DOCSLIB.ORG

Spatial Distribution of Benthic Foraminiferal

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Spatial Distribution of Benthic Foraminiferal EGU Journal Logos (RGB) Open Access Open Access Open Access Advances in Annales Nonlinear Processes Geosciences Geophysicae in Geophysics Open Access Open Access Natural Hazards Natural Hazards and Earth System and Earth System Sciences Sciences Discussions Open Access Open Access Atmospheric Atmospheric Chemistry Chemistry and Physics and Physics Discussions Open Access Open Access Atmospheric Atmospheric Measurement Measurement Techniques Techniques Discussions Open Access Biogeosciences, 10, 4433–4448, 2013 Open Access www.biogeosciences.net/10/4433/2013/ Biogeosciences doi:10.5194/bg-10-4433-2013 Biogeosciences Discussions © Author(s) 2013. CC Attribution 3.0 License. Open Access Open Access Climate Climate of the Past of the Past Discussions Spatial distribution of benthic foraminiferal stable isotopes and Open Access Open Access dinocyst assemblages in surface sediments of the Trondheimsfjord,Earth System Earth System central Norway Dynamics Dynamics Discussions G. Milzer1, J. Giraudeau1, J. Faust2, J. Knies2, F. Eynaud1, and C. Rühlemann3 Open Access 1Université de Bordeaux, CNRS, UMR5805 EPOC, Talence, France Geoscientific Geoscientific Open Access 2Geological Survey of Norway (NGU), Trondheim, Norway Instrumentation Instrumentation 3 Federal Institute for Geosciences and Natural Resources (BGR), Hannover, Germany Methods and Methods and Correspondence to: G. Milzer ([email protected]) Data Systems Data Systems Discussions Open Access Received: 4 February 2013 – Published in Biogeosciences Discuss.: 26 March 2013 Open Access Revised: 22 May 2013 – Accepted: 23 May 2013 – Published: 1 July 2013 Geoscientific Geoscientific Model Development Model Development Abstract. Instrumental records from the Norwegian Sea and thic foraminiferal isotopes reliably mirror the complex fjord Discussions the Trondheimsfjord show evidence that changes of bot- hydrology and can be used as proxies of Holocene climatic Open Access tom water temperature and salinity in the fjord are linked variability. Open Access to the salinity and temperature variability of the North At- Hydrology and Hydrology and lantic Current (NAC). Changes in primary productivity and Earth System Earth System salinity in the surface and intermediate water masses in the Trondheimsfjord as well as the fjord sedimentary budget are 1 Introduction Sciences Sciences mainly driven by changes in riverine input. In this study Discussions Open Access we use 59 surface sediment samples that are evenly dis- The North Atlantic Current (NAC) is the prolongationOpen Access of the tributed in the fjord to examine whether dinocyst assem- Gulf Stream and transports warm and saline water north- Ocean Science blages and stable isotope ratios of benthic foraminifera re- ward along the NorwegianOcean continental Science margin (Ganachaud flect the present-day hydrology and can be used as palaeo- and Wunsch, 2000). This poleward NAC flow essentially Discussions ceanographic proxies. In general, modern benthic δ18O and contributes to the deep water formation in the Nordic Seas δ13C values decrease from the fjord entrance towards the and strongly affects the northern European climate (Vellinga Open Access fjord head with lowest values close to river inlets. This is es- and Wood, 2002). The hydrology of NorwegianOpen Access fjords, ad- sentially explained by gradients in the amounts of fresh wa- joining the Norwegian Sea, is equally linked to the NAC and Solid Earth ter and terrigenous organic matter delivered from the hinter- the Norwegian Coastal CurrentSolid (NCC) Earth (Sætre, 1999; Eilert- land. The distribution of benthic δ13C ratios across the fjord sen and Skarðhamar, 2006; Sætre, 2007). Many fjords have Discussions is controlled by the origin (terrigenous vs. marine) of or- a bedrock threshold at the entrance causing a complex hy- ganic matter, local topography-induced variability in organic drology linked to the ocean currents in the adjacent sea, as matter flux at the water–sediment interface, and organic mat- well as their salinity and temperature structure,Open Access wind dynam- Open Access ter degradation. The dinocyst assemblages display the varia- ics, and riverine input (Inall and Gillibrand, 2010 in Howe et The Cryosphere tions in hydrography with