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  • 1
    Publication Date: 2024-04-19
    Keywords: CTD; CTD, underway; CTD/Rosette; CTD-RO; CTD-UW; DATE/TIME; DEPTH, water; Event label; LATITUDE; LONGITUDE; Maria S. Merian; MSM72; MSM72_100-1; MSM72_10-1; MSM72_101-1; MSM72_102-1; MSM72_103-1; MSM72_104-1; MSM72_105-1; MSM72_106-1; MSM72_107-1; MSM72_108-1; MSM72_109-1; MSM72_1-1; MSM72_110-1; MSM72_11-1; MSM72_111-1; MSM72_11-2; MSM72_112-1; MSM72_113-2; MSM72_114-1; MSM72_115-1; MSM72_116-1; MSM72_117-1; MSM72_118-1; MSM72_119-1; MSM72_120-1; MSM72_12-1; MSM72_121-1; MSM72_122-1; MSM72_123-1; MSM72_124-1; MSM72_125-1; MSM72_126-1; MSM72_127-1; MSM72_128-1; MSM72_129-1; MSM72_130-2; MSM72_13-1; MSM72_131-1; MSM72_132-1; MSM72_133-1; MSM72_134-1; MSM72_135-1; MSM72_136-1; MSM72_14-1; MSM72_15-1; MSM72_16-1; MSM72_17-1; MSM72_18-1; MSM72_19-1; MSM72_20-1; MSM72_2-1; MSM72_21-1; MSM72_22-1; MSM72_23-1; MSM72_24-1; MSM72_25-1; MSM72_26-1; MSM72_27-1; MSM72_28-1; MSM72_30-1; MSM72_3-1; MSM72_31-1; MSM72_32-1; MSM72_33-1; MSM72_34-1; MSM72_35-1; MSM72_36-1; MSM72_37-1; MSM72_38-1; MSM72_39-1; MSM72_40-1; MSM72_4-1; MSM72_41-1; MSM72_42-1; MSM72_43-1; MSM72_44-1; MSM72_45-1; MSM72_46-1; MSM72_47-2; MSM72_48-1; MSM72_49-1; MSM72_50-1; MSM72_5-1; MSM72_51-1; MSM72_52-1; MSM72_53-1; MSM72_54-1; MSM72_55-1; MSM72_56-1; MSM72_57-1; MSM72_58-1; MSM72_59-1; MSM72_60-1; MSM72_6-1; MSM72_61-1; MSM72_62-1; MSM72_63-1; MSM72_64-1; MSM72_65-1; MSM72_66-1; MSM72_67-1; MSM72_68-1; MSM72_69-1; MSM72_70-1; MSM72_7-1; MSM72_71-1; MSM72_72-1; MSM72_73-1; MSM72_74-1; MSM72_75-1; MSM72_75-2; MSM72_76-1; MSM72_77-2; MSM72_79-1; MSM72_80-1; MSM72_8-1; MSM72_81-1; MSM72_82-1; MSM72_83-1; MSM72_83-2; MSM72_84-1; MSM72_85-1; MSM72_86-1; MSM72_87-1; MSM72_88-1; MSM72_89-1; MSM72_90-1; MSM72_9-1; MSM72_91-2; MSM72_92-1; MSM72_93-1; MSM72_94-1; MSM72_95-1; MSM72_96-1; MSM72_97-2; MSM72_98-1; MSM72_99-1; Oxygen; Pressure, water; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 1168516 data points
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  • 2
    Publication Date: 2022-12-22
    Description: This chapter aims at introducing the reader to general concepts about the main forcings of the Mediterranean Sea, in terms of exchanges through the Strait of Gibraltar, and air-sea exchanges of heat, freshwater, and momentum. These forcings are also responsible for the peculiar characteristics of Mediterranean water masses. Therefore, the chapter continues with giving a general explanation on water mass analysis, and then it describes the properties and vertical and horizontal distributions of the main Mediterranean water masses. To conclude, the reader is introduced to the use of other (biogeochemical, and chemical) tracers of water masses, with a focus on the Mediterranean Sea.
    Type: Book chapter , PeerReviewed
    Format: text
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  • 3
    Publication Date: 2024-01-30
    Description: The Mediterranean Sea has been sampled irregularly by research vessels in the past, mostly by national expeditions in regional waters. To monitor the hydrographic, biogeochemical and circulation changes in the Mediterranean Sea, a systematic repeat oceanographic survey programme called Med-SHIP was recommended by the Mediterranean Science Commission (CIESM) in 2011, as part of the Global Ocean Ship-based Hydrographic Investigations Program (GO-SHIP). Med-SHIP consists of zonal and meridional surveys with different frequencies, where comprehensive physical and biogeochemical properties are measured with the highest international standards. The first zonal survey was done in 2011 and repeated in 2018. In addition, a network of meridional (and other key) hydrographic sections were designed: the first cycle of these sections was completed in 2016, with three cruises funded by the EU project EUROFLEETS2. This paper presents the physical and chemical data of the meridional and key transects in the Western and Eastern Mediterranean Sea collected during those cruises.
