{"id":5671,"date":"2021-04-14T07:31:25","date_gmt":"2021-04-14T05:31:25","guid":{"rendered":"https:\/\/zbsa.eu\/?p=5671"},"modified":"2021-04-15T09:06:11","modified_gmt":"2021-04-15T07:06:11","slug":"late-boreal","status":"publish","type":"post","link":"https:\/\/zbsa.eu\/en\/late-boreal\/","title":{"rendered":"Late Boreal"},"content":{"rendered":"<div data-elementor-type=\"wp-post\" data-elementor-id=\"5671\" class=\"elementor elementor-5671\" data-elementor-post-type=\"post\">\n\t\t\t\t\t\t<section data-particle_enable=\"false\" data-particle-mobile-disabled=\"false\" class=\"elementor-section elementor-top-section elementor-element elementor-element-687e00fc elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"687e00fc\" data-element_type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-50 elementor-top-column elementor-element elementor-element-20aebb41\" data-id=\"20aebb41\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-6161450 elementor-widget elementor-widget-image\" data-id=\"6161450\" data-element_type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<a href=\"https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_utm_v10x-scaled.jpg\" data-elementor-open-lightbox=\"yes\" data-elementor-lightbox-title=\"Late Boreal map\" data-e-action-hash=\"#elementor-action%3Aaction%3Dlightbox%26settings%3DeyJpZCI6NTY3NiwidXJsIjoiaHR0cHM6XC9cL3pic2EuZXVcL3dwLWNvbnRlbnRcL3VwbG9hZHNcLzIwMjFcLzA0XC9lcGhhX2JvcjJfdXRtX3YxMHgtc2NhbGVkLmpwZyJ9\">\n\t\t\t\t\t\t\t<img fetchpriority=\"high\" decoding=\"async\" width=\"960\" height=\"667\" src=\"https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_utm_v10x-1024x711.jpg\" class=\"attachment-large size-large wp-image-5676\" alt=\"Late Boreal map\" srcset=\"https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_utm_v10x-1024x711.jpg 1024w, https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_utm_v10x-300x208.jpg 300w, https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_utm_v10x-768x533.jpg 768w, https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_utm_v10x-1536x1066.jpg 1536w, https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_utm_v10x-2048x1422.jpg 2048w, https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_utm_v10x-16x12.jpg 16w, https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_utm_v10x-1140x791.jpg 1140w\" sizes=\"(max-width: 960px) 100vw, 960px\" \/>\t\t\t\t\t\t\t\t<\/a>\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t<div class=\"elementor-column elementor-col-50 elementor-top-column elementor-element elementor-element-5d1ae26f\" data-id=\"5d1ae26f\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-559cc80 elementor-widget elementor-widget-image\" data-id=\"559cc80\" data-element_type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<a href=\"https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_v10x_sources_map-scaled.jpg\" data-elementor-open-lightbox=\"yes\" data-elementor-lightbox-title=\"Late Boreal sources map\" data-elementor-lightbox-description=\"Late Boreal sources map\" data-e-action-hash=\"#elementor-action%3Aaction%3Dlightbox%26settings%3DeyJpZCI6NTY3NSwidXJsIjoiaHR0cHM6XC9cL3pic2EuZXVcL3dwLWNvbnRlbnRcL3VwbG9hZHNcLzIwMjFcLzA0XC9lcGhhX2JvcjJfdjEweF9zb3VyY2VzX21hcC1zY2FsZWQuanBnIn0%3D\">\n\t\t\t\t\t\t\t<img decoding=\"async\" width=\"960\" height=\"679\" src=\"https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_v10x_sources_map-1024x724.jpg\" class=\"attachment-large size-large wp-image-5675\" alt=\"Late Boreal sources map\" srcset=\"https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_v10x_sources_map-1024x724.jpg 1024w, https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_v10x_sources_map-300x212.jpg 300w, https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_v10x_sources_map-768x543.jpg 768w, https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_v10x_sources_map-1536x1086.jpg 1536w, https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_v10x_sources_map-2048x1448.jpg 2048w, https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_v10x_sources_map-16x12.jpg 16w, https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_v10x_sources_map-1140x806.jpg 1140w\" sizes=\"(max-width: 960px) 100vw, 960px\" \/>\t\t\t\t\t\t\t\t<\/a>\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section data-particle_enable=\"false\" data-particle-mobile-disabled=\"false\" class=\"elementor-section elementor-top-section elementor-element elementor-element-5bb55b48 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"5bb55b48\" data-element_type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-1af121e2\" data-id=\"1af121e2\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-7d3b8717 elementor-widget elementor-widget-text-editor\" data-id=\"7d3b8717\" data-element_type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p><strong>Version 1.0.1<\/strong><\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section data-particle_enable=\"false\" data-particle-mobile-disabled=\"false\" class=\"elementor-section elementor-top-section elementor-element elementor-element-2dd40f13 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"2dd40f13\" data-element_type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-790c2bae\" data-id=\"790c2bae\" data-element_type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-11d0bd1a elementor-widget elementor-widget-toggle\" data-id=\"11d0bd1a\" data-element_type=\"widget\" data-widget_type=\"toggle.