respect to the prevailing currents, al., 2010). Additionally,The fjords Cryosphere are semi-enclosed basins and Discussions the topography, and the freshwater and nutrient supply from act as natural sediment traps with high accumulation of ma- rivers. The strength and depth of the pycnocline in the fjord rine and terrigenous sediments. As a consequence fjord sed- strongly vary seasonally and thereby affect water mass char- iments bear a combined signature of marine, continental and acteristics as well as nutrient availability, temporally creating atmospheric environments and processes. Norwegian fjords local conditions that explain the observed species distribu- are therefore excellent locations for high resolution studies tion. Our results prove that dinocyst assemblages and ben- of the temporal variations in the physico-chemical character- istics of the NAC and NCC as well as the regional climate Published by Copernicus Publications on behalf of the European Geosciences Union. 4434 G. Milzer et al.: Benthic foraminiferal stable isotopes and dinocyst assemblages (Cage and Austin, 2008; Alve et al., 2011). The objective of ever, more sensitive to post-depositional effects than others, this study is to examine if micropaleontological proxies de- and bottom and pore water oxygenation may alter the origi- riving from sediments from the Trondheimsfjord reflect the nal cyst assemblage (Zonneveld et al., 1997, 2007). main elements of present-day oceanography and hydrology. Hence, in the following we will investigate benthic stable The motivation for this examination implies the question to isotopes and dinocyst assemblages across this particular fjord which extent these proxies from fjord sedimentary archives environment with regard to the hydrological conditions and can be used to determine changes in oceanographic regimes sediment characteristics. in the recent past (Holocene). In order to grasp the complex hydrological and environmental patterns of the bottom and surface waters in the Trondheimsfjord we analysed the stable 2 Physical settings and oceanography isotope composition of the benthic foraminifera Melonis bar- leeanus and organic-walled dinoflagellate cyst assemblages The following oceanographic and hydrological overview is from 59 surface sediment samples evenly distributed along mainly based on Jacobson (1983) which contains a detailed the fjord’s axis. description of the geomorphology and the main circulation Stable isotope ratios were analysed to determine bottom processes affecting the hydrology of the Trondheimsfjord. water characteristics and sediment dynamics in the fjord. Moreover, we used monthly hydrographical data and mea- Oxygen isotopes in calcite tests are conventional tools for surements from three mooring stations as well as CTD mea- the reconstruction of the past climate since the calcification surements conducted in April 2011 (Fig. 2) to further illus- processes are considered to occur in close equilibrium with trate the fjord hydrological context. the surrounding sea water (e.g. Urey, 1946; and Shackleton The Trondheimsfjord is located at the coast of mid Norway and Opdyke, 1973). The foraminiferal 18O/16O isotope ratio extending from 63◦400 N, 09◦450 E at Ørland to 64◦450 N, (δ18O) denotes the isotopic composition of the water linked 11◦300 E at the fjord head at Verdal (Bøe et al., 2003) (Fig. 1). to the salinity and temperature, in which the foraminifera has The Beitstadfjord adjoins the Trondheimsfjord at Skarnsund been ultimately living (e. g. Urey, 1946; Epstein et al., 1953; 63◦500 N, 11◦040 E and extends until Steinkjer at 63◦000 N, Shackleton and Opdyke, 1973; and Bemis and Spero, 1998). 11◦280 E. The Trondheimsfjord is divided into two basins, In coastal environments, however, the relative impact of the the Seaward Basin and the Middle Fjord basin, which are to- freshwater δ18O related to the source increases with increas- pographically separated from the Norwegian Sea and from ing proximity to the shore (Ingram et al., 1996; Scheurle each other by bedrock thresholds (Figs. 1, 2a). Stjørnfjord and Hebbeln, 2003). The carbon isotope ratio in benthic and the Seaward Basin are separated from the Norwegian foraminifera is mainly linked to the influence of deep wa- Sea by a broad and shallow sill at the fjord entrance rising ter ventilation, to the origin (marine vs. terrigenous) and the to 195 m water depth (Fig. 2a). The Tautra