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A 1.2Ma Record of Glaciation and Fluvial Discharge from the West European Atlantic Margin S
A 1.2Ma record of glaciation and fluvial discharge from the West European Atlantic margin S. Toucanne, S. Zaragosi, J.F. Bourillet, P.L. Gibbard, F. Eynaud, J. Giraudeau, J.L. Turon, M. Cremer, E. Cortijo, P. Martinez, et al. To cite this version: S. Toucanne, S. Zaragosi, J.F. Bourillet, P.L. Gibbard, F. Eynaud, et al.. A 1.2Ma record of glaciation and fluvial discharge from the West European Atlantic margin. Quaternary Science Reviews, Elsevier, 2009, 28 (25-26), pp.2974-2981. 10.1016/j.quascirev.2009.08.003. hal-03006683 HAL Id: hal-03006683 https://hal.archives-ouvertes.fr/hal-03006683 Submitted on 28 Jun 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. A 1.2 Ma record of glaciation and fluvial discharge from the West European Atlantic margin S. Toucannea, b, *, S. Zaragosia, J.F. Bourilletb, P.L. Gibbardc, F. Eynauda, J. Giraudeaua, J.L. Turona, M. Cremera, E. Cortijod, P. Martineza and L. Rossignola a Université de Bordeaux, UMR 5805, Avenue des Facultés, F-33405 Talence, France b IFREMER, Laboratoire Environnements Sédimentaires, BP70, 29280 Plouzané, France c Cambridge Quaternary, Department of Geography, University of Cambridge, Cambridge, CB2 3EN, UK d Laboratoire des Sciences du Climat et de l'Environnement LSCE/IPSL (UMR CEA-CNRS-UVSQ 1572), CE Saclay, L'Orme des Merisiers, Bât. -
Answers to the Comments by Reviewer RC2
Answers to the comments by reviewer RC2: General comments: 1) My main issue with this manuscript has to do with its readability. There are numerous grammatical errors throughout, some of which are pointed out below. A native English speaker should edit the paper before resubmission. This is now done. The authors are grateful for the thorough review also concerning the language. 2) The authors tend to make some broad sweeping conclusions based on trends that are only significant across a small fraction of the total study region. I would like to see more discussion of the full picture (like Figure 9). Pg 10 L2 and Pg11 L5 are two instances where the discussion is too narrow in focus. The authors have now extended the mentioned discussions (sections 3.1.1, 3.1.3 and 3.3.) as requested. The systematic signal of change is not as dramatic in Finland as in some areas, because of the large variation of winter weather. Especially the sea ice extent of Baltic Sea affects largely the Finnish winter weather. If the Gulf of Finland and Gulf of Bothnia freeze completely the Finnish climate is almost continental in winter even on the coast. We added a comment about the hemispherical study published recently, where we studied the effect of weather parameters on the observed changes in larger areas. Section 3.1.1 main addition: Especially variable melt onset timing is in the coastal regions (Southwestern Finland and Southern Ostrobothnia) and in the Lake district. For those regions the standard deviation values of the melt onset day are 14.3, 14.7 and 14.6, respectively. -
Icos23 665.Pdf (420.2Kb)
Antti Leino, Finland 665 Multilingual Names on the Finnish Basic Map Antti Leino Finland Abstract The Finnish Basic Map and the computerised Place Name Register maintained by the National Land Survey for map-making purposes have place names in five different languages: the official Finnish and Swedish, and three semi-official Sámi languages. As one would expect, distributions of the various languages overlap, and roughly one percent of the named places have names in more than one language. All five naming systems are similar enough that semantically transparent toponyms can be translated from one language to another. The three Sámi languages are also similar enough that virtually all common multilingual names are also common in each of their respective languages. This is also true for Finnish and Swedish, but the names common to Finnish and the Sámi languages often involve elements that have a