| 1. |
- Frisk, Henrik, et al.
(författare)
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Acts of Creation : Introduction
- 2015
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Ingår i: Acts of Creation : Thoughts on artistic research supervision - Thoughts on artistic research supervision. - 9789187483165 ; , s. 7-18
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Bokkapitel (övrigt vetenskapligt/konstnärligt)
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| 2. |
- Lindberg-Sand, Åsa, et al.
(författare)
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Contextual and conceptual ambiguities in supervision of artistic research : experiences from Konstnärliga forskarskolan
- 2015
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Ingår i: Acts of Creation : thoughts on artistic research supervision. - 9789187483165 ; , s. 189-220
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Bokkapitel (refereegranskat)abstract
- To accept the nomination to become the supervisor of a PhD candidate is not only to step into a specific, challenging and potentially rewarding relationship, but also to enter a new zone of uncertainty: what kind of contribution to this relationship is expected from me? In what ways is this new professional task framed and supported by the institutional context to which I belong? What do I gain from becoming a supervisor? In this chapter we draw together our experiences of spending many hundreds of hours listening to and discussing with supervisors of PhD candidates from a wide variety of research domains. We use our experiences from ten years of arranging pedagogical support for supervisors in the form of courses and seminars, and use what we have learned in these meeting places as material to describe how we perceive the cultural and contextual conditions for supervising PhD candidates both in general and in the emerging field of artistic research. The aim is therefore not to describe or evaluate our pedagogical efforts, but to use what we have encountered and reflected on in seminars with supervisors over the years. Another aim is to shed some light on the cultural and contextual conditions for supervising artistic research by comparing and contrasting the situation of the supervisors in this relatively new field with the situation in other fields of research. A more personal aim is to try to disentangle some of the persistent puzzlement that followed us through the years with Konstnärliga forskarskolan (KFS). Why was it that over and over again we were troubled by a feeling that the supervisors, compared to our expectations, were not regarded as being crucially important for the development of artistic research?In this chapter we will first discuss the importance of supervisors for doctoral education and for the regeneration and development of research, both in general and for new fields, with continuous references to artistic research, as it was mirrored to us through KFS. We will then continue along a road where we look at a number of contextual conditions (such as the learning trajectories of artists) and practiced concepts (such as interdisciplinarity and practice-based research), where we have experienced intriguing differences in artistic research when compared to other research environments. Finally, we offer two scenarios staging the institutional and cultural conditions for supervising artistic research in two quite different ways. They are constructed as ideal types and as a tool to disentangle some of the ambiguities supervisors have to face in the real settings where they meet their PhD candidates, and where everything is mixed up, as in life itself. Finally, we end our chapter by pointing out a ghost scenario, which we hope will disappear with the continued development of artistic research.
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| 3. |
- Anrup, Roland, et al.
(författare)
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Centrala universitetsvärden hotas av bolagiseringsidén
- 2013
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Ingår i: Dagens nyheter. - 1101-2447.
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Tidskriftsartikel (populärvet., debatt m.m.)abstract
- Högskolestiftelser. Förslaget att driva svenska universitet i stiftelseform öppnar för bolagisering. Men det är ingen riktig utredning, utan en politisk pamflett utan eftertanke. Privatisering av universitet hotar både oberoendet, forskningskvaliteten och samhällsnyttan, skriver 36 forskare vid svenska högskolor och universitet.
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| 4. |
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| 5. |
- Brosse, Morgane, et al.
(författare)
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Conodonts from the Early Triassic Microbialite of Guangxi (South China) : Implications for the Definition of the Base of the Triassic System
- 2015
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Ingår i: Palaeontology. - : Wiley. - 0031-0239 .- 1475-4983. ; 58:3, s. 563-584
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Tidskriftsartikel (refereegranskat)abstract
- We describe a new Early Triassic (Griesbachian) succession of conodont faunas from a high-resolution sampling of the basal Early Triassic microbial limestone and the base of the overlying unit at the Wuzhuan section (Nanpanjiang Basin, Guangxi, South China). The microbial limestone records the earliest phase of the Early Triassic biotic recovery after the end-Permian mass extinction. For the first time, rich conodont faunas are reported from within the microbialite. The faunas from Wuzhuan are largely dominated by anchignathodontids, including several Isarcicella species, which were previously documented only from strata above the microbialite. A total of 14 conodont species assigned to three genera is recorded from the Wuzhuan section. Starting from the base of the microbialite upwards, several species are sequentially added to the conodont assemblage. The alpha diversity peaks at the top of the microbialite. The conodont record in the considered microbialite interval at Wuzhuan is presumably unaffected by local ecological changes. It therefore more likely represents an evolutionary rather than an ecological pattern. We compare the Wuzhuan's conodont record with a well-supported phylogenetic model and suggest that the sequence of first occurrences at Wuzhuan is the closest to the true' sequence of evolutionary events that took place during this Griesbachian radiation of anchignathodontids. Based on comparisons with the GSSP section at Meishan, we suggest further that the first occurrence of Hindeodus parvus in Meishan does not correspond to its first appearance datum.
