Hylemya Floralis (Fallen) (Dipt., Anthomyiidae)

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Hylemya Floralis (Fallen) (Dipt., Anthomyiidae) NORSK ENTOMOLOGISK TIDSSKRIFT NORWEGIAN JOURNAL OF ENTOMOLOGY VOLUME 19· NO. 1 . 1972 Sip..... Higyar " Elvind 0 tbye: QU8IItitative Tore Randalff Nielsen: Syrphtdae (Dlpt.) from and Qualitative InvestiptlOllll of the Invertebrate JlI!I'eIl, Norway, n. 63 Fauna under Stones (the HypoUtbion) in Some Hans Mendl " Jobn O. Solem: Notes on Nonve- Alpine HaWtats at FInse. Soutb Norway 1 glaD LImonllnae (Dlptera, Tlpalidae) 73 0I'IDIl Dlclc.er "F. L. Waterbouse= Life History Jobn O. Solem: The Larva or ARJ1Iylea eognate118 of Geograpbic8IIy Dift'erent Popu­ McLadllan (Trlcboptera, Hydroptllidae) 77 of Ephestia eauteDa (Walker) (Lep. Phy­ Trygve Rygg " Laurib Somme: Oviposition and ) in Gnulient Environments 11 Larval Development of Hylemya f1ora1is (Fanen) ErliIgHauge: ew ReeonIs ofSpidersfrom Norway 17 (Dlpt., Antbomylidae) on varieties of Swedes and La S6mJDe " Trygve Rygg: Tbe Eft'eet of Turnips 81 Plmlical lUId Chemical StlmuU on Oviposition In Tore Ranclulff ielsen: Platycheirus monticulus DOV. floraIis (FaDm) (Dipt., AntbomyUdae) 19 sp., a ortbem Species Confused w1tb P. d1sci- MOI!lUd HDaU, Hans K. Dable " KjeU Aurstad: manus Loew (Dlpt., Syrpbldae) 91 Life History and Food-8polling Enzymes of Der­ Tont. Solb6y: Quantitative Invertebrate Studies IardarIus (L.) 25 In Mountain Communities at Hardangervldda, sa...: Eft'eet of Temperature on Develop­ South Norway. I. 99 of Thomaslniana tbeobeIdl Bames (Dlpt., Ced":yIdae) 33 Short CommunieatiOllll ......HAgvar " Slgmund HAgvar: Cban­ John O. Solem: Macroplea appendiculata Panz. aM Coleopterous Fauna Associated witb (CoL, CbrysomeUdae) New to Norway 109 tional Stages of the Fungus Leceinum Kaare Aagaard " John O. Solem: ParasemJdaUs telIbteeoseallll'Ulll (Seer.) Sing. (BoIetaaae) 39 f'uscipennls Rentei' (Neuroptera, Coniopterygidae) IfojPalIll: TtpuJa exelsa Sebum. (Dlptera, Dy for Norge 110 ·"'IidIM!), LIfe Cycleand Population Dyaamics 43 Kaare Aal8ard: Nye funn av saksedyr (Dermap- • Waaler: Spiders (Araneae) from .lnpaker, ten) I orge 110 49 Erllng Hauge: Notes on Norwegian Spiders, m. Ul FJelIM:r.. PreseIIt and Late WelcbseIian Qc­ TOI'e Randulft'NIeIsen: Syrpbidae (Dlpt.) from Orm- caTll8ee of Corynocera ambIRUa Zeat. (Dlpt.. tjemkampen National Park 111 OdIl'ClMJlUIlae) In orway 9 &_~_ lU UNIVERSITETSFORLAGE Norsk Entomologisk Tidsskrift Norwegian Journal ofEntomology EDITOR Dr. philos. Lauritz Sl'!mme, Zoologisk laboratorium, Universitetet Oslo, Blindern, Oslo 3, Norway. EDITORIAL SECRETARY Vit. ass. Fin-Christian Tandberg. EDITORIAL COMMITfEE Universitetslektor Eivind 6stbye, Konsulent Per F. Waaler. PUBLISHER Universitetsforiaget: P. O. Box 307, BIindern, Oslo 3, Norway. P. O. Box 142, Boston, Massachusetts 02II3, U. S. A. CONTRIBUTIONS These should be sent to the Editor. Authors are requested to follow the instructions on page 3 of the cover. Artikler som I'!nskes trykt i tidsskriftet sendes redakt0ren. Bidragsytere ma fl'!lge anvis­ ningen pa omslagets tredje side. SUBSCRIPTIONS Non-members of the Norwegian Entomological Society should send their orders to Uni­ versitetsforlaget. The subscription price per volume (two issues annually) is U.S. $ 7.50. (N. kr. 45,-). Notice of change of address should be accompanied by the old address. Back volumes should also be ordered from Universitetsforiaget. NORSK ENTOMOLOGISK FORENING ser sin hovedoppgave i a fremme det entomologiske studium i Norge, og danne et binde­ ledd mellom de interesserte. Sl'!knad om opptagelse i foreningen sendes formannen. Med­ lemskontingenten er for tiden kr. 20,- pr. ar. Medlemmer far tidsskriftet fritt tilsendt. STYRET Formann: Forsl'!ksleder, dr. philos. Alf Bakke, Det norske Skogforsl'!ksvesen, 1432 VolIebekk. Visejormann: Konsulent Per F. Waaler, Kristins vei 30, Oslo. Sekreta!r: Amanuensis Trygve Rygg, Statens plantevern, 1432 VoIIebekk. Styremedlem: Vit. ass. Eline Benestad Hagvar, Zoologisk laboratorium, Universitetet i Oslo. Kasserer: Vit. ass. Bjarne Meidell, Zoologisk Museum, Universitetet i Bergen. Styrets varamenn: Dr. Andreas Strand, Melumveien 38, Oslo. Konservator Johan Andersen, Tromsl'! Museum, Tromsl'! Revisor: Brukseier Eivind Sundt, Sl'!ndre Oppegard, Svartskog. © Universitetsforlaget 1972 Contribution from the Norwegian1BP/PT-UM sections Quantitative and Qualitative Investigations of the Invertebrate Fauna under Stones (the Hypolithion) in Some Alpine Habitats at Finse, South Norway SIGMUND HAGVAR & EIVIND oSTBYE Hagvar, s. & Ostbye, E. 1972. Quantitative and Qualitative Investigations of the Invertebrate Fauna under Stones (the Hypolithion) in Some Alpine Habitats at Finse, South Norway. Norsk ent. Tidsskr. 19,1-10. In five alpine habitats (1220-1350 m a.s.\.) at Finse, South Norway, the in­ vertebrate fauna under stones was studied qualitatively and quantitatively during the summers of 1969 and 1970. The stone cover of the ground varied from less than 5% to about 30%, and the majority of stones could be turned by hand. Typical soil animals, and Collembola and Acarina were not col­ lected. The data are compared with quantitative quick trap collections from litter and vegetation between stones in three habitats at Stigstuv (approx. 