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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Erika Gobet</dc:contributor>
  <dc:contributor>Christoph Schworer</dc:contributor>
  <dc:contributor>Giorgia Beffa</dc:contributor>
  <dc:contributor>Christoph Butz</dc:contributor>
  <dc:contributor>Paul D. Henne</dc:contributor>
  <dc:contributor>Cesar Morales-Molino</dc:contributor>
  <dc:contributor>Salvatore Pasta</dc:contributor>
  <dc:contributor>Jacqueline Van Leeuwen</dc:contributor>
  <dc:contributor>Hendrik Vogel</dc:contributor>
  <dc:contributor>Elias Zwimpfer</dc:contributor>
  <dc:contributor>Flavio Anselmetti</dc:contributor>
  <dc:contributor>Martin Grosjean</dc:contributor>
  <dc:contributor>Willy Tinner</dc:contributor>
  <dc:creator>Tiziana Pedrotta</dc:creator>
  <dc:date>2021</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Knowledge about the vegetation history of Sardinia, the second largest island of the Mediterranean, is scanty. Here, we present a new sedimentary record covering the past ~ 8,000&amp;nbsp;years from Lago di Baratz, north-west Sardinia. Vegetation and fire history are reconstructed by pollen, spores, macrofossils and charcoal analyses and environmental dynamics by high-resolution element geochemistry together with pigment analyses. During the period 8,100–7,500&amp;nbsp;cal&amp;nbsp;&lt;/span&gt;&lt;span class="u-small-caps"&gt;BP&lt;/span&gt;&lt;span&gt;, when seasonality was high and fire and erosion were frequent,&amp;nbsp;&lt;/span&gt;&lt;i&gt;Erica arborea&lt;/i&gt;&lt;span&gt;&amp;nbsp;and&amp;nbsp;&lt;/span&gt;&lt;i&gt;E. scoparia&lt;/i&gt;&lt;span&gt;&amp;nbsp;woodlands dominated the coastal landscape. Subsequently, between 7,500 and 5,500&amp;nbsp;cal&amp;nbsp;&lt;/span&gt;&lt;span class="u-small-caps"&gt;BP&lt;/span&gt;&lt;span&gt;, seasonality gradually declined and thermo-mediterranean woodlands with&amp;nbsp;&lt;/span&gt;&lt;i&gt;Pistacia&lt;/i&gt;&lt;span&gt;&amp;nbsp;and&amp;nbsp;&lt;/span&gt;&lt;i&gt;Quercus ilex&lt;/i&gt;&lt;span&gt;&amp;nbsp;partially replaced&amp;nbsp;&lt;/span&gt;&lt;i&gt;Erica&lt;/i&gt;&lt;span&gt;&amp;nbsp;communities under diminished incidence of fire. After 5,500&amp;nbsp;cal&amp;nbsp;&lt;/span&gt;&lt;span class="u-small-caps"&gt;BP&lt;/span&gt;&lt;span&gt;, evergreen oak forests expanded markedly, erosion declined and lake levels increased, likely in response to increasing (summer) moisture availability. Increased anthropogenic fire disturbance triggered shrubland expansions (e.g.&amp;nbsp;&lt;/span&gt;&lt;i&gt;Tamarix&lt;/i&gt;&lt;span&gt;&amp;nbsp;and&amp;nbsp;&lt;/span&gt;&lt;i&gt;Pistacia&lt;/i&gt;&lt;span&gt;) around 5,000–4,500&amp;nbsp;cal&amp;nbsp;&lt;/span&gt;&lt;span class="u-small-caps"&gt;BP&lt;/span&gt;&lt;span&gt;. Subsequently around 4,000–3,500&amp;nbsp;cal&amp;nbsp;&lt;/span&gt;&lt;span class="u-small-caps"&gt;BP&lt;/span&gt;&lt;span&gt;&amp;nbsp;evergreen oak-olive forests expanded massively when fire activity declined and lake productivity and anoxia reached Holocene maxima. Land-use activities during the past 4,000&amp;nbsp;years (since the Bronze Age) gradually disrupted coastal forests, but relict stands persisted under rather stable environmental conditions until ca. 200&amp;nbsp;cal&amp;nbsp;&lt;/span&gt;&lt;span class="u-small-caps"&gt;BP&lt;/span&gt;&lt;span&gt;, when agricultural activities intensified and&amp;nbsp;&lt;/span&gt;&lt;i&gt;Pinus&lt;/i&gt;&lt;span&gt;&amp;nbsp;and&amp;nbsp;&lt;/span&gt;&lt;i&gt;Eucalyptus&lt;/i&gt;&lt;span&gt;&amp;nbsp;were planted to stabilize the sand dunes. Pervasive prehistoric land-use activities since at least the Bronze Age Nuraghi period included the cultivation of&amp;nbsp;&lt;/span&gt;&lt;i&gt;Prunus&lt;/i&gt;&lt;span&gt;,&amp;nbsp;&lt;/span&gt;&lt;i&gt;Olea europaea&lt;/i&gt;&lt;span&gt;&amp;nbsp;and&amp;nbsp;&lt;/span&gt;&lt;i&gt;Juglans regia&lt;/i&gt;&lt;span&gt;&amp;nbsp;after 3,500–3,300&amp;nbsp;cal&amp;nbsp;&lt;/span&gt;&lt;span class="u-small-caps"&gt;BP&lt;/span&gt;&lt;span&gt;, and&amp;nbsp;&lt;/span&gt;&lt;i&gt;Quercus suber&lt;/i&gt;&lt;span&gt;&amp;nbsp;after 2,500&amp;nbsp;cal&amp;nbsp;&lt;/span&gt;&lt;span class="u-small-caps"&gt;BP&lt;/span&gt;&lt;span&gt;. We conclude that restoring less flammable native&amp;nbsp;&lt;/span&gt;&lt;i&gt;Q. ilex&lt;/i&gt;&lt;span&gt;&amp;nbsp;and&amp;nbsp;&lt;/span&gt;&lt;i&gt;O. europaea&lt;/i&gt;&lt;span&gt;&amp;nbsp;forest communities would markedly reduce fire risk and erodibility compared to recent forest plantations with flammable non-native trees (e.g.&amp;nbsp;&lt;/span&gt;&lt;i&gt;Pinus&lt;/i&gt;&lt;span&gt;,&amp;nbsp;&lt;/span&gt;&lt;i&gt;Eucalyptus&lt;/i&gt;&lt;span&gt;) and xerophytic shrubland (e.g.&amp;nbsp;&lt;/span&gt;&lt;i&gt;Cistus&lt;/i&gt;&lt;span&gt;,&amp;nbsp;&lt;/span&gt;&lt;i&gt;Erica&lt;/i&gt;&lt;span&gt;).&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1007/s00334-021-00832-3</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Springer</dc:publisher>
  <dc:title>8,000 years of climate, vegetation, fire and land-use dynamics in the thermo-mediterranean vegetation belt of northern Sardinia (Italy)</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>