Sill with a mini- amount of organic matter deposited at the sediment surface, mum water depth of 98 m separates the Seaward Basin from and to remineralization processes in the sediment (e.g. Car- the Middle Fjord (Fig. 2a). The innermost fjord, the Beitstad- alp 1989; Schmiedl et al., 2004; and Fontanier et al., 2008). fjord, is separated from the Trondheimsfjord by the Skarn- The stable isotope ratio incorporated in the calcite shell may sund Sill with a minimum water depth of 140 m (Fig. 2a). thus considerably deviate from the isotopic ratio of the bot- The deepest part in the fjord with a maximum water depth tom water due to fractionation effects, the microhabitat in of 620 m is located in the narrow passage between the fjord which the foraminifera lives and calcifies, and the geochem- entrance and Røberg in the Seaward Basin. In the follow- ical composition
Load more

Recommended publications
  • Wahlenbergia 1 Distribution
    Wahlenbergia 1 Distribution: University of Umeå, Department of Ecological Botany, S-901 87 UMEÂ, SWEDEN Åke Strid Wood-inhabiting Fungi of Alder Forests in North-Central Scandinavia. I. Aphyllophorales (Basidiomycetes). Taxonomy, Ecology and Distri­ bution. Akademisk avhandling som med tillstånd av rektorsämbetet vid Umeå universitet för avläggande av filosofie doktorsexamen framlägges till offentlig granskning vid Avdelningen för ekologisk botanik, Botanik, Fysiologi, Hufo, sem.-rum B, tisdagen den 27 maj 1975, kl. 10. Abstract Wood-inhabiting fungi were collected on different trees in 99 loca-' lities of alder woods, dominated by Alnus incana or occasionally A. glutinosa, in N-C Sweden and C Norway. Most of the localities are situated near the east coast of Sweden where the prevailing land elevation creates conditions suitable for colonization by alder. The remaining localities are mainly found in the inland parts of Sweden and Norway, along streams, in ravines etc. The investigated localities are briefly described as to their general vegetation, and a regional survey of the alder forests is given. The number of collections of Aphyllophorales amounts to approxi­ mately 5,000, comprising 286 species. The following new combinations are proposed: Hypoohnicium polonense (Bres.) Strid, H. pruinosum (Bres.) Strid, Phlebia lindtneri (Pil.) Parm. and Sistotrema hete- roncmum (John Erikss.) Strid. Seven species are collected as new to Scandinavia, viz., Botryobasidium aure urn3 Ceratobasidium stridiit Hyphoderma orphanellum, Hyphodontiella multiseptata, Hypoohnicium pruinosum> Phlebia lindtneri and Tubuliorinis effugiens, and approxi­ mately 85 additional species are reported for the first time from the investigation area. Six specimens of Cortioiaoeae have remained undetermined but are included in the species list.
    [Show full text]
  • “Proud to Be Norwegian”
    (Periodicals postage paid in Seattle, WA) TIME-DATED MATERIAL — DO NOT DELAY Travel In Your Neighborhood Norway’s most Contribute to beautiful stone Et skip er trygt i havnen, men det Amundsen’s Read more on page 9 er ikke det skip er bygget for. legacy – Ukjent Read more on page 13 Norwegian American Weekly Vol. 124 No. 4 February 1, 2013 Established May 17, 1889 • Formerly Western Viking and Nordisk Tidende $1.50 per copy News in brief Find more at blog.norway.com “Proud to be Norwegian” News Norway The Norwegian Government has decided to cancel all of commemorates Mayanmar’s debts to Norway, nearly NOK 3 billion, according the life of to Mayanmar’s own government. The so-called Paris Club of Norwegian creditor nations has agreed to reduce Mayanmar’s debts by master artist 50 per cent. Japan is cancelling Edvard Munch debts worth NOK 16.5 billion. Altogether NOK 33 billion of Mayanmar’s debts will be STAFF COMPILATION cancelled, according to an Norwegian American Weekly announcement by the country’s government. (Norway Post) On Jan. 23, HM King Harald and other prominent politicians Statistics and cultural leaders gathered at In 2012, the total river catch of Oslo City Hall to officially open salmon, sea trout and migratory the Munch 150 celebration. char amounted to 503 tons. This “Munch is one of our great is 57 tons, or 13 percent, more nation-builders. Along with author than in 2011. In addition, 91 tons Henrik Ibsen and composer Edvard of fish were caught and released. Grieg, Munch’s paintings lie at the The total catch consisted of core of our cultural foundation.
