologies for the improvement of science teaching and dissemination” of Italian Ministry of Education, University and Research (ARGO3D - https://argo3d.unimib.it/); ii) Erasmus+ Key Action 2 2017-1-UK01-KA203- 036719 “3DTeLC – Bringing the 3D-world into the classroom: a new approach to Teaching, Learning and Communicating the science of geohazards in terrestrial and marine environments” (http://3dtelc.lmv.uca.fr/; https://www.3dtelc.com/); iii) 2018 EGU Public Engagement Grants (https://www.egu.eu/outreach/peg/).
    Description: Published
    Description: Vienna (Austria)
    Description: 1TM. Formazione
    Keywords: Virtual Reality ; geology ; tectonophysics ; education ; 04.07. Tectonophysics ; 05.03. Educational, History of Science, Public Issues ; 05.04. Instrumentation and techniques of general interest
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Conference paper
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  • 20
    Publication Date: 2022-11-15
    Description: © The Author(s), 2022. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in LeKieffre, C., Jauffrais, T., Bernhard, J., Filipsson, H., Schmidt, C., Roberge, H., Maire, O., Panieri, G., Geslin, E., & Meibom, A. Ammonium and sulfate assimilation is widespread in benthic foraminifera. Frontiers in Marine Science, 9, (2022): 861945, https://doi.org/10.3389/fmars.2022.861945.
    Description: Nitrogen and sulfur are key elements in the biogeochemical cycles of marine ecosystems to which benthic foraminifera contribute significantly. Yet, cell-specific assimilation of ammonium, nitrate and sulfate by these protists is poorly characterized and understood across their wide range of species-specific trophic strategies. For example, detailed knowledge about ammonium and sulfate assimilation pathways is lacking and although some benthic foraminifera are known to maintain intracellular pools of nitrate and/or to denitrify, the potential use of nitrate-derived nitrogen for anabolic processes has not been systematically studied. In the present study, NanoSIMS isotopic imaging correlated with transmission electron microscopy was used to trace the incorporation of isotopically labeled inorganic nitrogen (ammonium or nitrate) and sulfate into the biomass of twelve benthic foraminiferal species from different marine environments. On timescales of twenty hours, no detectable 15N-enrichments from nitrate assimilation were observed in species known to perform denitrification, indicating that, while denitrifying foraminifera store intra-cellular nitrate, they do not use nitrate-derived nitrogen to build their biomass. Assimilation of both ammonium and sulfate, with corresponding 15N and 34S-enrichments, were observed in all species investigated (with some individual exceptions for sulfate). Assimilation of ammonium and sulfate thus can be considered widespread among benthic foraminifera. These metabolic capacities may help to underpin the ability of benthic foraminifera to colonize highly diverse marine habitats.
    Description: This work was supported by the Swiss National Science Foundation (grant no. 200021_149333), and a postdoctoral fellowship allowed to CL by the University Loire-Bretagne. SBB sampling was funded by US National Science Foundation grant BIO IOS 1557430 to JMB, who also acknowledges NASA grant #80NSSC21K0478 for partial support. HF acknowledges funding from the Swedish Research Council VR (grant number 2017-04190). Svalbard sampling was supported by the Research Council of Norway through CAGE (Center for Excellence in Arctic Gas Hydrate Environment and Climate, project number 223259) and NORCRUST (project number 255150) to GP and the fellowship MOPGA (Make Our Planet Great Again) by CAMPUS France to CS.
    Keywords: Marine protists ; Coastal environments ; Biogeochemical cycles ; NanoSIMS ; Nitrogen ; Sulfur
    Repository Name: Woods Hole Open Access Server
    Type: Article
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