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Volcanoes
\"Volcanoes are a natural part of the process in the formation of Earth. Learn the different types, how they form, which ones have done the most damage, and what we are doing to mitigate their destructive power.\"-- Provided by publisher.
Book
Vertical distribution of megafauna on the Bering Sea slope based on ROV survey
Video surveys were carried out during the 75th cruise of the RV Akademik M.A. Lavrentyev (June 2016) along the northern slope of the Volcanologists Massif, in the south-western Bering Sea. The seafloor was explored using the ROV Comanche 18 . Seven dives were performed in the depth range from 4,278 m to 349 m. Overall, about 180 species of megafauna were recognised. Fifteen types of megafauna communities corresponding to certain depth ranges were distinguished based on the most abundant taxa. Dominance changed with depth in the following order: the holothurian Kolga kamchatica at the maximum depth (4,277–4,278 m); the holothurian Scotoplanes kurilensis at 3,610–2,790 m; the ophiuroid Ophiura bathybia at 3,030–2,910 m; benthic shrimps of the family Crangonidae at 2,910–2,290 m; the holothurian Paelopatides solea at 2,650–2,290 m; benthic jellyfish from the family Rhopalonematidae at 2,470–2,130 m; the enteropneust Torquaratoridae at 2,290–1,830 m; the holothurian Synallactes chuni and the ophiuroid of the genera Ophiura and Ophiocantha at 1,830–1,750 m. At depths 1,750–720 m most of the megafauna was associated with live or dead colonies of the sponge Farrea spp. Depths 720–390 m were dominated by the coral Heteropolypus ritteri and/or Corallimorphus pilatus. At 390–350 m depth, the shallowest depth range, the dominant taxon was the zoantharian Epizoanthus sp. Soft sediment megafauna communities dominated by torquaratorid enteropneusts to our knowledge have not been observed before in the deep-sea, the same as communities with a dominance of benthopelagic rhopalonematid jellyfish. The depths of the largest community changes, or the largest turnover of dominant species, were revealed at ∼2,790 m between the bathyal and abyssal zones and ∼1,750 m and ∼720 m within the bathyal zone.
Journal Article
Volcanologists : examining active volcanoes
See what a volcanologist does through case studies, photographs, and interviews with the people who study volcanoes.
Book
Some Biogeochemical Characteristics of the Trace Element Bioaccumulation in the Benthic Fauna of the Piip Volcano (The Southwestern Bering Sea)
The Piip Volcano is a submarine volcanic edifice occupying the central part of the Volcanologists Massif in the southwestern Bering Sea, with two tops, southern and northern. The minimum depth of the northern top is located at 368 m, and of the southern at 464 m. Active hydrothermal venting occurring at both summits of the volcano supports diverse biological communities, including animals specific for chemosynthetic habitats. In benthic organisms inhabiting the northern and southern tops of the Piip Volcano, for the first time, we examined distribution patterns of the following trace elements: titanium, vanadium, chromium, manganese, iron, nickel, copper, zinc, arsenic, selenium, zirconium, molybdenum, silver, cadmium, antimony, barium, tungsten, lead, bismuth, and uranium. The element contents were quantified by the ICP-MS. Total carbon (TC) and total inorganic carbon (TIC) were determined using a Shimadzu TOC-L-CPN and mineral composition of sediment was determined using the XRD. In the water of the biotope from the northern top, concentrations of Mn, Zn, Ag, Cd, Sb, W, Pb were 2–6 times, and Ba was 50 times higher than those from the southern top. This was attributed to the lower temperature of fluids emanating at the southern top. An abundant population of Calyptogena pacifica (Bivalvia: Vesicomyidae: Pliocardiinae) was found only at the southern top. The main target of most trace elements, such as Fe, V, Cr, Co, Ni, Zn, As, Mo, Ag, Cd, W, Pb, Bi, and U were the soft parts of Calyptogena pacifica (with high TOC content, on average 53.1% in gills and 49.6% in the rest of the body). Gills were characterized by particular high contents (>100 µg g−1 dry w.) of Zn, Cd, Fe, Ni, Cu, and Pb, which can form sulphides or be associated with them. Shells of C. pacifica, as well as Brachiopoda, were depleted in these elements, as well as tissues of the carnivores Paguridae (Crustacea) and Actiniaria (Anthozoa). In suspension feeders from both tops, the lower contents of most elements were detected. Estimation of Biological Concentration Factor (BCF) for most elements varied from 102 to 104, reaching n105 for Ni, Zn, Ag, Cd, and Pb. A significant difference in BCF values between Fe and Mn was revealed.
Journal Article
Volcanologist
Introduces the field of volcanology, explaining the necessary educational steps, useful character traits, potential hazards, and daily job tasks related to this occupation.
Book
Hazard communication by volcanologists: Part 1 - Framing the case for contextualisation and related quality standards in volcanic hazard assessments
Scientific communication is one of the most challenging aspects of volcanic risk management because the complexities and uncertainties of volcanic unrest make it difficult for scientists to provide information that is timely, relevant, easily comprehensible and trusted. When poorly handled, scientific communication can cause social, economic and political problems, and undermine community confidence in disaster management regimes.
This is the first of two related papers that together investigate the interface between the scientific consideration of volcanic hazards and the governance of volcanic risks. Both papers are principally concerned with issues of risk governance, and their focus is hazard communication by volcanologists at this hazard-risk interface (the interface) during periods of volcanic unrest. In this paper, we argue that the working practices of contextualisation must be more methodical and propose four quality assurance standards that will enhance hazard assessments.
To improve hazard communication between volcanologists and risk-mitigation decision-makers (decision-makers), we argue that volcanologists need to adopt a more iterative and structured approach that openly embraces the benefits, and confronts the challenges, of stakeholder-orientated ‘contextualisation’.
Our analysis of the published literature reveals evidence of a slow paradigm shift from practices based upon strict linear technocratic approaches to more iterative stakeholder participation. The extent of this shift varies in different regions, however, the rules and practices of deliberation often appear
ad hoc
and unstructured.
Since there is currently insufficient guidance for managing the practicalities and standards of contextualisation, we introduce two novel concepts; the
‘scrutiny dimension’
of risk governance, which is the slow changing governance context that may influence the processes of contextualisation, and the dynamic
‘equilibrium of contextualisation’
, which is the metastable product of regulatory standards, natural and organisational constraints, and stakeholder pressures.
We argue that the working practices of contextualisation must be more structured and should strive to be open, transparent and fully articulated. Contextualisation, which meets proposed quality assurance standards of materiality, proximity, comprehensibility and integrity, will enhance hazard assessments and, thereby, the utility of their outputs. In our second paper (Bretton et al, J Appl. Volcanol. DOI 10.1186/s13617-018-0079-8, 2018), the focus is directed away from the perceived qualities of more ‘socially robust’ hazard assessments towards the actual process of contextualisation.
Journal Article