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t<div class=\"elementor-toggle\">\n\t\t\t\t\t\t\t<div class=\"elementor-toggle-item\">\n\t\t\t\t\t<div id=\"elementor-tab-title-2981\" class=\"elementor-tab-title\" data-tab=\"1\" role=\"button\" aria-controls=\"elementor-tab-content-2981\" aria-expanded=\"false\">\n\t\t\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon elementor-toggle-icon-left\" aria-hidden=\"true\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon-closed\"><i class=\"fas fa-caret-down\"><\/i><\/span>\n\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon-opened\"><i class=\"elementor-toggle-icon-opened fas fa-caret-up\"><\/i><\/span>\n\t\t\t\t\t\t\t\t\t\t\t\t\t<\/span>\n\t\t\t\t\t\t\t\t\t\t\t\t<a class=\"elementor-toggle-title\" tabindex=\"0\">Files<\/a>\n\t\t\t\t\t<\/div>\n\n\t\t\t\t\t<div id=\"elementor-tab-content-2981\" class=\"elementor-tab-content elementor-clearfix\" data-tab=\"1\" role=\"region\" aria-labelledby=\"elementor-tab-title-2981\"><p><a href=\"https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/EPHA_Bor2_v101.zip\">Late Boreal version 1.0.1<\/a><\/p><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t\t<div class=\"elementor-toggle-item\">\n\t\t\t\t\t<div id=\"elementor-tab-title-2982\" class=\"elementor-tab-title\" data-tab=\"2\" role=\"button\" aria-controls=\"elementor-tab-content-2982\" aria-expanded=\"false\">\n\t\t\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon elementor-toggle-icon-left\" aria-hidden=\"true\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon-closed\"><i class=\"fas fa-caret-down\"><\/i><\/span>\n\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon-opened\"><i class=\"elementor-toggle-icon-opened fas fa-caret-up\"><\/i><\/span>\n\t\t\t\t\t\t\t\t\t\t\t\t\t<\/span>\n\t\t\t\t\t\t\t\t\t\t\t\t<a class=\"elementor-toggle-title\" tabindex=\"0\">Citation<\/a>\n\t\t\t\t\t<\/div>\n\n\t\t\t\t\t<div id=\"elementor-tab-content-2982\" class=\"elementor-tab-content elementor-clearfix\" data-tab=\"2\" role=\"region\" aria-labelledby=\"elementor-tab-title-2982\"><p>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; P\u00e5sse\/Andersson 2005; Seguinot et al. 2018; Stroeven et al. 2016; Subetto et al. 2017; Weaver et al. 2003&#8220;<\/p><p>For full references see below.<\/p><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t\t<div class=\"elementor-toggle-item\">\n\t\t\t\t\t<div id=\"elementor-tab-title-2983\" class=\"elementor-tab-title\" data-tab=\"3\" role=\"button\" aria-controls=\"elementor-tab-content-2983\" aria-expanded=\"false\">\n\t\t\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon elementor-toggle-icon-left\" aria-hidden=\"true\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon-closed\"><i class=\"fas fa-caret-down\"><\/i><\/span>\n\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon-opened\"><i class=\"elementor-toggle-icon-opened fas fa-caret-up\"><\/i><\/span>\n\t\t\t\t\t\t\t\t\t\t\t\t\t<\/span>\n\t\t\t\t\t\t\t\t\t\t\t\t<a class=\"elementor-toggle-title\" tabindex=\"0\">Timeslice<\/a>\n\t\t\t\t\t<\/div>\n\n\t\t\t\t\t<div id=\"elementor-tab-content-2983\" class=\"elementor-tab-content elementor-clearfix\" data-tab=\"3\" role=\"region\" aria-labelledby=\"elementor-tab-title-2983\"><p>The map is approximately representing the timeslice:<\/p><div class=\"wp-block\" data-align=\"left\"><figure id=\"block-c5a791c7-6678-425e-b68a-029cde18cb41\" class=\"wp-block-table block-editor-block-list__block\" tabindex=\"0\" role=\"group\" aria-label=\"Block: Tabelle\" data-block=\"c5a791c7-6678-425e-b68a-029cde18cb41\" data-type=\"core\/table\" data-title=\"Tabelle\"><table><tbody><tr><td class=\"block-editor-rich-text__editable wp-block-table__cell-content rich-text\" role=\"textbox\" aria-multiline=\"true\" aria-label=\"Text der Body-Zelle\"><strong>chronological frame<\/strong><\/td><td class=\"block-editor-rich-text__editable wp-block-table__cell-content rich-text\" role=\"textbox\" aria-multiline=\"true\" aria-label=\"Text der Body-Zelle\"><strong>timeslice<\/strong><\/td><\/tr><tr><td class=\"block-editor-rich-text__editable wp-block-table__cell-content rich-text\" role=\"textbox\" aria-multiline=\"true\" aria-label=\"Text der Body-Zelle\">Greenlandic isotope chronology<\/td><td class=\"block-editor-rich-text__editable wp-block-table__cell-content rich-text\" role=\"textbox\" aria-multiline=\"true\" aria-label=\"Text der Body-Zelle\">&#8211;<\/td><\/tr><tr><td class=\"block-editor-rich-text__editable wp-block-table__cell-content rich-text\" role=\"textbox\" aria-multiline=\"true\" aria-label=\"Text der Body-Zelle\">years calibrated BC<\/td><td class=\"block-editor-rich-text__editable wp-block-table__cell-content rich-text\" role=\"textbox\" aria-multiline=\"true\" aria-label=\"Text der Body-Zelle\">8000\u20137200<\/td><\/tr><tr><td class=\"block-editor-rich-text__editable wp-block-table__cell-content rich-text\" role=\"textbox\" aria-multiline=\"true\" aria-label=\"Text der Body-Zelle\">year calibrated BP<\/td><td class=\"block-editor-rich-text__editable wp-block-table__cell-content rich-text\" role=\"textbox\" aria-multiline=\"true\" aria-label=\"Text der Body-Zelle\">10000\u20139200<\/td><\/tr><tr><td class=\"block-editor-rich-text__editable wp-block-table__cell-content rich-text\" role=\"textbox\" aria-multiline=\"true\" aria-label=\"Text der Body-Zelle\"><sup>14<\/sup>C years BP<\/td><td class=\"block-editor-rich-text__editable