    [Show full text]
  • Ritual Landscapes and Borders Within Rock Art Research Stebergløkken, Berge, Lindgaard and Vangen Stuedal (Eds)
    Stebergløkken, Berge, Lindgaard and Vangen Stuedal (eds) and Vangen Lindgaard Berge, Stebergløkken, Art Research within Rock and Borders Ritual Landscapes Ritual Landscapes and Ritual landscapes and borders are recurring themes running through Professor Kalle Sognnes' Borders within long research career. This anthology contains 13 articles written by colleagues from his broad network in appreciation of his many contributions to the field of rock art research. The contributions discuss many different kinds of borders: those between landscapes, cultures, Rock Art Research traditions, settlements, power relations, symbolism, research traditions, theory and methods. We are grateful to the Department of Historical studies, NTNU; the Faculty of Humanities; NTNU, Papers in Honour of The Royal Norwegian Society of Sciences and Letters and The Norwegian Archaeological Society (Norsk arkeologisk selskap) for funding this volume that will add new knowledge to the field and Professor Kalle Sognnes will be of importance to researchers and students of rock art in Scandinavia and abroad. edited by Heidrun Stebergløkken, Ragnhild Berge, Eva Lindgaard and Helle Vangen Stuedal Archaeopress Archaeology www.archaeopress.com Steberglokken cover.indd 1 03/09/2015 17:30:19 Ritual Landscapes and Borders within Rock Art Research Papers in Honour of Professor Kalle Sognnes edited by Heidrun Stebergløkken, Ragnhild Berge, Eva Lindgaard and Helle Vangen Stuedal Archaeopress Archaeology Archaeopress Publishing Ltd Gordon House 276 Banbury Road Oxford OX2 7ED www.archaeopress.com ISBN 9781784911584 ISBN 978 1 78491 159 1 (e-Pdf) © Archaeopress and the individual authors 2015 Cover image: Crossing borders. Leirfall in Stjørdal, central Norway. Photo: Helle Vangen Stuedal All rights reserved. No part of this book may be reproduced, or transmitted, in any form or by any means, electronic, mechanical, photocopying or otherwise, without the prior written permission of the copyright owners.
    [Show full text]
  • Poststeder Nord-Trøndelag Listet Alfabetisk Med Henvisning Til Kommune
    POSTSTEDER NORD-TRØNDELAG LISTET ALFABETISK MED HENVISNING TIL KOMMUNE Aabogen i Foldereid ......................... Nærøy Einviken ..................................... Flatanger Aadalen i Forradalen ...................... Stjørdal Ekne .......................................... Levanger Aarfor ............................................ Nærøy Elda ........................................ Namdalseid Aasen ........................................ Levanger Elden ...................................... Namdalseid Aasenfjorden .............................. Levanger Elnan ......................................... Steinkjer Abelvær ......................................... Nærøy Elnes .............................................. Verdal Agle ................................................ Snåsa Elvalandet .................................... Namsos Alhusstrand .................................. Namsos Elvarli .......................................... Stjørdal Alstadhoug i Schognen ................. Levanger Elverlien ....................................... Stjørdal Alstadhoug ................................. Levanger Faksdal ......................................... Fosnes Appelvær........................................ Nærøy Feltpostkontor no. III ........................ Vikna Asp ............................................. Steinkjer Feltpostkontor no. III ................... Levanger Asphaugen .................................. Steinkjer Finnanger ..................................... Namsos Aunet i Leksvik ..............................