more limited geographic distribution in Finnish. All this gives some insight into the underlying cultural interplay, and also into the role of semantic transparency in name use. *** Introduction The Republic of Finland has two official and five semi-official languages, as shown in Table 1. Of these the Sámi languages, Finnish, and Swedish have the longest history of being spoken in the region, reaching further back than historical records. Pitkänen (2001) outlines how originally Finnish toponyms along the southern coast have been loaned to a new, Swedish-speaking population in the early Middle Ages, and also dates (1990) some of them to as early as the end of the last millennium B.C. Loan words in the Finnic languages also make it clear that contacts with Germanic languages have been constant since prehistoric times, and it has been argued (Itkonen 1983) that contacts with Indo-Europeans, both Baltic and Germanic, were the original cause for the differentiation of Finnic and Sámi languages. -
Answers to the Comments by Reviewer RC1: This Is an Interesting
Answers to the comments by reviewer RC1: This is an interesting and thorough study, but some of the methods are hard to follow. In particular, I recommend some effort on simplifying and clarifying the descriptions of sigmoid fits in sections 2.2.1 and 2.2.2; figures of example fits might help. The authors are grateful for the encouraging comment. The sigmoid fitting is described now in more detail and related images are included. The method sounds complicated, because one has to take into account also rare, but possible complications (such as marked snowfall after melt onset). However, the main complication really to take into account is the greening up of vegetation. This is demonstrated in the added Figure 2, where we also now include examples of temporary pits before melt onset and temporary peaks after snow melt. Minor comments: page 1, line 26. Forest cover having a significant influence on albedo does not follow from it being an important component of the carbon budget. This sentence is now edited according to the comment. page 2, line 11. “by in” – delete one “in” is deleted as requested. page 2, line 24 “since 200” is sufficient “Year” is removed as suggested. page 3, line 3 I think that standalone forcing of land models with climate model outputs is being dis- cussed here, but it is not clear. The text is edited (page 3, line 6). page 4, line 6 Delete “only” “Only” is deleted as requested. page 5, line 21 “using in-situ FSC observations” Is FSC %-units simply %? Yes, the FSC units is %. -
Reconstructing the Confluence Zone Between Laurentide and Cordilleran Ice Sheets Along the Rocky Mountain Foothills, Southwest Alberta
This is a repository copy of Reconstructing the confluence zone between Laurentide and Cordilleran ice sheets along the Rocky Mountain Foothills, southwest Alberta. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/105138/ Version: Accepted Version Article: Utting, D., Atkinson, N., Pawley, S. et al. (1 more author) (2016) Reconstructing the confluence zone between Laurentide and Cordilleran ice sheets along the Rocky Mountain Foothills, southwest Alberta. Journal of Quaternary Science, 31 (7). pp. 769-787. ISSN 0267-8179 https://doi.org/10.1002/jqs.2903 Reuse Unless indicated otherwise, fulltext items are protected by copyright with all rights reserved. The copyright exception in section 29 of the Copyright, Designs and Patents Act 1988 allows the making of a single copy solely for the purpose of non-commercial research or private study within the limits of fair dealing. The publisher or other rights-holder may allow further reproduction and re-use of this version - refer to the White Rose Research Online record for this item. Where records identify the publisher as the copyright holder, users can verify any specific terms of use on the publisher’s website. Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ Reconstructing the confluence zone between Laurentide and Cordilleran ice sheets along the Rocky Mountain Foothills, south-west Alberta Daniel J. Utting1, Nigel Atkinson1, Steven Pawley1, Stephen J. -