wp-block-table__cell-content rich-text\" role=\"textbox\" aria-multiline=\"true\" aria-label=\"Text der Body-Zelle\">8800\u20138500<\/td><\/tr><\/tbody><tfoot><\/tfoot><\/table><figcaption class=\"block-editor-rich-text__editable rich-text\" role=\"textbox\" aria-multiline=\"true\" aria-label=\"Tabellen-Beschriftungs-Text\"><\/figcaption><\/figure><\/div><div class=\"block-list-appender wp-block\" tabindex=\"-1\">\u00a0<\/div><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t\t<div class=\"elementor-toggle-item\">\n\t\t\t\t\t<div id=\"elementor-tab-title-2984\" class=\"elementor-tab-title\" data-tab=\"4\" role=\"button\" aria-controls=\"elementor-tab-content-2984\" aria-expanded=\"false\">\n\t\t\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon elementor-toggle-icon-left\" aria-hidden=\"true\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon-closed\"><i class=\"fas fa-caret-down\"><\/i><\/span>\n\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon-opened\"><i class=\"elementor-toggle-icon-opened fas fa-caret-up\"><\/i><\/span>\n\t\t\t\t\t\t\t\t\t\t\t\t\t<\/span>\n\t\t\t\t\t\t\t\t\t\t\t\t<a class=\"elementor-toggle-title\" tabindex=\"0\">Release notes<\/a>\n\t\t\t\t\t<\/div>\n\n\t\t\t\t\t<div id=\"elementor-tab-content-2984\" class=\"elementor-tab-content elementor-clearfix\" data-tab=\"4\" role=\"region\" aria-labelledby=\"elementor-tab-title-2984\"><p>This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this license, visit <a href=\"https:\/\/creativecommons.org\/licenses\/by\/4.0\/\" target=\"_blank\" rel=\"noopener\">https:\/\/creativecommons.org\/licenses\/by\/4.0\/<\/a><\/p><figure id=\"attachment_5345\" aria-describedby=\"caption-attachment-5345\" style=\"width: 200px\" class=\"wp-caption alignleft\"><img decoding=\"async\" class=\"wp-image-5345\" src=\"https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/zbsa-300x106.png\" alt=\"CCBY\" width=\"200\" height=\"71\" srcset=\"https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/zbsa-300x106.png 300w, https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/zbsa-1024x361.png 1024w, https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/zbsa-768x271.png 768w, https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/zbsa-1536x541.png 1536w, https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/zbsa-16x6.png 16w, https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/zbsa-1140x402.png 1140w, https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/zbsa.png 2000w\" sizes=\"(max-width: 200px) 100vw, 200px\" \/><figcaption id=\"caption-attachment-5345\" class=\"wp-caption-text\">CCBY<\/figcaption><\/figure><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t\t<div class=\"elementor-toggle-item\">\n\t\t\t\t\t<div id=\"elementor-tab-title-2985\" class=\"elementor-tab-title\" data-tab=\"5\" role=\"button\" aria-controls=\"elementor-tab-content-2985\" aria-expanded=\"false\">\n\t\t\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon elementor-toggle-icon-left\" aria-hidden=\"true\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon-closed\"><i class=\"fas fa-caret-down\"><\/i><\/span>\n\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon-opened\"><i class=\"elementor-toggle-icon-opened fas fa-caret-up\"><\/i><\/span>\n\t\t\t\t\t\t\t\t\t\t\t\t\t<\/span>\n\t\t\t\t\t\t\t\t\t\t\t\t<a class=\"elementor-toggle-title\" tabindex=\"0\">Content<\/a>\n\t\t\t\t\t<\/div>\n\n\t\t\t\t\t<div id=\"elementor-tab-content-2985\" class=\"elementor-tab-content elementor-clearfix\" data-tab=\"5\" role=\"region\" aria-labelledby=\"elementor-tab-title-2985\"><p>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.<\/p><p>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.<\/p><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t\t<div class=\"elementor-toggle-item\">\n\t\t\t\t\t<div id=\"elementor-tab-title-2986\" class=\"elementor-tab-title\" data-tab=\"6\" role=\"button\" aria-controls=\"elementor-tab-content-2986\" aria-expanded=\"false\">\n\t\t\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon elementor-toggle-icon-left\" aria-hidden=\"true\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon-closed\"><i class=\"fas fa-caret-down\"><\/i><\/span>\n\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon-opened\"><i class=\"elementor-toggle-icon-opened fas fa-caret-up\"><\/i><\/span>\n\t\t\t\t\t\t\t\t\t\t\t\t\t<\/span>\n\t\t\t\t\t\t\t\t\t\t\t\t<a class=\"elementor-toggle-title\" tabindex=\"0\">Basic Information<\/a>\n\t\t\t\t\t<\/div>\n\n\t\t\t\t\t<div id=\"elementor-tab-content-2986\" class=\"elementor-tab-content elementor-clearfix\" data-tab=\"6\" role=\"region\" aria-labelledby=\"elementor-tab-title-2986\"><p>This is map version <strong>1.0.<\/strong> 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.<\/p><p>The modern coastline is derived from Natural Earth (<a href=\"https:\/\/www.naturalearthdata.com\" target=\"_blank\" rel=\"noopener\">https:\/\/www.naturalearthdata.com<\/a>), large lakes were added from the \u201cWISE Large rivers and large lakes\u201d dataset provided by the European Environment Agency (<a href=\"https:\/\/www.eea.europa.eu\/data-and-maps\/data\/wise-large-rivers-and-large-lakes\" target=\"_blank\" rel=\"noopener\">https:\/\/www.eea.europa.eu\/data-and-maps\/data\/wise-large-rivers-and-large-lakes<\/a>). Finally the shaded elevation is calculated on the \u201cGEBCO One Minute Grid\u201d from the \u201cGEBCO Gridded bathymetric Data\u201d (<a href=\"https:\/\/www.gebco.net\/\" target=\"_blank\" rel=\"noopener\">https:\/\/www.gebco.net\/<\/a>).