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  • 2020E1; ArcticABCDevelopment; Arctic Ocean; Arctic Ocean ecosystems - Applied technology, Biological interactions and Consequences in an era of abrupt climate change; Arctic Research Icebreaker Consortium: A strategy for meeting the needs for marine-based research in the Arctic; ARICE; Autonomous buoy; BUOY_DRIFT; Buoy, drifting; HAVOC; Light; MOSAiC; MOSAiC20192020; Multidisciplinary drifting Observatory for the Study of Arctic Climate; optical; Polarstern; PS122/2; PS122/2_14-342; Ridges - Safe HAVens for ice-associated Flora and Fauna in a Seasonally ice-covered Arctic OCean; sub-surface  (1)
  • Arctic Ocean; Chaetoceros convolutus; Chaetoceros decipiens; Dinobryon balticum; Event label; Ice-St_04-1; Ice-St_04-2; MULT; Multiple investigations; Navicula pelagica; Nitzschia frigida; Phaeocystis pouchetii; Pseudo-nitzschia delicatissima; Rhizosolenia hebetata forma semispina; Station label  (1)
  • Biotic communities.  (1)
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  • 1
    Keywords: Biotic communities. ; Biodiversity. ; Freshwater ecology. ; Marine ecology. ; Climatology. ; Physical geography. ; Botanical chemistry. ; Ecosystems. ; Biodiversity. ; Freshwater and Marine Ecology. ; Climate Sciences. ; Physical Geography. ; Plant Biochemistry.
    Description / Table of Contents: Preface -- The marine physical environment during the Polar Night -- Light in the Polar Night -- Marine micro- and macroalgae in the Polar Night -- Zooplankton in the Polar Night -- Benthic communities in the Polar Night -- Fish ecology in the Polar Night -- Biological clocks and rhythms in polar organisms -- Sensor carrying platforms -- Operative habitat mapping and monitoring in the Polar Night -- The Polar Night exhibition: Life and light at the dead of night -- Index.
    Abstract: Until recently, the prevailing view of marine life at high latitudes has been that organisms enter a general resting state during the dark Polar Night and that the system only awakens with the return of the sun. Recent research, however, with coordinated, multidisciplinary field campaigns based on the high Arctic Archipelago of Svalbard, have provided a radical new perspective. Instead of a system in dormancy, a new perspective of a system in full operation and with high levels of activity across all major phyla is emerging. Examples of such activities and processes include: Active marine organisms at sea surface, water column and the sea-floor. At surface we find active foraging in seabirds and fish, in the water column we find a high biodiversity and activity of zooplankton and larvae such as active light induced synchronized diurnal vertical migration, and at seafloor there is a high biodiversity in benthic animals and macroalgae. The Polar Night is a period for reproduction in many benthic and pelagic taxa, mass occurrence of ghost shrimps (Caprellides), high abundance of Ctenophores, physiological evidence of micro- and macroalgal cells that are ready to utilize the first rays of light when they appear, deep water fishes found at water surface in the Polar night, and continuous growth of bivalves throughout the winter. These findings not only begin to shape a new paradigm for marine winter ecology in the high Arctic, but also provide conclusive evidence for a top-down controlled system in which primary production levels are close to zero. In an era of environmental change that is accelerated at high latitudes, we believe that this new insight is likely to strongly impact how the scientific community views the high latitude marine ecosystem. Despite the overwhelming darkness, the main environmental variable affecting marine organisms in the Polar Night is in fact light. The light regime during the Polar Night is unique with respect to light intensity, spectral composition of light and photoperiod. .
    Type of Medium: Online Resource
    Pages: XI, 375 p. 133 illus., 116 illus. in color. , online resource.
    Edition: 1st ed. 2020.