    Type: Article , PeerReviewed
    Format: text
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  • 4
    Publication Date: 2024-02-07
    Description: A rich data set on particulate matter optical properties and parameters (beam attenuation coefficient, volume concentration, particle size and PSD slope), accompanied by measurements of biochemical indices (particulate organic carbon, particulate nitrogen and their stable isotopic composition) was obtained from the surface to deep waters across the Mediterranean Sea, in March-April 2018. A decrease of beam attenuation coefficients, total particle volume concentrations, particulate organic carbon and nitrogen concentrations was noted towards the eastern Mediterranean Sea (EMed) in comparison to the western Mediterranean Sea (WMed). LISST-derived optical properties were significantly correlated with water mass characteristics. Overall, the most turbid water mass identified in the Mediterranean Sea was the Surface Atlantic water (AW), and the most transparent was the Transitional Mediterranean Water (TMW) in the Cretan Sea, whereas a general decrease in particulate matter concentration is observed from the WMed towards the EMed. Relatively depleted δ13C-POC values in the particle pool of the open Mediterranean Sea can be attributed to contribution from terrestrial inputs, mainly via atmospheric deposition. Throughout the entire water column, a significant positive correlation between particle beam attenuation coefficient and particulate organic carbon concentration is observed in the open Mediterranean Sea. Such relationship suggests the predominance of organic particles with biogenic origin. POC concentration and particle median diameter D50 are significantly and negatively correlated both in the WMed and the EMed Sea, confirming that small particles are POC-rich. At depth, a prominent decrease of most measured parameters was observed, with the exception of particle median diameter that increased substantially in the EMed towards the deep sea, suggesting potentially enhanced aggregation processes. The low particle size distribution slope ξ observed in the EMed, corresponding to larger particle populations, supports the above notion. Basin-wide Rayleigh-type isotopic fractionation in vertical profiles of δ15N-PN across the Mediterranean Sea, underlines the differences in the trophic characters of the two sub-basins and highlights the role of circulation changes on biogeochemical parameters and the redistribution of particulate matter as a source of nutrients in the water column.
    Type: Article , PeerReviewed
    Format: text
    Format: text
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  • 5
    Publication Date: 2022-10-27
    Description: © The Author(s), 2021. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Pedrosa-Pamies, R., Parinos, C., Sanchez-Vidal, A., Calafat, A., Canals, M., Velaoras, D., Mihalopoulos, N., Kanakidou, M., Lampadariou, N., & Gogou, A. Atmospheric and oceanographic forcing impact particle flux composition and carbon sequestration in the eastern Mediterranean Sea: a three-year time-series study in the deep Ierapetra Basin. Frontiers in Earth Science, 9, (2021): 591948, https://doi.org/10.3389/feart.2021.591948.
    Description: Sinking particles are a critical conduit for the export of organic material from surface waters to the deep ocean. Despite their importance in oceanic carbon cycling, little is known about the biotic composition and seasonal variability of sinking particles reaching abyssal depths. Herein, sinking particle flux data, collected in the deep Ierapetra Basin for a three-year period (June 2010 to June 2013), have been examined at the light of atmospheric and oceanographic parameters and main mass components (lithogenic, opal, carbonates, nitrogen, and organic carbon), stable isotopes of particulate organic carbon (POC) and source-specific lipid biomarkers. Our aim is to improve the current understanding of the dynamics of particle fluxes and the linkages between atmospheric dynamics and ocean biogeochemistry shaping the export of organic matter in the deep Eastern Mediterranean Sea. Overall, particle fluxes showed seasonality and interannual variability over the studied period. POC fluxes peaked in spring April–May 2012 (12.2 mg m−2 d−1) related with extreme atmospheric forcing. Summer export was approximately fourfold higher than mean wintertime, fall and springtime (except for the episodic event of spring 2012), fueling efficient organic carbon sequestration. Lipid biomarkers indicate a high relative contribution of natural and anthropogenic, marine- and land-derived POC during both spring (April–May) and summer (June–July) reaching the deep-sea floor. Moreover, our results highlight that both seasonal and episodic pulses are crucial for POC export, while the coupling of extreme weather events and atmospheric deposition can trigger the influx of both marine labile carbon and anthropogenic compounds to the deep Levantine Sea. Finally, the comparison of time series data of sinking particulate flux with the corresponding biogeochemical parameters data previously reported for surface sediment samples from the deep-sea shed light on the benthic–pelagic coupling in the study area. Thus, this study underscores that accounting the seasonal and episodic pulses of organic carbon into the deep sea is critical in modeling the depth and intensity of natural and anthropogenic POC sequestration, and for a better understanding of the global carbon cycle.
    Description: This research was supported by the REDECO (CTM2008-04973-E/MAR) and PERSEUS (GA 287600) projects. We further acknowledge support by the projects PANACEA—‘PANhellenic infrastructure for Atmospheric Composition and climatE chAnge’ (MIS 5021516) and ENIRISST—‘Intelligent Research Infrastructure for Shipping, Supply Chain, Transport and Logistics’ (MIS 5027930), which are implemented under the Action “Reinforcement of the Research and Innovation Infrastructure,” funded by the Operational Program “Competitiveness, Entrepreneurship and Innovation” (NSRF 2014-2020) and co-financed by Greece and EU; and by the Action “National Νetwork on Climate Change and its Impacts - Climpact” which is implemented under the sub-project 3 of the project “Infrastructure of national research networks in the fields of Precision Medicine, Quantum Technology and Climate Change,” funded by the Public Investment Program of Greece, General Secretary of Research and Technology/Ministry of Development and Investments.” Researchers from GRC Geociències Marines benefited from a Grups de Recerca Consolidats grant (2017 SGR 315) by Generalitat de Catalunya autonomous government.
    Keywords: Sinking particle fluxes ; Carbon cycle ; Lipid biomarkers ; Atmospheric forcing ; Eastern mediterranean sea ; Surface sediment ; Deep ocean ; Particulate organic carbon
    Repository Name: Woods Hole Open Access Server
    Type: Article
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