Late Pleistocene – Holocene environmental changes – records from submerged speleothems along the Eastern Adriatic coast (Croatia)

• Main Authors: Maša Surić, Mladen Juračić
• Format: Article
• Language: English
• Published: Croatian Geological Survey 2010-06-01
• Series: Geologia Croatica
• Subjects: Palaeoenvironment; Late Pleistocene-Holocene; U-Th dating; 14C dating; sea-level change; submerged speleothems; Adriatic Sea; Croatia
• Online Access: http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/112

<p class="MsoBodyText" style="margin: 0cm 0cm 0pt; text-indent: 35.4pt; line-height: 200%; mso-outline-level: 1;"><span style="font-family: Times New Roman;"><span style="font-size: 12pt; line-height: 200%;" lang="EN-GB">U-Th and ¹⁴C dating, and X-ray diffraction of the parts of 16 submerged speleothems taken from the depths of 1.5&minus;41.5 m from 7 submarine caves and pits along the Eastern Adriatic coast, provided insight to the sea-level fluctuations during the last 220 ka and to the palaeogeographic changes caused by sea-level changes. Due to the climate changes, palaeoenvironmental settings also varied, but not so abrupt and intensive as in the rest of </span><span style="font-size: 12pt; line-height: 200%;" lang="EN-GB">Europe</span><span style="font-size: 12pt; line-height: 200%;" lang="EN-GB">.<span style="color: red;"> </span>Namely, owing to the </span><span style="font-size: 12pt; line-height: 200%;" lang="EN-GB">Alps</span><span style="font-size: 12pt; line-height: 200%;" lang="EN-GB"> and Dinarides acting as orographic barriers, </span><span style="font-size: 12pt; line-height: 200%;" lang="EN-GB">Eastern Adriatic</span><span style="font-size: 12pt; line-height: 200%;" lang="EN-GB"> coast was the border region between periglacial </span><span style="font-size: 12pt; line-height: 200%;" lang="EN-GB">Europe</span><span style="font-size: 12pt; line-height: 200%;" lang="EN-GB"> and temperate Mediterranean region. It was, also, refuge area for plant species from the north. This study showed that appropriate temperature, humidity and vegetation cover ensured favourable conditions for karstification and speleothems formation processes even during Last Glacial Maximum.</span></span></p>