36 km from Finse, 1210-1240 m a.s.!.). In the comparisons, Oligochaeta. Collembola, and Acarina are excluded. The hypolithic fauna is very rich. containing about the same orders, and to a certain extent the same families. as found in litter and vegetation. In the hypolithic communities, Araneida dominate in number (52-99%), while Araneida never make up as much as 50% of the individuals between stones. The density of invertebrates between stones at Stigstuv may be more than ten times higher than under stones at Finse. However, the density of Araneida under stones was almost as high as between stones. The mean weight of hypolithion ranged from 66 to 157 mg per m2 of stones turned. Araneida seemed to prefer stones that covered about 400 cm2 of the ground. When the energy flow of a habitat is estimated, the hypolithion has to be included. S. Hagvar & E. 6stbye, Zoological Laboratory, University of Oslo. Blindem, Oslo 3, Norway Very little work has been done on the quantity favourable and relatively constant microc1imat­ and quality of the invertebrates living under ic conditions, compared with most other habi­ stones, and their role in the ecosystems. Schon­ tats in this region (Mani 1968). The impor­ born (1961) uses the term 'hypolithion' for tance of stones for invertebrates has also been this fauna. He groups the fauna into three investigated by Brundin (1934), Cole (1946), vertical layers: fauna living on the under SliT­ and Balogh (1958), and the rich hypolithion in face of the stone, fauna living on the litter SliT­ high mountains has been stressed by Kiihnelt face, and fauna present in the litter layer. If (1970). After several years of experience it is the litter layer is wanting under the stone, then felt that this faunal component is of great the second (and last) group of animals are importance in Norwegian mountain areas. those living on the true soil surface. At Finse the lower hypolithic layer of Schon· The hypolithion always has a characteristic born (1961) is lacking. All the majJr plant species composition in a given area (Schonborn communities in the study area cont::dn varying 1961), and the fauna is also very uniform on a degrees of stone cover. The hypolithion of five world basis (Tischler 1955). In high mountains different plant communities has been investi­ above the timber line, thehypolithic habitats gated. become especially important, because of the This paper is part of an analysis of a high 1 - Norsk ent. Tidsskr. 2 S. Hagvar & E. Vstbye mountain ecosystem being carried out under of 1300 m. The area is relatively flat. and the leadership of the second author. The au­ stones and barren rocks cover about 10 % of thors shared the planning of this study and the the surface. Some boulders are present in a sampling of the materia!' The treatment of the small part of the area. Most of the hypolithic data and the main task of writing is the respon­ area is covered by stones which can be turned sibility of the first author. by hand. The soil has a high humidity, and there are tussocks in some places. The domi­ nant plants are mosses, and Carex sp. Polygonum viviparum and Salix herbacea are STUDY AREA also common. The study area at Finse is located in the C. The oligotrophic dry heath. The next habi­ north-western part of the Hardangervidda tat represents oligotrophic dry heath communi­ mountain plateau (60°36' N- r30' E) and ties located approximately 2.5 km from the consists of five habitats situated in the mid­ glacier at 1230 m a.s.!. This study area is rela­ alpine region in the area between the Finse­ tively flat. Most of the stone cover is repre­ vatn lake (1214 m a.s.!') and the Blaisen glacier sented by boulders, and only a smaller part of (1390 m a.s.!.), one of the largest outlets of the the hypolithic area is covered by stones which Hardangerjokulen glacier. They form parts of can be turned by hand. Altogether stones a north-sloped succession gradient, going from cover 5-10 % of the habitat. Cladonia rangije­ recently free-laid ground in front of the glacier rina, Cl. silvatica, and Carex bigelowii to the presumed climax community of this dominate, but mosses and Empetrum herma­ area. A fully detailed description of the geo­ phroditum are also common. morphology, pedology, and plant cover of the D. The snow bed. This site can be character­ study area will appear elsewhere. Therefore ized as a Salix herbacea-snow bed, situated on only a brief description of the plant cover of a north-faced slope, approximately 2.6 km the habitats under study will be given here. from the glacier at an altitude of 1220 m. In A. The pioneer community. The first habitat this type of habitat there are large snow accu­ is characterized by a pioneer vegetation (in the mulations during winter. A distinct solifluction text referred to as the pioneer community), occurs during the melting period. Stones cover located 800 m from the glacier at an altitude 15-20 % of the habitat, and most of them can of 1350 m.
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