322,890 research outputs found
Stenus ceramicola PUTHZ 1994
Stenus ceramicola PUTHZ 1994 spec. propr. Stenus piliferus ceramicola PUTHZ 1994b: 54. Der sklerotisierte Innenring des Medianlobus (vgl. Abb. 1, l. c.) – ähnlich wie bei S. hirtellus SHARP – stellt einen klaren Unterschied zu S. piliferus und seinen Subspezies dar, deshalb muss dieses Taxon aufgewertet werden.Published as part of Puthz, V., 2013, Übersicht über die orientalischen Arten der Gattung Stenus LATREILLE 1797 (Coleoptera, Staphylinidae) 330. Beitrag zur Kenntnis der Steninen, pp. 1279-1470 in Linzer biologische Beiträge 45 (2) on page 1361, DOI: 10.5281/zenodo.530092
Submarine Mass-Movements Along the Slopes of the Active Ionian Continental Margins and Their Consequences for Marine Geohazards (Mediterranean Sea)
The Ionian margins of Calabria and Apulia (IMCA) have been affected by mass movements of varying style, scale and age. Here we present examples of seabed and subsurface features identified along more than 400 km of the IMCA from multibeam seabed imagery and subbottom profiles acquired by OGS since
2005. Four different types of mass movement phenomena are recognized with expression at seabed and in the shallow subsurface: (1) mass transport complexes (MTCs) within intra-slope basins, (2) isolated slide scars (ISS) along open slopes, (3) slope-parallel sediment undulations (SPSU) recording block-rotations linked to fluid migration, and (4) headwall and sidewall scarps (HSC) in submarine canyons.
Preliminary analyses of sedimentary processes suggest that both open-slope failures capable of triggering tsunamis and retrogression of canyon headwallswithin 1–3 km
of the Calabrian coast represent potential geohazards for coastal populations and offshore infrastructures
Textural and mineralogic characteristics of sediment cores from mud volcanoes on the Calabrian Arc, Northern Ionian Sea.
Submarine Canyon dynamics - Executive summary
Ceramicola, S. ... et al.-- Submarine Canyon Dynamics in the Mediterranean and Tributary Seas - An integrated geological, oceanographic and biological perspective, 15-18 April 2015, Sorrento, Italy.-- 14 pages, 6 figures, 1 tableThis synthesis, sketched during the course of the workshop discussions, was developed and consolidated in the months thereafter thanks to further inputs, assembled by Silvia Ceramicola, that were received from the meeting participants. The editor, Frederic Briand, reviewed and edited the entire Monograph, with special attention to this opening chapter where his correspondence with Peter Harris, Pere Puig, Namik Çağatay, Marie-Claire Fabri and David Amblas was particularly useful. His gratitude is extended to Valerie Gollino for attending to the physical production of the Monograph under tighter deadlines than usualPeer Reviewe
Tectonically-driven mud volcanism since the late Pliocene on the Calabrian accretionary prism, central Mediterranean Sea
Active tectonics in the Calabrian Arc: Insights from the Late Miocene to Recent structural evolution of the Squillace Basin (offshore eastern Calabria)
The Calabrian Arc represents one of the most active sectors of the upper plate of the Tyrrhenian-Ionian subduction
system. This research aims to reconstruct the evolution of the Squillace Basin (Ionian offshore of the
Calabrian Arc) from the Late Miocene to Recent times and recognise active shallow and deep structures using a
multiscale approach. The latter is based on interpreting high-penetration and high-resolution seismic reflection
profiles, calibrated with well-log data coupled with bathymetric data and the distribution of instrumental
earthquakes. Data highlight three steps in the evolution of the Squillace Basin. A Late Miocene extensional event
led to the formation of WNW-ESE oriented horst and half-graben structures. During the Pliocene, deformation
was localised in the central and northern sectors of the basin and expressed by a WNW-ESE oriented strike-slip
fault and NW-SE normal to trastensional faults, respectively. A transpressional event started in the Early Pleistocene,
causing the positive inversion of deep (> 3 km) extensional faults and the formation of NW-SE to WNWESE
oriented transpressional/reverse faults and related anticlines. The kinematics of these faults agree with the
NW-SE oriented left-lateral Albi-Cosenza, Lamezia-Catanzaro and Petilia-Sosti crustal fault zones developed in
north Calabria. The results of this work suggest that the transpressional structures in the northwestern sector of
the basin likely represent the offshore prolongation of the Albi-Cosenza fault zone. NW-SE to WNW-ESE trending,
shallow (<2 km) high-angle normal faults offset the younger deposits. Their depth and direction indicate that
these faults are secondary structures formed in the extrados of the anticlines associated with the transpressional
faults. The distribution of earthquakes shows events with M > 3 and depth <15 km located in the hanging wall of
transpressional faults. The integrated data suggest that these structures are active and probably responsible for
the major earthquakes that affected the Ionian offshore
Diffusive author(s), cohesive author: Analysis of S/N (1994)
This study indicates the ways in which various aspects of the author(s) are brought forth in Dumb type’s performance art, the S/N production. Previous research has suggested a non-hierarchical organization of Dumb type and the absence of a “privileged author” in Dumb type’s collaborative work, S/N. However, the results that I have investigated from member’s interviews on the creative process of S/N along with my analysis of the recorded images of S/N, indicate a different aspect of the author(s). First, S/N was created through, so to speak, the collective ideas of the members of Dumb type. Further, S/N has at least nine quotations from previous performances, installations, and printed writings, besides the work-in-progress technique. Explicating one of the “author functions” as given by Michel Foucault, each text has plural subjects of the author. However, it has been revealed from members’ interviews that Teiji Furuhashi had a decision-making role in selecting the members’ ideas within the performance. Since then, S/N has had plural subjects of creation; however, Furuhashi is one of the subjects of creation along with the “privileged author.” S/N has plural authors (diffusive authors) yet at the same time, it has a “privileged author,” Teiji Furuhashi (cohesive author)
Going Beyond Counting First Authors in Author Co-citation Analysis
The present study examines one of the fundamental aspects of author co-citation analysis (ACA) - the way co-citation
counts are defined. Co-citation counting provides the data on which all subsequent statistical analyses and mappings
are based, and we compare ACA results based on two different types of co-citation counting - the traditional type that
only counts the first one among a cited work's authors on the one hand and a non-traditional type that takes into
account the first 5 authors of a cited work on the other hand. Results indicate that the picture produced through this non-traditional author co-citation counting contains more coherent author groups and is therefore considerably clearer. However, this picture represents fewer specialties in the research field being studied than that produced through the traditional first-author co-citation counting when the same number of top-ranked authors is selected and analyzed. Reasons for these effects are discussed
Methane Seepage on Mars: Looking for analogues from submarine fluid flow systems on Earth
Methane Seepage on Mars: Looking for analogues from submarine fluid flow systems on Eart
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