<\/p><p>The maps were produced with QGIS 3.<\/p><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t\t<div class=\"elementor-toggle-item\">\n\t\t\t\t\t<div id=\"elementor-tab-title-2987\" class=\"elementor-tab-title\" data-tab=\"7\" role=\"button\" aria-controls=\"elementor-tab-content-2987\" aria-expanded=\"false\">\n\t\t\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon elementor-toggle-icon-left\" aria-hidden=\"true\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon-closed\"><i class=\"fas fa-caret-down\"><\/i><\/span>\n\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon-opened\"><i class=\"elementor-toggle-icon-opened fas fa-caret-up\"><\/i><\/span>\n\t\t\t\t\t\t\t\t\t\t\t\t\t<\/span>\n\t\t\t\t\t\t\t\t\t\t\t\t<a class=\"elementor-toggle-title\" tabindex=\"0\">Source notes<\/a>\n\t\t\t\t\t<\/div>\n\n\t\t\t\t\t<div id=\"elementor-tab-content-2987\" class=\"elementor-tab-content elementor-clearfix\" data-tab=\"7\" role=\"region\" aria-labelledby=\"elementor-tab-title-2987\"><ul><li>Fennoscandian ice sheet data that is not corresponding with Stroeven et al. 2017 was removed and replaced by either water or land areas<\/li><li>The interpolation of the Swedish coastline is approximated on steps between 280 m a.s.l. (most southern part of interpolated area) to 220 m a.s.l. (most northern part of interpolated area)<\/li><li>Sea level for the Adriatic sea was set to -20 m a.s.l. based on sea level curve from Moscon et al. 2015<\/li><li>Sea level for the Black sea was set to -2 m a.s.l. based on sea level curve from Lericolais2017<\/li><li>Minor adjustments were made to smoothen the coastline<\/li><\/ul><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t\t<div class=\"elementor-toggle-item\">\n\t\t\t\t\t<div id=\"elementor-tab-title-2988\" class=\"elementor-tab-title\" data-tab=\"8\" role=\"button\" aria-controls=\"elementor-tab-content-2988\" aria-expanded=\"false\">\n\t\t\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon elementor-toggle-icon-left\" aria-hidden=\"true\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon-closed\"><i class=\"fas fa-caret-down\"><\/i><\/span>\n\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon-opened\"><i class=\"elementor-toggle-icon-opened fas fa-caret-up\"><\/i><\/span>\n\t\t\t\t\t\t\t\t\t\t\t\t\t<\/span>\n\t\t\t\t\t\t\t\t\t\t\t\t<a class=\"elementor-toggle-title\" tabindex=\"0\">Version history<\/a>\n\t\t\t\t\t<\/div>\n\n\t\t\t\t\t<div id=\"elementor-tab-content-2988\" class=\"elementor-tab-content elementor-clearfix\" data-tab=\"8\" role=\"region\" aria-labelledby=\"elementor-tab-title-2988\"><table><tbody><tr><td role=\"textbox\" aria-multiline=\"true\" aria-label=\"Text der Body-Zelle\">09-08-2019<\/td><td role=\"textbox\" aria-multiline=\"true\" aria-label=\"Text der Body-Zelle\">release of Version 1.0.1<\/td><\/tr><tr><td role=\"textbox\" aria-multiline=\"true\" aria-label=\"Text der Body-Zelle\">29-11-2018<\/td><td role=\"textbox\" aria-multiline=\"true\" aria-label=\"Text der Body-Zelle\">1<sup>st<\/sup>\u00a0release of the map<\/td><\/tr><\/tbody><tfoot><\/tfoot><\/table><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t\t<div class=\"elementor-toggle-item\">\n\t\t\t\t\t<div id=\"elementor-tab-title-2989\" class=\"elementor-tab-title\" data-tab=\"9\" role=\"button\" aria-controls=\"elementor-tab-content-2989\" aria-expanded=\"false\">\n\t\t\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon elementor-toggle-icon-left\" aria-hidden=\"true\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon-closed\"><i class=\"fas fa-caret-down\"><\/i><\/span>\n\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon-opened\"><i class=\"elementor-toggle-icon-opened fas fa-caret-up\"><\/i><\/span>\n\t\t\t\t\t\t\t\t\t\t\t\t\t<\/span>\n\t\t\t\t\t\t\t\t\t\t\t\t<a class=\"elementor-toggle-title\" tabindex=\"0\">Changes to previous version<\/a>\n\t\t\t\t\t<\/div>\n\n\t\t\t\t\t<div id=\"elementor-tab-content-2989\" class=\"elementor-tab-content elementor-clearfix\" data-tab=\"9\" role=\"region\" aria-labelledby=\"elementor-tab-title-2989\"><ul><li>Corrected spelling (&#8222;ice sheet&#8220; instead of &#8222;ice shield&#8220;) in release notes and shape files<\/li><\/ul><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t\t<div class=\"elementor-toggle-item\">\n\t\t\t\t\t<div id=\"elementor-tab-title-29810\" class=\"elementor-tab-title\" data-tab=\"10\" role=\"button\" aria-controls=\"elementor-tab-content-29810\" aria-expanded=\"false\">\n\t\t\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon elementor-toggle-icon-left\" aria-hidden=\"true\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon-closed\"><i class=\"fas fa-caret-down\"><\/i><\/span>\n\t\t\t\t\t\t\t\t<span class=\"elementor-toggle-icon-opened\"><i class=\"elementor-toggle-icon-opened fas fa-caret-up\"><\/i><\/span>\n\t\t\t\t\t\t\t\t\t\t\t\t\t<\/span>\n\t\t\t\t\t\t\t\t\t\t\t\t<a class=\"elementor-toggle-title\" tabindex=\"0\">References<\/a>\n\t\t\t\t\t<\/div>\n\n\t\t\t\t\t<div id=\"elementor-tab-content-29810\" class=\"elementor-tab-content elementor-clearfix\" data-tab=\"10\" role=\"region\" aria-labelledby=\"elementor-tab-title-29810\"><div id=\"parent-fieldname-text\" class=\"plain\"><p>Bj\u00f6rck, S. 1995. A review of the history of the Baltic Sea, 13.0-8.0 ka BP. Quaternary International 27, 19\u201340.