'Fleuve Manche' Discharges Over the Last 350
Quaternary Science Reviews Archimer June 2009, Volume 28, Issues 13-14, Pages 1238- http://archimer.ifremer.fr 1256 http://dx.doi.org/10.1016/j.quascirev.2009.01.006 © 2009 Elsevier Ltd All rights reserved. ailable on the publisher Web site Timing of massive ‘Fleuve Manche’ discharges over the last 350 kyr: insights into the European ice-sheet oscillations and the European drainage network from MIS 10 to 2 S. Toucannea, *, S. Zaragosia, J.F. Bourilletb, M. Cremera, F. Eynauda, B. Van Vliet-Lanoëc, A. Penauda, C. Fontanierd, J.L. Turona, E. Cortijoe and P.L. Gibbardf a Université de Bordeaux, UMR 5805, Avenue des Facultés, F-33405 Talence, France b IFREMER, Laboratoire Environnements Sédimentaires, BP70, 29280 Plouzané, France c blisher-authenticated version is av Institut Européen Universitaire de la Mer, Domaines Océaniques (UMR CNRS 6538), Place Nicolas Copernic, 29280 Plouzané, France d Université d'Angers, Laboratoire des Bio-indicateurs Actuels et fossiles (UPRES EA 2644), Boulevard Lavoisier, 49045 Angers Cedex 01, France e Laboratoire des Sciences du Climat et de l'Environnement LSCE/IPSL (UMR CEA-CNRS-UVSQ 1572), CE Saclay, L'Orme des Merisiers, Bât 701, 91191 Gif-sur-Yvette cedex, France f Cambridge Quaternary, Department of Geography, University of Cambridge, Cambridge CB2 3EN, UK *: Corresponding author : S. Toucanne, Tel.: +33 540 00 8438; fax: +33 556 84 0848, email address : [email protected] Abstract: Continuous high-resolution mass accumulation rates (MAR) and X-ray fluorescence (XRF) measurements from marine sediment records in the Bay of Biscay (NE Atlantic) have allowed the determination of the timing and the amplitude of the ‘Fleuve Manche’ (Channel River) discharges during glacial stages MIS 10, MIS 8, MIS 6 and MIS 4–2. -
The First Estimation of Fleuve Manche Palaeoriver Discharge During The
Earth and Planetary Science Letters Archimer February 2010, Volume 290, Issues 3-4, Pages 459- http://archimer.ifremer.fr 473 http://dx.doi.org/10.1016/j.epsl.2009.12.050 © 2010 Elsevier B.V. All rights reserved. ailable on the publisher Web site The first estimation of Fleuve Manche palaeoriver discharge during the last deglaciation: Evidence for Fennoscandian ice sheet meltwater flow in the English Channel ca 20–18 ka ago Samuel Toucannea, b, *, Sébastien Zaragosia, Jean-François Bourilletb, Vincent Marieua, Michel Cremera, Masa Kageyamac, Brigitte Van Vliet-Lanoëd, Frédérique Eynauda, Jean-Louis Turona and Philip L. Gibbarde a Université de Bordeaux, UMR 5805, Avenue des Facultés, F-33405 Talence, France b blisher-authenticated version is av IFREMER, Laboratoire Environnements Sédimentaires, BP70, 29280 Plouzané, France c Laboratoire des Sciences du Climat et de l'Environnement LSCE/IPSL (UMR CEA-CNRS-UVSQ 1572), CE Saclay, L'Orme des Merisiers, Bât. 701, 91191 Gif-sur-Yvette cedex, France d Institut Européen Universitaire de la Mer, Domaines Océaniques (UMR CNRS 6538), Place Nicolas Copernic, 29280 Plouzané, France e Cambridge Quaternary, Department of Geography, University of Cambridge, Cambridge, CB2 3EN, UK *: Corresponding author : Samuel Toucanne, Tel.: +33 298 22 4249; fax: +33 298 22 4570, email address : [email protected] Abstract: The Fleuve Manche (English Channel) palaeoriver represents the largest river system that drained the European continent during Pleistocene lowstands, particularly during the Elsterian (Marine Isotope Stage 12) and Saalian Drenthe (MIS 6) glaciations when extensive ice advances into the North Sea area forced the central European rivers to flow southwards to the Bay of Biscay (NE Atlantic). -
The Morphological Units Between the End Moraines of the Pomeranian Phase and the Eberswalde Ice-Marginal Valley (Urstromtal), Ge