    [Show full text]
  • Statistikk 2012
    Årsstatistikk 2012 Utarbeid av Kjell Olav Storflor Korrigeringer rapporteres : [email protected] eller 952 52 277 Statistikk - 2012. Jenter 10 år 40 meter Idun Viem Ness Snåsa il 7,31 Snåsa 26.05 Jonna Dunfjeld Mølnvik Snåsa il 7,54 Snåsa 26.05 Lilly Marie Johansen Snåsa il 7,82 Snåsa 26.05 Sigrid Skaug Snåsa il 8,31 Snåsa 26.05 (manuell tidtaking) Sigrid Bonslet Røkke Flora il 8,2 Flora 16.05 Elisabet Husås Flora il 8,7 Flora 16.05 60 meter Malin Moen Lånke il 9,81 Stjørdal 10.06 Erle Musum Lyng Verdal fik 10,03 Steinkjer 16.06 Dagrun Ystad Derås Namdalseid il 10,24 Namdalseid 04.08 Jonna Dunfjeld Mølnvik Snåsa il 10,38 Steinkjer 12.08 Idun Viem Ness Snåsa il 10,39 Steinkjer 12.08 Sofie Aune Frol il 10,52 Levanger 27.08 Ine Tronstad Steinkjer fik 10,73 Steinkjer 15.05 Maria M. Johansen Frol il 10,74 Levanger 27.08 Guro Flatås Frol il 10,81 Levanger 04.06 Lilly Marie Johansen Snåsa il 10,86 Steinkjer 12.08 (manuell tidtaking) Ine Tronstad Steinkjer fik 10,0 Beitstad 04.09 Marte Aas Inderøy il 10,4 Inderøy 20.08 Innendørs Erle Musum Lyng Verdal fik 10,00 Steinkjer 08.12 Ine Tronstad Steinkjer fik 10,61 Steinkjer 19.01 200 meter Innendørs Erle Musum Lyng Verdal fik 34,28 Steinkjer 08.12 Ine Tronstad Steinkjer fik 37,14 Steinkjer 02.02 Hanna Marie Gangstad Steinkjer fik 39,29 Steinkjer 19.01 Maria Øgstad Verdal fik 41,27 Steinkjer 02.02 Ragne Kristin Brovold Steinkjer fik 41,42 Steinkjer 02.02 Lina Austli Berg Steinkjer fik 42,29 Steinkjer 19.01 600 meter Erle Musum Lyng Verdal fik 2.14,86 Steinkjer 16.06 Liv Merethe Prigge il Nybrott 2.22,1
    [Show full text]
  • Administrative and Statistical Areas English Version – SOSI Standard 4.0
    Administrative and statistical areas English version – SOSI standard 4.0 Administrative and statistical areas Norwegian Mapping Authority [email protected] Norwegian Mapping Authority June 2009 Page 1 of 191 Administrative and statistical areas English version – SOSI standard 4.0 1 Applications schema ......................................................................................................................7 1.1 Administrative units subclassification ....................................................................................7 1.1 Description ...................................................................................................................... 14 1.1.1 CityDistrict ................................................................................................................ 14 1.1.2 CityDistrictBoundary ................................................................................................ 14 1.1.3 SubArea ................................................................................................................... 14 1.1.4 BasicDistrictUnit ....................................................................................................... 15 1.1.5 SchoolDistrict ........................................................................................................... 16 1.1.6 <<DataType>> SchoolDistrictId ............................................................................... 17 1.1.7 SchoolDistrictBoundary ...........................................................................................