    ISBN: 9783030332082
    Series Statement: Advances in Polar Ecology, 4
    DDC: 577
    Language: English
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  • 2
    Publication Date: 2023-07-10
    Keywords: Arctic Ocean; Chaetoceros convolutus; Chaetoceros decipiens; Dinobryon balticum; Event label; Ice-St_04-1; Ice-St_04-2; MULT; Multiple investigations; Navicula pelagica; Nitzschia frigida; Phaeocystis pouchetii; Pseudo-nitzschia delicatissima; Rhizosolenia hebetata forma semispina; Station label
    Type: Dataset
    Format: text/tab-separated-values, 18 data points
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  • 3
    Publication Date: 2024-04-20
    Description: Three ice-tethered / floating systems measuring sub - sea-ice Photosynthetic Active Radiation (PAR) were deployed within the MOSAiC ice camp from February 2020, and recorded hourly data through to later summer 2020. These Optical Chain And Logger (OptiCAL) systems capture PAR-like data at 12 logarithmically-spaced levels down to 50 m depth, and, along with positional data, transmit these data hourly via Iridium. The PAR sensors have a wide dynamic range, able to detect PAR from 5x10⁻⁵ µMol s⁻¹ m⁻² to 100 µMol s⁻¹ m⁻² and thereby graph a wide range of light behaviour from winter to summer and from surface to depth. Sampling at the 12 levels is accomplished by resin-containment 'nodes' located along a power and communication cable that hangs vertically from the underside of the surface spar-buoy. The nodes are at nominal depths of 1, 2, 3, 4, 5, 6, 7, 9, 14, 21, 32, and 50m. Each node has six 'PAR' sensors, three detecting downwelling light and three upwelling light. Two of each set of three sensor sets have simple optical filters: one transmitting 'orange' the other 'blue'. The third sensor, being unfiltered, is 'white'. PAR data are archived in a CSV file as 'counts' from the sensors, and are in units of millihertz (mHz). The detail of the CSV format is provided in this directory (see "OptiCAL 'ee' buoy: Detail of the CSV format" under Documentation), but to convert from mHz to the expected SI unit of µMol s⁻¹ m⁻² requires a conversion function. Details of this conversion are provided in this directory (see "OptiCAL 'ee' buoy: Data description" under Documentation). The 'ee' unit was deployed in level ice by the Sea Ice Ridge Observatory in the MOSAiC Central Observatory. Its drift started at N 88.0312885, E 80.2587416, on 14th Feb 2020 and last data transmission was on the 2nd July 2020 due to battery power being exhausted. Intended recovery was not possible before positional data were lost. A field deployment report is included (see "OptiCAL 'ee' buoy: Field deployment report" under Documentation). This instrument was deployed as part of the project Ridges - Safe HAVens for ice-associated Flora and Fauna in a Seasonally ice-covered Arctic OCean (HAVOC), funded by the Research Council of Norway, project number: 280292 and Arctic Ocean ecosystems - Applied technology, Biological interactions and Consequences in an era of abrupt climate change (Arctic ABC Development, Research Council of Norway, project number: 245923). Ship-time associated to the participation of the DEARice team (D. Divine on leg 2) on the MOSAiC Expedition has been supported by the European Union's Horizon 2020 research and innovation programme under grant agreement No 730965 (ARICE).
    Keywords: 2020E1; ArcticABCDevelopment; Arctic Ocean; Arctic Ocean ecosystems - Applied technology, Biological interactions and Consequences in an era of abrupt climate change; Arctic Research Icebreaker Consortium: A strategy for meeting the needs for marine-based research in the Arctic; ARICE; Autonomous buoy; BUOY_DRIFT; Buoy, drifting; HAVOC; Light; MOSAiC; MOSAiC20192020; Multidisciplinary drifting Observatory for the Study of Arctic Climate; optical; Polarstern; PS122/2; PS122/2_14-342; Ridges - Safe HAVens for ice-associated Flora and Fauna in a Seasonally ice-covered Arctic OCean; sub-surface
    Type: Dataset
    Format: text/plain, 2 MBytes
    Location Call Number Expected Availability
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