Quaternary Science Journal GEOZON SCIENCE MEDIA Volume 66 / Number 1 / 2017 / 44-56 / DOI 10.3285/eg.66.1.04 ISSN 0424-7116 E&G www.quaternary-science.net The morphological units between the end moraines of the Pomeranian phase and the Eberswalde ice-marginal valley (Urstromtal), Germany – a critical examination by means of a high-resolution DEM Maximilian Krambach, Margot Böse How to cite: Krambach, M., Böse, M. (2017): The morphological units between the end moraines of the Pomeranian phase and the Eberswal- de ice-marginal valley (Urstromtal), Germany – a critical examination by means of a high-resolution DEM. – E&G Quaternary Science Journal, 66 (1): 44–56. DOI: 10.3285/eg.66.1.04 Abstract: The area between the Pomeranian end moraine and the town of Eberswalde, located in the Torun-Eberswalde ice marginal val- ley (IMV), has long been considered to represent a sequence of proglacial landforms in good agreement with the model of the glacial series of Penck & Brückner (1901–1909). The most prominent geomorphological feature in the area is the Pomeranian end moraine which was formed at about 20 ka. However, the meltwater deposits in the research area were not only formed by melt- waters from the Pomeranian ice margin but also by those draining the Parstein and the Angermünde subphases of the retreating Scandinavian Ice Sheet (SIS). The main meltwater discharge was assumed to have followed a major valley structure, which today forms a gap in the end moraine ridge. The analysis of the landforms, their altitudes as well as the surface features, by means of a high-resolution digital elevation model (DEM) based on light detection and ranging (LiDAR) data now allow a new interpreta- tion. -
Finnish Flies of the Family Therevidae
© Entomologica Fennica. 3 March 2006 Finnish flies of the family Therevidae Antti Haarto & Kaj Winqvist Haarto, A. & Winqvist, K. 2006: Finnish flies of the family Therevidae. — Ento- mol. Fennica 17: 46–55. An illustrated key for the 17 Finnish species of Therevidae is presented that in- cludes six species recorded from neighbouring areas. Distributions of the Finnish species are discussed and presented in maps; evaluations concerning the threatenedness status of Finnish species are included. Antti Haarto, Zoological Museum, Section of Biodiversity and Environmental Science, University of Turku, FI-20014 Turku, Finland; E-mail: antti.haarto @turkuamk.fi Kaj Winqvist, Zoological Museum, University of Turku, FI-20014 Turku, Fin- land; E-mail: [email protected] Received 31 January 2005, accepted 13 July 2005 1. Introduction book on lower Brachycera (Stubbs & Drake 2001) lacks many Finnish species. The most ac- Flies of the family Therevidae belong to the sub- curate key for determining Finnish Therevidae order Brachycera and are relatively large Diptera. was presented by Lyneborg and Spitzer (1974); Unlike Asilidae, a morphologically and biologi- this key covers the Czech Republic fauna. cally close family, adults of Therevidae are not The purpose of this article is to provide an up- predatory and lack the deep groove between the dated key for the Finnish Therevidae and some eyes characteristic of Asilidae. species found in the neighbouring countries. The In Finland, there has been very little informa- distribution and habitat associations for each spe- tion published on Therevidae. Frey (1911) listed cies are briefly discussed based on the few avail- some of the oldest records for the lower able distributional and ecological data. -
The Last British Ice Sheet: a Review of the Evidence Utilised in the Compilation of the Glacial Map of Britain
