{"version":"1.0","provider_name":"Centre for Baltic and Scandinavian Archaeology (ZBSA)","provider_url":"https:\/\/zbsa.eu\/en","author_name":"Matthias Bolte","author_url":"https:\/\/zbsa.eu\/en\/author\/matthias-bolte\/","title":"Early Boreal - Zentrum f\u00fcr Baltische und Skandinavische Arch\u00e4ologie (ZBSA) \u2014 Zentrum f\u00fcr Baltische und Skandinavische Arch\u00e4ologie","type":"rich","width":600,"height":338,"html":"<blockquote class=\"wp-embedded-content\" data-secret=\"RDKMVkYJia\"><a href=\"https:\/\/zbsa.eu\/en\/early-boreal\/\">Early Boreal<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/zbsa.eu\/en\/early-boreal\/embed\/#?secret=RDKMVkYJia\" width=\"600\" height=\"338\" title=\"&#8220;Early Boreal&#8221; &#8212; Zentrum f\u00fcr Baltische und Skandinavische Arch\u00e4ologie (ZBSA) \u2014 Zentrum f\u00fcr Baltische und Skandinavische Arch\u00e4ologie\" data-secret=\"RDKMVkYJia\" frameborder=\"0\" marginwidth=\"0\" marginheight=\"0\" scrolling=\"no\" class=\"wp-embedded-content\"><\/iframe><script type=\"text\/javascript\">\n\/* <![CDATA[ *\/\n\/*! This file is auto-generated *\/\n!function(d,l){\"use strict\";l.querySelector&&d.addEventListener&&\"undefined\"!=typeof URL&&(d.wp=d.wp||{},d.wp.receiveEmbedMessage||(d.wp.receiveEmbedMessage=function(e){var t=e.data;if((t||t.secret||t.message||t.value)&&!\/[^a-zA-Z0-9]\/.test(t.secret)){for(var s,r,n,a=l.querySelectorAll('iframe[data-secret=\"'+t.secret+'\"]'),o=l.querySelectorAll('blockquote[data-secret=\"'+t.secret+'\"]'),c=new RegExp(\"^https?:$\",\"i\"),i=0;i<o.length;i++)o[i].style.display=\"none\";for(i=0;i<a.length;i++)s=a[i],e.source===s.contentWindow&&(s.removeAttribute(\"style\"),\"height\"===t.message?(1e3<(r=parseInt(t.value,10))?r=1e3:~~r<200&&(r=200),s.height=r):\"link\"===t.message&&(r=new URL(s.getAttribute(\"src\")),n=new URL(t.value),c.test(n.protocol))&&n.host===r.host&&l.activeElement===s&&(d.top.location.href=t.value))}},d.addEventListener(\"message\",d.wp.receiveEmbedMessage,!1),l.addEventListener(\"DOMContentLoaded\",function(){for(var e,t,s=l.querySelectorAll(\"iframe.wp-embedded-content\"),r=0;r<s.length;r++)(t=(e=s[r]).getAttribute(\"data-secret\"))||(t=Math.random().toString(36).substring(2,12),e.src+=\"#?secret=\"+t,e.setAttribute(\"data-secret\",t)),e.contentWindow.postMessage({message:\"ready\",secret:t},\"*\")},!1)))}(window,document);\n\/\/# sourceURL=https:\/\/zbsa.eu\/wp-includes\/js\/wp-embed.min.js\n\/* ]]> *\/\n<\/script>","description":"Version 1.0.1 Files Early Boreal version 1.0.1 Citation Please cite this map as &#8222;compiled by ZBSA after Bj\u00f6rck 1995; Brooks et al. 2011; Cohen et al. 2017; Edwards\/Brooks 2008; Harff et al. 2017; Lericolais 2017; Moscon et al. 2015;\u00a0P\u00e5sse\/Andersson 2005;\u00a0Seguinot et al. 2018;\u00a0Stroeven et al. 2016;\u00a0Subetto et al. 2017; Weaver et al. 2003&#8220; For full references see below.\u00a0 Timeslice The map is approximately representing the timeslice: chronological frame timeslice Greenlandic isotope chronology &#8211; years calibrated BC 8700\u20138000 year calibrated BP 10700\u201310000 14C years BP 9400\u20138800 \u00a0 Release notes This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this license, visit https:\/\/creativecommons.org\/licenses\/by\/4.0\/ CCBY Content The archive contains different files. A processed high resolution Geotiff in UTM 33N (1200 dpi), a processed JPG in UTM 33N (300 dpi), the raw Geotiff in WGS84, the used Source SHP File with their secondary files, the \u201csources map\u201d PDF and the release notes PDF. The processed UTM 33N Geotiff and JPG are designed for simple and direct usage, while the raw WGS84 Geotiff is for work in different map projections. The original SHP-Files are for work with alternative colour ramps or detailed insight on the used sources and specific reasons for interpolation. Basic Information This