<\/p><p>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.<\/p><p>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.<\/p><p>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.<\/p><p>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.<\/p><p>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.<\/p><p>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><p>P\u00e5sse, T., Andersson, L., 2005. Shore-level displacement in Fennoscandia calculated from empirical data. Gff 127, 253-268.<\/p><p>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.<\/p><p>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.<\/p><p>Subetto, D., Zobkov, M., Potakhin, M., Tarasov, A., 2017. Paleoreconstructions of Lake Onego. Development in the Late Pleistocene and Holocene.<\/p><p>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.<\/p><\/div><div class=\"visualClear\">\u00a0<\/div><div class=\"relatedItems\">\u00a0<\/div><div class=\"visualClear\">\u00a0<\/div><div class=\"documentActions\"><h5 class=\"hiddenStructure\">Artikelaktionen<\/h5><\/div><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<\/div>","protected":false},"excerpt":{"rendered":"<p>Version 1.0.1 Files Late 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; P\u00e5sse\/Andersson 2005; Seguinot et al. 2018; Stroeven et al. 2016; Subetto et al. 2017; Weaver et al. 2003&#8220; For full references see below. Timeslice The map is approximately representing the timeslice: chronological frame timeslice Greenlandic isotope chronology &#8211; years calibrated BC 8000\u20137200 year calibrated BP 10000\u20139200 14C years BP 8800\u20138500 \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 Fennoscandian ice sheet data that is not corresponding with Stroeven et al. 2017 was removed and replaced by either water or land areas The interpolation of the Swedish coastline is approximated on steps between 280 m a.s.l. (most southern part of interpolated area) to 220 m a.s.l. (most northern part of interpolated area) Sea level for the Adriatic sea was set to -20 m a.s.l. based on sea level curve from Moscon et al. 2015 Sea level for the Black sea was set to -2 m a.s.l. based on sea level curve from Lericolais2017 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 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. \u00a0\u00a0\u00a0 Artikelaktionen<\/p>","protected":false},"author":3,"featured_media":0,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_eb_attr":"","inline_featured_image":false,"footnotes":""},"categories":[80],"tags":[],"class_list":["post-5671","post","type-post","status-publish","format-standard","hentry","category-epha"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v24.4 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Late Boreal - Zentrum f\u00fcr Baltische und Skandinavische Arch\u00e4ologie (ZBSA) \u2014 Zentrum f\u00fcr Baltische und Skandinavische Arch\u00e4ologie<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/zbsa.eu\/en\/late-boreal\/\" \/>\n<meta property=\"og:locale\" content=\"en_GB\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Late Boreal - Zentrum f\u00fcr Baltische und Skandinavische Arch\u00e4ologie (ZBSA) \u2014 Zentrum f\u00fcr Baltische und Skandinavische Arch\u00e4ologie\" \/>\n<meta property=\"og:description\" content=\"Version 1.0.1 Files Late 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; P\u00e5sse\/Andersson 2005; Seguinot et al. 2018; Stroeven et al. 2016; Subetto et al. 2017; Weaver et al. 2003&#8220; For full references see below. Timeslice The map is approximately representing the timeslice: chronological frame timeslice Greenlandic isotope chronology &#8211; years calibrated BC 8000\u20137200 year calibrated BP 10000\u20139200 14C years BP 8800\u20138500 \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 Fennoscandian ice sheet data that is not corresponding with Stroeven et al. 2017 was removed and replaced by either water or land areas The interpolation of the Swedish coastline is approximated on steps between 280 m a.s.l. (most southern part of interpolated area) to 220 m a.s.l. (most northern part of interpolated area) Sea level for the Adriatic sea was set to -20 m a.s.l. based on sea level curve from Moscon et al. 2015 Sea level for the Black sea was set to -2 m a.s.l. based on sea level curve from Lericolais2017 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 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. \u00a0\u00a0\u00a0 Artikelaktionen\" \/>\n<meta property=\"og:url\" content=\"https:\/\/zbsa.eu\/en\/late-boreal\/\" \/>\n<meta property=\"og:site_name\" content=\"Zentrum f\u00fcr Baltische und Skandinavische Arch\u00e4ologie (ZBSA) \u2014 Zentrum f\u00fcr Baltische und Skandinavische Arch\u00e4ologie\" \/>\n<meta property=\"article:published_time\" content=\"2021-04-14T05:31:25+00:00\" \/>\n<meta property=\"article:modified_time\" content=\"2021-04-15T07:06:11+00:00\" \/>\n<meta property=\"og:image\" content=\"https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_utm_v10x-1024x711.jpg\" \/>\n<meta name=\"author\" content=\"Matthias Bolte\" \/>\n<meta name=\"twitter:card\" content=\"summary_large_image\" \/>\n<meta name=\"twitter:label1\" content=\"Written by\" \/>\n\t<meta name=\"twitter:data1\" content=\"Matthias Bolte\" \/>\n\t<meta name=\"twitter:label2\" content=\"Estimated reading time\" \/>\n\t<meta name=\"twitter:data2\" content=\"4 