    [Show full text]
  • Namsos Inderøy Innherred Stjørdal Meråker Steinkjer
    NAMSOS MERÅKER INDERØY STEINKJER INNHERRED GRONG STJØRDAL BEITSTAD 2020 Foto: Siv Fiskvik Foto: Siv Våre turregler: Foto: Mari Louise Fossland - Alle barn kan gå på tur. - Vi vil gjerne ha med en venn. - Vi vil være med å planlegge turen. - Vi har lyst til å gå foran og bestemme farten. - Vi vil ha tid til å leke og oppleve spennende ting underveis. - Vi vil ha tid til å snakke om det vi ser og opplever på turen. - Vi vil ha no` godt på toppen. Dato Aktivitet / turmål 2. februar - Vi vil kose oss om kvelden når Setertun vi er på overnattingstur. 24.mai Topptur - Vi vil ikke være frosne, våte Valan eller redde. 22.-23. Overnattingstur august Kalvøya 6. september Tømte naturlekeplass Namdalseid 18. oktober Reflekstur til uglas plass 29. november Juletur Følg med på nettsiden vår og Bråten Facebook-sidene til de ulike turlagene. Foto: Eirik Vyen Foto: Eirik BARNAS TURREGLER BARNAS Barnas Turlag Inderøy Foto: Anne Grethe Holmvik Foto: Anne Grethe Dato Aktivitet / turmål 2. februar Skallstuggu 2. eller 4. mars Skileik og kveldsmattur Torsbustaden 11. mars Aking og kveldsmattur Leirådalen 6. april Påskeeggjakt Røstadfjæra 6.-7.juni Overnattingstur Telt, lavvo, hengekøye, under åpen himmel. Tromsdalen 14. juni Sommeravslutning Sundsand Dato Aktivitet / turmål 2. februar 6. september Skihytta på Røra Skallstuggu 23. april Kveldsmattur til Røsethavna 14. oktober Refleksløype og kveldsmattur Torsbustaden 14. juni Aktivitetsdag på Sundsand November Aktivitetskveld Trønderhallen 6. september «Trillegruppa prøver å få til tur Liatjønna i Mosvik hver uke. Alle med små barn og fri på dagtid er velkommen med 6. desember Nissegrøtfest 30.
    [Show full text]
  • 7317 Buss Rutetabell & Linjerutekart
    7317 buss rutetabell & linjekart 7317 Egge Ungdomskole Vis I Nettsidemodus 7317 buss Linjen Egge Ungdomskole har 2 ruter. For vanlige ukedager, er operasjonstidene deres 1 Egge Ungdomskole 07:35 2 Melland 14:15 Bruk Moovitappen for å ƒnne nærmeste 7317 buss stasjon i nærheten av deg og ƒnn ut når neste 7317 buss ankommer. Retning: Egge Ungdomskole 7317 buss Rutetabell 26 stopp Egge Ungdomskole Rutetidtabell VIS LINJERUTETABELL mandag 07:35 tirsdag 07:35 Vellamelen Namsosvegen 983, Norway onsdag 07:35 Beitstad torsdag 07:35 Brattbergsvegen 2, Norway fredag 07:35 Østvik lørdag Opererer Ikke Kvarving søndag Opererer Ikke Namsosvegen 701, Norway Korsenget Klætt 7317 buss Info Namsosvegen 546, Norway Retning: Egge Ungdomskole Stopp: 26 Jådåren Reisevarighet: 49 min Namsosvegen 475, Norway Linjeoppsummering: Vellamelen, Beitstad, Østvik, Kvarving, Korsenget, Klætt, Jådåren, Røsegg, Røsegg Gulling, Dyrstad, Asp, Rungstad, Sneve, Egge Ungdomsskole, Vammen, Nordsida, Nordsileiret, Gulling Steinkjer Montessoriskole, Nordsileiret, Bogen, Steinvika Terrasse, Steinvika, Søndre Egge, Dyrstad Lundsengvegen, Egge Barneskole, Egge Ungdomsskole Asp Kvamsvegen 781, Norway Rungstad Sneve Egge Ungdomsskole Vammen Nordsida Kongens gate, Steinkjer Nordsileiret Jæktskippergata 1, Steinkjer Steinkjer Montessoriskole Nordsileiret Jæktskippergata 1, Steinkjer Bogen Bogavegen 103, Steinkjer Steinvika Terrasse Bogavegen 126, Steinkjer Steinvika Bogavegen 145, Steinkjer Søndre Egge Balders Veg 3, Steinkjer Lundsengvegen Lundsengvegen 105, Steinkjer Egge Barneskole
    [Show full text]