is map version 1.0. The map extend is defined from 12\u00b0W to 44\u00b0E and 43\u00b0N to 72\u00b0N. All Data were digitalised from different sources (See sources map), which are listed further down on this site. The modern coastline is derived from Natural Earth (https:\/\/www.naturalearthdata.com), large lakes were added from the \u201cWISE Large rivers and large lakes\u201d dataset provided by the European Environment Agency (https:\/\/www.eea.europa.eu\/data-and-maps\/data\/wise-large-rivers-and-large-lakes). Finally the shaded elevation is calculated on the \u201cGEBCO One Minute Grid\u201d from the \u201cGEBCO Gridded bathymetric Data\u201d (https:\/\/www.gebco.net\/). The maps were produced with QGIS 3. Source notes The British coastline from Brooks et al. 2011 was assumed as the mean value of the 10000 and 8000 BP maps Sea level for the Adriatic sea was set to -30 m a.s.l. based on sea level curve from Moscon et al. 2015 Sea level for the Black sea was set to -5 m a.s.l. based on sea level curve from Lericolais 2017 Minor adjustments were made to smoothen the coastline Version history 09-08-2019 release of Version 1.0.1 29-11-2018 1st\u00a0release of the map Changes to previous version Corrected spelling (&#8222;ice sheet&#8220; instead of &#8222;ice shield&#8220;) in release notes and shape files Corrected timeframe References Bj\u00f6rck, S. 1995. A review of the history of the Baltic Sea, 13.0-8.0 ka BP. Quaternary International 27, 19\u201340. Brooks, A. J., Bradley, S. L., Edwards, R. J. and Goodwyn, N. 2011. The palaeogeography of Northwest Europe during the last 20,000 years. . Journal of Maps 7, 573-587. Cohen, K. M., Westley, K., Erkens, G., Hijma, M. P. and Weerts, H. J. T. 2017: The North Sea. Submerged Landscapes of the European Continental Shelf: John Wiley &amp; Sons, Ltd, 147-186. Edwards, R., Brooks, E., 2008. The Island of Ireland: Drowning the Myth of an Irish Land-bridge?, In: Davenport, J.J., Sleeman, D.P., Woodman, P.C. (Eds.), Mind the Gap: Postglacial Colonisa, pp. 19-34. Harff, J., Flemming, N. C., Groh, A., H\u00fcnicke, B., Lericolais, G., Meschede, M., Rosentau, A., Sakellariou, D., U\u015bcinowicz, S., Zhang, W. and Zorita, E. 2017: Sea Level and Climate. In Flemming, N. C., Harff, J., Moura, D., Burgess, A. and Bailey, G. N., editors, Submerged Landscapes of the European Continental Shelf, Hoboken, NJ: Wiley &amp; Sons, 11-49. Lericolais, G., 2017. Late Pleistocene Environmental Factors defining the Black Sea, and Submerged Landscapes on the Western Continental Shelf, Submerged Landscapes of the European Continental Shelf, John Wiley &amp; Sons, Ltd, pp. 479-495. Moscon, G., Corregiari, A., Stefani, C., Fontana, A. and Remia, A. 2015. Very-high resolution analysis of a transgessive deposit in the Northern Adriactic sea (Italy). Alpine and Mediterranean Quaternary 28, 121-129. P\u00e5sse, T., Andersson, L., 2005. Shore-level displacement in Fennoscandia calculated from empirical data. Gff 127, 253-268. Seguinot, J., Ivy-Ochs, S., Jouvet, G., Huss, M., Funk, M., Preusser, F., 2018. Modelling last glacial cycle ice dynamics in the Alps. The Cryosphere 12, 3265-3285. Stroeven, A.P., H\u00e4ttestrand, C., Kleman, J., Heyman, J., Fabel, D., Fredin, O., Goodfellow, B.W., Harbor, J.M., Jansen, J.D., Olsen, L., Caffee, M.W., Fink, D., Lundqvist, J., Rosqvist, G.C., Str\u00f6mberg, B., Jansson, K.N., 2016. Deglaciation of Fennoscandia. Quaternary Science Reviews 147, 91-121. Subetto, D., Zobkov, M., Potakhin, M., Tarasov, A., 2017. Paleoreconstructions of Lake Onego. Development in the Late Pleistocene and Holocene. Weaver, A.J., Saenko, O.A., Clark, P.U., Mitrovica, J.X., 2003. Meltwater Pulse 1A from Antarctica as a Trigger of the B\u00f8lling-Aller\u00f8d Warm Interval. Science 299, 1709-1713.","thumbnail_url":"https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor1_utm_v10x-1024x711.jpg"}