<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:creator>Strasser, André</dc:creator>
  <dc:creator>Samankassou, Elias</dc:creator>
  <dc:date>2003</dc:date>
  <dc:description xmlns:ns0="xml" ns0:lang="en">Lagoonal to intertidal sediments from the Holocene in Florida Bay, on the Bahamas,  and in Bermuda are compared to similar facies in the Kimmeridgian and Berriasian of  the Swiss and French Jura Mountains. Dating by 14C permits the estimation of  sediment accumulation rates in the Holocene. In the ancient outcrops, the timing is  given by cyclostratigraphic analysis. Elementary depositional sequences formed in  tune with the 20-ka precession cycle, although much of this time may have been  spent in non-deposition and/or erosion. After decompaction of the ancient sequences,  their accumulation rates can be evaluated. It is suggested that the studied Holocene  sediments accumulated over the past 6000 years with rates of 0.3 to 3 mm/a,  whereas the Kimmeridgian and Berriasian facies show somewhat lower rates of 0.07  to 0.6 mm/a. This difference may be due to metho-dological errors, but also to variable  carbonate production. In shallow carbonate systems, much of the sediment produced  may be redistributed over the platforme or exported. Furthermore, basin morpho-logy  and currents can strongly influence facies and thickness of the accumulated sediment.  Finally, the accumulated sediment may suffer further erosion before it is preserved in  the sedimentary record. Consequently, when estimating sedimentation rates in ancient  sequences, it is important to do this with the highest time resolution possible, and only  after having decompacted the sediment and evaluated the time lost in hiatuses or  condensed intervals.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>https://folia.unifr.ch/global/documents/299547</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/299547/files/1_Strasser_csr.pdf</dc:identifier>
  <dc:language>eng</dc:language>
  <dc:relation>https://hrcak.srce.hr/3784</dc:relation>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>License undefined</dc:rights>
  <dc:source>Geologia Croatica. - 2003, vol. 56, no. 1, p. 1-18</dc:source>
  <dc:subject xmlns:ns1="xml" ns1:lang="en">Shallow-marine carbonates</dc:subject>
  <dc:subject xmlns:ns2="xml" ns2:lang="en">Sedimentation rate</dc:subject>
  <dc:subject xmlns:ns3="xml" ns3:lang="en">Sequence stratigraphy</dc:subject>
  <dc:subject xmlns:ns4="xml" ns4:lang="en">Cyclostratigraphy</dc:subject>
  <dc:subject xmlns:ns5="xml" ns5:lang="en">Holocen</dc:subject>
  <dc:subject xmlns:ns6="xml" ns6:lang="en">Upper Jurassic</dc:subject>
  <dc:subject xmlns:ns7="xml" ns7:lang="en">Lower Cretaceous</dc:subject>
  <dc:subject xmlns:ns8="xml" ns8:lang="en">Florida Bay</dc:subject>
  <dc:subject xmlns:ns9="xml" ns9:lang="en">Bahamas</dc:subject>
  <dc:subject xmlns:ns10="xml" ns10:lang="en">Bermuda</dc:subject>
  <dc:subject xmlns:ns11="xml" ns11:lang="en">Jura Mountains</dc:subject>
  <dc:subject>info:eu-repo/classification/udc/55</dc:subject>
  <dc:title xmlns:ns12="xml" ns12:lang="en">Carbonate Sedimentation Rates Today and in the Past: Holocene of Florida Bay, Bahamas, and Bermuda vs. Upper Jurassic and Lower Cretaceous of the Jura Mountains (Switzerland and France)</dc:title>
  <dc:type>http://purl.org/coar/resource_type/c_6501</dc:type>
</oai_dc:dc>