  • 2 Jan 2012 Familieslektsbok Velde-Slekta - Etterkommere Etter Paul Jakobsen Rostad Paul Jakobsen Rostad , F
    2 jan 2012 Familieslektsbok Velde-slekta - Etterkommere etter Paul Jakobsen Rostad Paul Jakobsen Rostad , f. 1704, d. 1780. Han giftet seg med Maria Iversdatter , f. 1712 (ca.). I. Jakob Paulsen Rostad , f. 1737, d. 1802. Gift 1767, med Anne Hansdatter Glasø , f. 1739 (datter av Hans Estensen Glasø og Maren Jonsdatter). A. Marit J. Tessem , f. 1780, d. 26 aug 1845. Gift 20 okt 1804, med Staal P. Kjeldseth , f. 1780 (sønn av Peder S. Jønnum og Kjersti O. Kjeldseth), d. 10 okt 1825. 1. Jakob Stålsen Velde , f. 1805 på Skevik, Beitstad, d. 1877 på Nedre Velde, Beitstad. Gift 25 jun 1832 i Solberg Kirke, med Johanna Sivertsdatter Malmo , f. 1810 på Malmo, Malm (datter av Sivert Mortensen Malmo og Guru Hågensdatter Skaar), d. 1882 på Nedre Velde, Beitstad. a. Stasius J. Velde , f. 16 jan 1833 på Nedre Velde, Beitstad, d. 6 des 1890 på Buvarp, Namdalseid. Gift 25 nov 1860 i Halmøy, Flatanger, med Eline J. Aagesdtr. Aagård , f. 1843 i Flatanger, d. 1921 i Levanger. (A) Jakob Karl Arnold Welde , f. 1861, d. 1900 i Lilleelvdal. (B) Johanna Alberta Welde , f. 1864, d. i Fannrem. (C) Mette Marianne Welde Rinnan , f. 1866, d. 1915 i Levanger. Hun giftet seg med E. Rinnan , d. i Levanger. (1) Einar Rinnan . (2) Trygve Rinnan , f. 1902 i Levanger. (3) Agnes Rinnan Solheim , f. 25 mai 1905 i Levanger. Hun giftet seg med Torvald Solheim , f. 1900. (a) Ruth Solheim , f. 1925 i Sørli. (b) Berge Solheim , f. 1927 i Sørli. (c) Eldbjørg Solheim , f. 1928 i Sørli. (D) Sturla Sigvart Welde , f.
    [Show full text]
  • Fylkesfinale Ta-Sprinten 2019
    FYLKESFINALETA-SPRINTEN2019 - Gratulerer tilallesom er kvalifisert! Sted: Guldbergaunet Dato: lørdag 17.august Tid: kl.14.00 Tekniskarrangør: Steinkjerfriidrettsklubb Nå er vi klare forFylkesfinale iTAsprinten og ønsker alleaktive, trenere, ledere og andre friidrettsnyskjerrige hjerteligvelkommentil GuldbergaunetIdrettspark iSteinkjerlørdag17. august kl.14.00.Her blir detspenning, myegøy og massevisavknivskarpedueller iløp,hoppogkast! Vi harogsåiår satt opp heat og øvelsermed aktive etteroppnådde resultat og offisiell statistikk.Dvs.atutøvere somvar forhindretogikkehaddeanledning tilådelta på sonestevneniårnåerkvalifisertvia andregodkjente stevner. Godkjentestevner er stevnersom finnesiNFIFs datosorterte Terminliste, www.friidrett.no/aktivitet/terminliste/webdel---terminliste/ Herkommer ny komplett oversiktoverhvemsom er kvalifisertihvilkeøvelserogklasser.Omdet blir endringer pga. forfallvil vi prøve åfåmed detteiannonsen fredag 16.august. Vi håper klubbene kanvære behjelpelig med følgende: •Forsikreseg om at utøverne vetatdehar kvalifisert seg. Normaltsørgervel foreldrefor transport, meniden grad klubbenkan være behjelpelig, er detfint. •For de someventueltkan kommeinn somreserver, og forarrangøren,erdet viktig at eventuelle forfallblir varsletsåsnart sommuligogseinestonsdag15. august. •Viminneromatpiggskoertillattifinalen. PREMIERING: De trebeste ihver klasse/øvelsepremieres medegenmedalje igull, sølv og bronse. HERERDESOMHAR KVALIFISERTSEG TILÅRETS FINALER: GUTTER 11 ÅR Johnsen,NamsenFIF.Imre ValleViken,Lånke IL.Iver Beitstad IL.Ingeborg
    [Show full text]
  • Visitinnherred.Com › Files › 2014 › 02 › A-Komplett-NOR-2016.Pdf Visit