minutes\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\/\/schema.org\",\"@graph\":[{\"@type\":\"WebPage\",\"@id\":\"https:\/\/zbsa.eu\/late-boreal\/\",\"url\":\"https:\/\/zbsa.eu\/late-boreal\/\",\"name\":\"Late Boreal - Zentrum f\u00fcr Baltische und Skandinavische Arch\u00e4ologie (ZBSA) \u2014 Zentrum f\u00fcr Baltische und Skandinavische Arch\u00e4ologie\",\"isPartOf\":{\"@id\":\"https:\/\/zbsa.eu\/#website\"},\"primaryImageOfPage\":{\"@id\":\"https:\/\/zbsa.eu\/late-boreal\/#primaryimage\"},\"image\":{\"@id\":\"https:\/\/zbsa.eu\/late-boreal\/#primaryimage\"},\"thumbnailUrl\":\"https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_utm_v10x-1024x711.jpg\",\"datePublished\":\"2021-04-14T05:31:25+00:00\",\"dateModified\":\"2021-04-15T07:06:11+00:00\",\"author\":{\"@id\":\"https:\/\/zbsa.eu\/#\/schema\/person\/b980623b66a6ffb097697286521920c5\"},\"breadcrumb\":{\"@id\":\"https:\/\/zbsa.eu\/late-boreal\/#breadcrumb\"},\"inLanguage\":\"en-GB\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[\"https:\/\/zbsa.eu\/late-boreal\/\"]}]},{\"@type\":\"ImageObject\",\"inLanguage\":\"en-GB\",\"@id\":\"https:\/\/zbsa.eu\/late-boreal\/#primaryimage\",\"url\":\"https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_utm_v10x-1024x711.jpg\",\"contentUrl\":\"https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_utm_v10x-1024x711.jpg\"},{\"@type\":\"BreadcrumbList\",\"@id\":\"https:\/\/zbsa.eu\/late-boreal\/#breadcrumb\",\"itemListElement\":[{\"@type\":\"ListItem\",\"position\":1,\"name\":\"Startseite\",\"item\":\"https:\/\/zbsa.eu\/\"},{\"@type\":\"ListItem\",\"position\":2,\"name\":\"Open Access\",\"item\":\"https:\/\/zbsa.eu\/category\/open_access\/\"},{\"@type\":\"ListItem\",\"position\":3,\"name\":\"EPHA\",\"item\":\"https:\/\/zbsa.eu\/category\/open_access\/epha\/\"},{\"@type\":\"ListItem\",\"position\":4,\"name\":\"Late Boreal\"}]},{\"@type\":\"WebSite\",\"@id\":\"https:\/\/zbsa.eu\/#website\",\"url\":\"https:\/\/zbsa.eu\/\",\"name\":\"Zentrum f\u00fcr Baltische und Skandinavische Arch\u00e4ologie (ZBSA) \u2014 Zentrum f\u00fcr Baltische und Skandinavische Arch\u00e4ologie\",\"description\":\"\",\"potentialAction\":[{\"@type\":\"SearchAction\",\"target\":{\"@type\":\"EntryPoint\",\"urlTemplate\":\"https:\/\/zbsa.eu\/?s={search_term_string}\"},\"query-input\":{\"@type\":\"PropertyValueSpecification\",\"valueRequired\":true,\"valueName\":\"search_term_string\"}}],\"inLanguage\":\"en-GB\"},{\"@type\":\"Person\",\"@id\":\"https:\/\/zbsa.eu\/#\/schema\/person\/b980623b66a6ffb097697286521920c5\",\"name\":\"Matthias Bolte\",\"image\":{\"@type\":\"ImageObject\",\"inLanguage\":\"en-GB\",\"@id\":\"https:\/\/zbsa.eu\/#\/schema\/person\/image\/\",\"url\":\"https:\/\/secure.gravatar.com\/avatar\/1f3bc1bfe4b641855cb944e558d4f3de1b57120f6dfe8f4368ebfe0384a5acab?s=96&d=mm&r=g\",\"contentUrl\":\"https:\/\/secure.gravatar.com\/avatar\/1f3bc1bfe4b641855cb944e558d4f3de1b57120f6dfe8f4368ebfe0384a5acab?s=96&d=mm&r=g\",\"caption\":\"Matthias Bolte\"},\"url\":\"https:\/\/zbsa.eu\/en\/author\/matthias-bolte\/\"}]}<\/script>\n<!-- \/ Yoast SEO plugin. -->","yoast_head_json":{"title":"Late Boreal - Zentrum f\u00fcr Baltische und Skandinavische Arch\u00e4ologie (ZBSA) \u2014 Zentrum f\u00fcr Baltische und Skandinavische Arch\u00e4ologie","robots":{"index":"index","follow":"follow","max-snippet":"max-snippet:-1","max-image-preview":"max-image-preview:large","max-video-preview":"max-video-preview:-1"},"canonical":"https:\/\/zbsa.eu\/en\/late-boreal\/","og_locale":"en_GB","og_type":"article","og_title":"Late Boreal - Zentrum f\u00fcr Baltische und Skandinavische Arch\u00e4ologie (ZBSA) \u2014 Zentrum f\u00fcr Baltische und Skandinavische Arch\u00e4ologie","og_description":"Version 1.0.1 Files Late 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; P\u00e5sse\/Andersson 2005; Seguinot et al. 2018; Stroeven et al. 2016; Subetto et al. 2017; Weaver et al. 2003&#8220; For full references see below. Timeslice The map is approximately representing the timeslice: chronological frame timeslice Greenlandic isotope chronology &#8211; years calibrated BC 8000\u20137200 year calibrated BP 10000\u20139200 14C years BP 8800\u20138500 \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 Fennoscandian ice sheet data that is not corresponding with Stroeven et al. 2017 was removed and replaced by either water or land areas The interpolation of the Swedish coastline is approximated on steps between 280 m a.s.l. (most southern part of interpolated area) to 220 m a.s.l. (most northern part of interpolated area) Sea level for the Adriatic sea was set to -20 m a.s.l. based on sea level curve from Moscon et al. 2015 Sea level for the Black sea was set to -2 m a.s.l. based on sea level curve from Lericolais2017 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 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. \u00a0\u00a0\u00a0 Artikelaktionen","og_url":"https:\/\/zbsa.eu\/en\/late-boreal\/","og_site_name":"Zentrum f\u00fcr Baltische und Skandinavische Arch\u00e4ologie (ZBSA) \u2014 Zentrum f\u00fcr Baltische und Skandinavische Arch\u00e4ologie","article_published_time":"2021-04-14T05:31:25+00:00","article_modified_time":"2021-04-15T07:06:11+00:00","og_image":[{"url":"https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_utm_v10x-1024x711.jpg","type":"","width":"","height":""}],"author":"Matthias Bolte","twitter_card":"summary_large_image","twitter_misc":{"Written by":"Matthias Bolte","Estimated reading time":"4 