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| 6. |
- Brosse, Morgane, et al.
(författare)
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New data from Oman indicate benthic high biomass productivity coupled with low taxonomic diversity in the aftermath of the Permian-Triassic Boundary mass extinction
- 2019
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Ingår i: Lethaia. - : WILEY. - 0024-1164 .- 1502-3931. ; 52:2, s. 165-187
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Tidskriftsartikel (refereegranskat)abstract
- A new Early Triassic marine fauna is described from an exotic block (olistolith) from the Ad Daffah conglomerate in eastern Oman (Batain), which provides new insights into the ecology and diversity during the early aftermath of the Permian-Triassic Boundary mass extinction. Based on conodont quantitative biochronology, we assign a middle Griesbachian age to the upper part of this boulder. It was derived from an offshore seamount and yielded both nektonic and benthic faunas, including conodonts, ammonoids, gastropods and crinoid ossicles in mass abundance. This demonstrates that despite the stratigraphically near extinction at the Permian-Triassic Boundary, Crinoidea produced enough biomass to form crinoidal limestone as early as middle Griesbachian time. Baudicrinus, previously placed in Dadocrinidae, is now placed in Holocrinidae; therefore, Dadocrinidae are absent in the Early Triassic, and Holocrinidae remains the most basal crown-group articulates, originating during the middle Griesbachian in the Tethyan Realm. Abundant gastropods assigned to Naticopsis reached a shell size larger than 20 mm and provide another example against any generalized Lilliput effect during the Griesbachian. Whereas the benthic biomass was as high as to allow the resumption of small carbonate factories, the taxonomic diversity of the benthos remained low compared to post-Early Triassic times. This slow benthic taxonomic recovery is here attributed to low competition within impoverished post-extinction faunas.
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| 7. |
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| 8. |
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| 9. |
- Ebbestad, Jan Ove R., et al.
(författare)
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Gastropods and tergomyans from the Upper Ordovician (Viru–Harju) of the Fågelsång area, Scania, southern Sweden
- 2013
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Ingår i: Journal of Systematic Palaeontology. - : Informa UK Limited. - 1477-2019 .- 1478-0941. ; 11:3, s. 295-336
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Tidskriftsartikel (refereegranskat)abstract
- A diverse tergomyan and gastropod assemblage is described from the Global Boundary Stratotype Section and Point (GSSP)section of the Sandbian Stage, Upper Ordovician, in the Fågelsång area, Scania, southern Sweden. Deep water graptolitic mudstone and shale comprise the succession, and previously only one gastropod species was known. The new material spans the Sularp Formation through the Lindegård Mudstone (Nemagraptus gracilis–Dicellograptus complanatus biozones). Fourteen species are described: two tergomyan, five bellerophontoid gastropods, and seven anisostrophically coiled gastropods.Three species are new: Peelerophon hodites, Tetranota scanica and Lophospira sandbiana. Three taxa (Tritonophon subtrilobatus,Tetranota scanica and Holopea mobergi) are found high in the Lindegård Mudstone (Vormsi–Pirgu stages). Cyrtodiscus, Peelerophon and Tritonophon are recorded for the first time in Baltoscandia. Some taxa may have been transportedfrom shallower water settings, whereas species of Peelerophon, Joleaudella, Mestoronema and Sinuites may have been partof the local benthos. Except for Bucania erratica, no species are shared with the fauna of the coeval Dalby Limestone in Sweden. Deaechospira elliptica, common in the Dalby Limestone, is not recorded at Fågelsång, although two closely relatedspecies are found (Deaechospira rotunda and Deaechospira? sp.). The Fågelsång assemblage has more in common with the older to coeval fauna of the Elnes and Arnestad formations in the Oslo Region, Norway (e.g. sharing Joleaudella, Sinuites, Mestoronema and Pararaphistoma). The Sandbian fauna of Fågelsång includes peri-Gondwanan taxa, e.g. Cyrtodiscus,Peelerophon and Deaechospira. Nevertheless, cluster analysis reveals that the faunas of Baltica and Laurentia were most similar, whereas faunas from Perunica and Baltica remained distinct and separated during the Darriwilian–Sandbian. The few similarities may result from spread of a temperate fauna supplementing rather than replacing taxa in deep water assemblages.The main Fåagelsång assemblage coincides both with the Baltoscandian Middle Caradoc Faunal Turnover and the Gutenberg Carbon Isotope Excursion.
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| 10. |
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