    GUIDE 2016 innherred levanger, verdal, inderøy, steinkjer, snåsa Innherred Trondheim Stockholm Oslo WWW.VISITINNHERRED.COM OVERNATTING - SERVERDIGHETER - SYKKEL - VANDRING AVSTANDSTABELL ØSTERSUNDÅRE NAMSKOGANNAMSOSVERRAN/MALAMGRONGSNÅSASTEINKJERINDERØYVERDALLEVANGERFROSTASTJØRDALTRONDHEIM Km ØSTERSUND 101 396 321 273 323 299 243 229 211 223 235 240 275 ÅRE 101 293 218 170 220 196 140 128 110 122 163 139 174 NAMSKOGAN 396 293 121 183 73 106 153 175 184 194 235 242 274 NAMSOS 321 218 121 80 48 80 78 102 112 118 159 164 202 VERRAN/MALM 273 170 183 80 98 80 30 52 63 73 112 121 150 GRONG 323 220 73 48 98 33 80 102 112 118 159 164 202 SNÅSA 299 196 106 80 80 33 56 78 88 97 138 146 176 STEINKJER 243 140 153 78 30 80 56 22 30 41 82 89 124 INDERØY 229 128 175 102 52 102 78 22 18 28 69 74 106 VERDAL 211 110 184 112 63 112 88 30 18 12 53 59 94 LEVANGER 223 122 194 118 73 118 97 41 28 12 41 47 79 FROSTA 235 163 235 159 112 159 138 82 69 53 41 42 64 STJØRDAL 240 139 242 164 121 164 146 89 74 59 47 42 35 TRONDHEIM 275 174 274 202 150 202 176 124 106 94 79 64 35 @visitinnherred #innherred INNHOLD 4 Velkommen til Innherred 48 Fuglekassen Overnatting i 6 Topp 20 på Innherred Inderøy 10 Mat og matkultur på 49 Spise, sove, gjøre, Inderøy Innherred 52 Steinkjer kommune 12 Museer på Innherred 54 Norges Midtpunkt 14 Action på Innherred 16 Fiske 57 Spise, sove, gjøre i 18 Turmuligheter Steinkjer 20 Sykkelturer 62 Snåsa Kommune 22 Badestrender 64 Spise, sove, gjøre i Snåsa 23 Kano, kajakk - og båtutleie 68 Transport og Turproduksjon 24 Levanger kommune 70 Nyttig
    [Show full text]
  • Local Ideas About Rights of Common in the Context of a Historical Transformation from Commons to Private Property
    Paper for presentation at the 14th global conference of the International Association for the Study of Commons, Mt Fuji, June 3- June 7, 2013 _________________________________________________________________________________________ Local ideas about rights of common in the context of a historical transformation from commons to private property Erling Berge Department of Landscape Architecture and Spatial Planning/ Centre for Land Tenure Studies, Norwegian University of Life Sciences, e-mail: [email protected] and Anne Sigrid Haugset Trøndelag R&D Institute, Abstract More than 200 years after the King sold one of the “King’s commons” (Follafoss, located in the current Verran municipality) to urban timber merchants, local people in some ways still behave as if the area is a kind of commons. The paper will outline the history of the transformation of the area from an 18th century King’s commons to a 21th century battleground for ideas about ancient access and use rights of community members facing rights of a commercial forest owner and the local consequences of national legislation. This battleground will be illuminated by the answers that current users provide to questions about what they believe their rights of access and use are. We shall in particular look for differences between what people believe and what the law seems to say about rights and duties in the Follafoss area. Key words King’s commons; private forest; rights of common; customary rights; national legislation; loss of customary rights; © Copyright by the authors. The authors agree to allow the Digital Library of the Commons to add this paper to its archives for IASC conferences.
    [Show full text]