minutes"},"schema":{"@context":"https:\/\/schema.org","@graph":[{"@type":"WebPage","@id":"https:\/\/zbsa.eu\/late-boreal\/","url":"https:\/\/zbsa.eu\/late-boreal\/","name":"Late Boreal - Zentrum f\u00fcr Baltische und Skandinavische Arch\u00e4ologie (ZBSA) \u2014 Zentrum f\u00fcr Baltische und Skandinavische 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Access","item":"https:\/\/zbsa.eu\/category\/open_access\/"},{"@type":"ListItem","position":3,"name":"EPHA","item":"https:\/\/zbsa.eu\/category\/open_access\/epha\/"},{"@type":"ListItem","position":4,"name":"Late Boreal"}]},{"@type":"WebSite","@id":"https:\/\/zbsa.eu\/#website","url":"https:\/\/zbsa.eu\/","name":"Zentrum f\u00fcr Baltische und Skandinavische Arch\u00e4ologie (ZBSA) \u2014 Zentrum f\u00fcr Baltische und Skandinavische Arch\u00e4ologie","description":"","potentialAction":[{"@type":"SearchAction","target":{"@type":"EntryPoint","urlTemplate":"https:\/\/zbsa.eu\/?s={search_term_string}"},"query-input":{"@type":"PropertyValueSpecification","valueRequired":true,"valueName":"search_term_string"}}],"inLanguage":"en-GB"},{"@type":"Person","@id":"https:\/\/zbsa.eu\/#\/schema\/person\/b980623b66a6ffb097697286521920c5","name":"Matthias Bolte","image":{"@type":"ImageObject","inLanguage":"en-GB","@id":"https:\/\/zbsa.eu\/#\/schema\/person\/image\/","url":"https:\/\/secure.gravatar.com\/avatar\/1f3bc1bfe4b641855cb944e558d4f3de1b57120f6dfe8f4368ebfe0384a5acab?s=96&d=mm&r=g","contentUrl":"https:\/\/secure.gravatar.com\/avatar\/1f3bc1bfe4b641855cb944e558d4f3de1b57120f6dfe8f4368ebfe0384a5acab?s=96&d=mm&r=g","caption":"Matthias Bolte"},"url":"https:\/\/zbsa.eu\/en\/author\/matthias-bolte\/"}]}},"featured_image_src":" ","featured_image_src_square":" ","author_info":{"display_name":"Matthias Bolte","author_link":"https:\/\/zbsa.eu\/en\/author\/matthias-bolte\/"},"category_info":"<a href=\"https:\/\/zbsa.eu\/en\/category\/open_access\/epha\/\" rel=\"category tag\">EPHA<\/a>","tags_info":"","social_share_info":"<a data-share=\"facebook\" href=\"https:\/\/www.facebook.com\/sharer.php?u=https:\/\/zbsa.eu\/en\/late-boreal\/\" class=\"pl-facebook-share social-share-default pl-social-share\" target=\"_blank\"><i class=\"fab fa-facebook-f\" aria-hidden=\"true\"><\/i><\/a><a data-share=\"twitter\" href=\"https:\/\/twitter.com\/share?url=https:\/\/zbsa.eu\/en\/late-boreal\/\" class=\"pl-twiiter-share social-share-default pl-social-share\" target=\"_blank\"><i class=\"fab fa-twitter\" aria-hidden=\"true\"><\/i><\/a><a data-share=\"linkedin\" href=\"https:\/\/www.linkedin.com\/shareArticle?url=https:\/\/zbsa.eu\/en\/late-boreal\/\" class=\"pl-linkedin-share social-share-default pl-social-share\" target=\"_blank\"><i class=\"fab fa-linkedin-in\" aria-hidden=\"true\"><\/i><\/a>","wordExcerpt_info":"<p><a href=\"https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_utm_v10x-scaled.jpg\" data-elementor-open-lightbox=\"yes\" data-elementor-lightbox-title=\"Late Boreal map\"><br \/>\n\t\t\t\t\t\t\t<img loading=\"lazy\" width=\"960\" height=\"667\" src=\"https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_utm_v10x-1024x711.jpg\" alt=\"Late Boreal map\" \/>\t\t\t\t\t\t\t\t<\/a><br \/>\n\t\t\t\t\t\t\t\t\t\t\t<a href=\"https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_v10x_sources_map-scaled.jpg\" data-elementor-open-lightbox=\"yes\" data-elementor-lightbox-title=\"Late Boreal sources map\" data-elementor-lightbox-description=\"Late Boreal sources map\"><br \/>\n\t\t\t\t\t\t\t<img loading=\"lazy\" width=\"960\" height=\"679\" src=\"https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/epha_bor2_v10x_sources_map-1024x724.jpg\" alt=\"Late Boreal sources map\" \/>\t\t\t\t\t\t\t\t<\/a><\/p>\n<p><strong>Version 1.0.1<\/strong><\/p>\n<p>\t\t\t\t\t\t\t\t\t\t\t\t<a href=\"\">Files<\/a><\/p>\n<p><a href=\"https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/EPHA_Bor2_v101.zip\">Late Boreal version 1.0.1<\/a><\/p>\n<p>\t\t\t\t\t\t\t\t\t\t\t\t<a href=\"\">Citation<\/a><\/p>\n<p>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; P\u00e5sse\/Andersson 2005; Seguinot et al. 2018; Stroeven et al. 2016; Subetto et al. 2017; Weaver et al. 2003&#8220;<\/p>\n<p>For full references see below.<\/p>\n<p>\t\t\t\t\t\t\t\t\t\t\t\t<a href=\"\">Timeslice<\/a><\/p>\n<p>The map is approximately representing the timeslice:<\/p>\n<figure id=\"block-c5a791c7-6678-425e-b68a-029cde18cb41\" role=\"group\" aria-label=\"Block: Tabelle\" data-block=\"c5a791c7-6678-425e-b68a-029cde18cb41\" data-type=\"core\/table\" data-title=\"Tabelle\">\n<table>\n<tbody>\n<tr>\n<td role=\"textbox\" aria-label=\"Text der Body-Zelle\"><strong>chronological frame<\/strong><\/td>\n<td role=\"textbox\" aria-label=\"Text der Body-Zelle\"><strong>timeslice<\/strong><\/td>\n<\/tr>\n<tr>\n<td role=\"textbox\" aria-label=\"Text der Body-Zelle\">Greenlandic isotope chronology<\/td>\n<td role=\"textbox\" aria-label=\"Text der Body-Zelle\">&#8211;<\/td>\n<\/tr>\n<tr>\n<td role=\"textbox\" aria-label=\"Text der Body-Zelle\">years calibrated BC<\/td>\n<td role=\"textbox\" aria-label=\"Text der Body-Zelle\">8000\u20137200<\/td>\n<\/tr>\n<tr>\n<td role=\"textbox\" aria-label=\"Text der Body-Zelle\">year calibrated BP<\/td>\n<td role=\"textbox\" aria-label=\"Text der Body-Zelle\">10000\u20139200<\/td>\n<\/tr>\n<tr>\n<td role=\"textbox\" aria-label=\"Text der Body-Zelle\"><sup>14<\/sup>C years BP<\/td>\n<td role=\"textbox\" aria-label=\"Text der Body-Zelle\">8800\u20138500<\/td>\n<\/tr>\n<\/tbody>\n<tfoot><\/tfoot>\n<\/table><figcaption