This is a repository copy of The last British Ice Sheet: A review of the evidence utilised in the compilation of the Glacial Map of Britain . White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/915/ Article: Evans, D.J.A., Clark, C.D. and Mitchell, W.A. (2005) The last British Ice Sheet: A review of the evidence utilised in the compilation of the Glacial Map of Britain. Earth-Science Reviews, 70 (3-4). pp. 253-312. ISSN 0012-8252 https://doi.org/10.1016/j.earscirev.2005.01.001 Reuse Unless indicated otherwise, fulltext items are protected by copyright with all rights reserved. The copyright exception in section 29 of the Copyright, Designs and Patents Act 1988 allows the making of a single copy solely for the purpose of non-commercial research or private study within the limits of fair dealing. The publisher or other rights-holder may allow further reproduction and re-use of this version - refer to the White Rose Research Online record for this item. Where records identify the publisher as the copyright holder, users can verify any specific terms of use on the publisher’s website. Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ White Rose Consortium ePrints Repository http://eprints.whiterose.ac.uk/ This is an author produced version of a paper published in Earth-Science Reviews. -
Use of Different Fractions and Heavy
Use of different fractions and heavy minerals of till for ore prospecting in ribbed moraine areas in southern Finnish Lapland Glacial flow direction N Pertti Sarala* and Vesa Peuraniemi** * Geological Survey of Finland FI-96101 Rovaniemi [email protected] ** University of Oulu FI-90014 Oulun yliopisto IGES 2005 [email protected] Finland 19.9.2005 Pertti Sarala Outline Location of southern Finnish Lapland Geological background Ribbed moraines – what and where they are? Case studies and prospecting examples Till geochemistry Heavy minerals Boulders General prospecting strategy in ribbed moraine areas Conclusions IGES 2005 19.9.2005 Pertti Sarala Location of southern Finnish Lapland Finland Arctic circle m u Perth m axi l M acia Last Gl Southern Finnish Lapland is located in Northern Hemisphere near the Arctic Circle Glacial centre of the Last Glacial Maximum was situated in the area IGES 2005 19.9.2005 Pertti Sarala Bedrock and mines Peräpohja Schist Belt IGES 2005 19.9.2005 Pertti Sarala Relief ja landforms Hummocky Ribbed moraines ribbed and drumlins moraines Drumlins in Kuusamo NW-SE oriented drumlins and mostly till-covered esker chains drumlin field IGES 2005 19.9.2005 Pertti Sarala Glacial morphology Ribbed Kuusamo ice lobe moraines Tervola Younger drumlins Older drumlins Ranua interlobate area Glacial flow direction younger o Oulu ice lobe l d e r IGES 2005 19.9.2005 Pertti Sarala Ridges perpendicular to the latest glacial flow direction (200 m – 1.5 km in length, 50-200 Ribbed moraines m in width and 5-20 m -
Valtakunnallisesti Arvokkaat Moreenimuodostumat
SUOMEN YMPÄRISTÖ 14 | 2007 LUONNON- Valtakunnallisesti arvokkaat VARAT moreenimuodostumat Kalevi Mäkinen, Jukka-Pekka Palmu, Jari Teeriaho, Hannu Rönty, Tom Rauhaniemi & Jaana Jarva YMPÄRISTÖMINISTERIÖ SUOMEN YMPÄRISTÖ 14 | 2007 Valtakunnallisesti arvokkaat moreenimuodostumat Kalevi Mäkinen, Jukka-Pekka Palmu, Jari Teeriaho, Hannu Rönty, Tom Rauhaniemi & Jaana Jarva Helsinki 2007 YMPÄRISTÖMINISTERIÖ SUOMEN YMPÄRISTÖ 14 | 2007 Ympäristöministeriö Alueidenkäytön osasto Taitto: Ainoliisa Miettinen Kansikuva: ���������rumliine�������������������������������������a Kuusamon Iivaaran kaakkoispuolella �������Kuva: R Aario����� Poh�akartat: © Maanmittauslaitos lupa nro 197/MYY/05 Julkaisu on saatavana myös internetistä: wwwymparistofi/�ulkaisut Edita Prima Oy, Helsinki 2007 ISBN 978-952-11-2661-1 (nid) ISBN 978-952-11-2662-8 (P�F) ISSN 1238-7312 (pain) ISSN 1796-1637 (verkkoj.) ESIPUHE Moreenimuodostumat ovat Suomessa monipuolisin geomorfologisten maaperämuo- dostumien ryhmä, johon kuuluu syntytavaltaan, rakenteeltaan ja muodoiltaan hyvin erilaisia muodostumia. Moreenimuodostumiin ei toistaiseksi ole kiinnitetty erityistä suojelullista tai taloudellista huomiota, ilmeisesti muodostumien laajan levinneisyy- den ja moreeniaineksen heikohkon hyödynnettävyyden vuoksi. Moreenimuodos- tumista löytyy kuitenkin sellaista luonnon geologista, biologista ja maisemallista monimuotoisuutta, jolla suojeluarvojen kannalta on huomattavaa merkitystä. Mo- reenimuodostumiin liittyy samantyyppisiä maisemallisia ja elollisen luonnon arvoja kuin kallioihin ja harjuihin;