role=\"textbox\" aria-label=\"Tabellen-Beschriftungs-Text\"><\/figcaption><\/figure>\n<p>\u00a0<br \/>\n\t\t\t\t\t\t\t\t\t\t\t\t<a href=\"\">Release notes<\/a><\/p>\n<p>This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this license, visit <a href=\"https:\/\/creativecommons.org\/licenses\/by\/4.0\/\" target=\"_blank\" rel=\"noopener\">https:\/\/creativecommons.org\/licenses\/by\/4.0\/<\/a><\/p>\n<figure id=\"attachment_5345\" aria-describedby=\"caption-attachment-5345\" style=\"width: 200px\"><img loading=\"lazy\" src=\"https:\/\/zbsa.eu\/wp-content\/uploads\/2021\/04\/zbsa-300x106.png\" alt=\"CCBY\" width=\"200\" height=\"71\" \/><figcaption id=\"caption-attachment-5345\">CCBY<\/figcaption><\/figure>\n<p>\t\t\t\t\t\t\t\t\t\t\t\t<a href=\"\">Content<\/a><\/p>\n<p>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.<\/p>\n<p>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.<\/p>\n<p>\t\t\t\t\t\t\t\t\t\t\t\t<a href=\"\">Basic Information<\/a><\/p>\n<p>This is map version <strong>1.0.<\/strong> 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.<\/p>\n<p>The modern coastline is derived from Natural Earth (<a href=\"https:\/\/www.naturalearthdata.com\" target=\"_blank\" rel=\"noopener\">https:\/\/www.naturalearthdata.com<\/a>), large lakes were added from the \u201cWISE Large rivers and large lakes\u201d dataset provided by the European Environment Agency (<a href=\"https:\/\/www.eea.europa.eu\/data-and-maps\/data\/wise-large-rivers-and-large-lakes\" target=\"_blank\" rel=\"noopener\">https:\/\/www.eea.europa.eu\/data-and-maps\/data\/wise-large-rivers-and-large-lakes<\/a>). Finally the shaded elevation is calculated on the \u201cGEBCO One Minute Grid\u201d from the \u201cGEBCO Gridded bathymetric Data\u201d (<a href=\"https:\/\/www.gebco.net\/\" target=\"_blank\" rel=\"noopener\">https:\/\/www.gebco.net\/<\/a>).<\/p>\n<p>The maps were produced with QGIS 3.<\/p>\n<p>\t\t\t\t\t\t\t\t\t\t\t\t<a href=\"\">Source notes<\/a><\/p>\n<ul>\n<li>Fennoscandian ice sheet data that is not corresponding with Stroeven et al. 2017 was removed and replaced by either water or land areas<\/li>\n<li>The interpolation of the Swedish coastline is approximated on steps between 280 m a.s.l. (most southern part of interpolated area) to 220 m a.s.l. (most northern part of interpolated area)<\/li>\n<li>Sea level for the Adriatic sea was set to -20 m a.s.l. based on sea level curve from Moscon et al. 2015<\/li>\n<li>Sea level for the Black sea was set to -2 m a.s.l. based on sea level curve from Lericolais2017<\/li>\n<li>Minor adjustments were made to smoothen the coastline<\/li>\n<\/ul>\n<p>\t\t\t\t\t\t\t\t\t\t\t\t<a href=\"\">Version history<\/a><\/p>\n<table>\n<tbody>\n<tr>\n<td role=\"textbox\" aria-label=\"Text der Body-Zelle\">09-08-2019<\/td>\n<td role=\"textbox\" aria-label=\"Text der Body-Zelle\">release of Version 1.0.1<\/td>\n<\/tr>\n<tr>\n<td role=\"textbox\" aria-label=\"Text der Body-Zelle\">29-11-2018<\/td>\n<td role=\"textbox\" aria-label=\"Text der Body-Zelle\">1<sup>st<\/sup>\u00a0release of the map<\/td>\n<\/tr>\n<\/tbody>\n<tfoot><\/tfoot>\n<\/table>\n<p>\t\t\t\t\t\t\t\t\t\t\t\t<a href=\"\">Changes to previous version<\/a><\/p>\n<ul>\n<li>Corrected spelling (&#8222;ice sheet&#8220; instead of &#8222;ice shield&#8220;) in release notes and shape files<\/li>\n<\/ul>\n<p>\t\t\t\t\t\t\t\t\t\t\t\t<a href=\"\">References<\/a><\/p>\n<p>Bj\u00f6rck, S. 1995. A review of the history of the Baltic Sea, 13.0-8.0 ka BP. Quaternary International 27, 19\u201340.<\/p>\n<p>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.<\/p>\n<p>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.<\/p>\n<p>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.<\/p>\n<p>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.<\/p>\n<p>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.<\/p>\n<p>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>\n<p>P\u00e5sse, T., Andersson, L., 2005. Shore-level displacement in Fennoscandia calculated from empirical data. Gff 127, 253-268.<\/p>\n<p>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.<\/p>\n<p>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.<\/p>\n<p>Subetto, D., Zobkov, M., Potakhin, M., Tarasov, A., 2017. Paleoreconstructions of Lake Onego. Development in the Late Pleistocene and Holocene.<\/p>\n<p>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.<\/p>\n<p>\u00a0\u00a0\u00a0<\/p>\n<h5>Artikelaktionen<\/h5>\n","comment_info":"No Comments","acf":[],"_links":{"self":[{"href":"https:\/\/zbsa.eu\/en\/wp-json\/wp\/v2\/posts\/5671","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/zbsa.eu\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/zbsa.eu\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/zbsa.eu\/en\/wp-json\/wp\/v2\/users\/3"}],"replies":[{"embeddable":true,"href":"https:\/\/zbsa.eu\/en\/wp-json\/wp\/v2\/comments?post=5671"}],"version-history":[{"count":8,"href":"https:\/\/zbsa.eu\/en\/wp-json\/wp\/v2\/posts\/5671\/revisions"}],"predecessor-version":[{"id":5867,"href":"https:\/\/zbsa.eu\/en\/wp-json\/wp\/v2\/posts\/5671\/revisions\/5867"}],"wp:attachment":[{"href":"https:\/\/zbsa.eu\/en\/wp-json\/wp\/v2\/media?parent=5671"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/zbsa.eu\/en\/wp-json\/wp\/v2\/categories?post=5671"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/zbsa.eu\/en\/wp-json\/wp\/v2\/tags?post=5671"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}