<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>Särkinen T</dc:creator>
  <dc:creator>Kottner S</dc:creator>
  <dc:creator>Stuppy W</dc:creator>
  <dc:creator>Ahmed F</dc:creator>
  <dc:creator>Knapp S</dc:creator>
  <dc:date>2018</dc:date>
  <dc:description xmlns:ns0="xml" ns0:lang="en">PREMISE OF THE STUDY
Fossils provide minimum age estimates for extant lineages. Here we critically evaluate Cantisolanum daturoides Reid &amp; Chandler and two other early putative seed fossils of Solanaceae, an economically important plant family in the Asteridae.


METHODS
Three earliest seed fossil taxa of Solanaceae from the London Clay Formation (Cantisolanum daturoides) and the Poole and Branksome Sand Formations (Solanum arnense Chandler and Solanispermum reniforme Chandler) were studied using x-ray microcomputed tomography (MCT) and scanning electron microscopy (SEM).


KEY RESULTS
The MCT scans of Cantisolanum daturoides revealed a high level of pyrite preservation at the cellular level. Cantisolanum daturoides can be clearly excluded from Solanaceae and has more affinities to the commelinid monocots based on a straight longitudinal axis, a prominent single layer of relatively thin-walled cells in the testa, and a clearly differentiated micropyle surrounded by radially elongated and inwardly curved testal cells. While the MCT scans show no internal preservation in Solanum arnense and Solanispermum reniforme, SEM images show the presence of several characteristics that allow the placement of these taxa at the stem node of Solanaceae.


CONCLUSIONS
Cantisolanum daturoides is likely a member of commelinid monocots and not Solanaceae as previously suggested. The earliest fossil record of Solanaceae is revised to consist of fruit fossil with inflated calyces from the early Eocene of Patagonia (52 Ma) and fossilized seeds from the early to mid-Eocene of Europe (48-46 Ma). The new identity for Cantisolanum daturoides does not alter a late Cretaceous minimum age for commelinids.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>https://sonar.ch/global/documents/18881</dc:identifier>
  <dc:language>eng</dc:language>
  <dc:relation>info:eu-repo/semantics/altIdentifier/doi/10.1002/ajb2.1009</dc:relation>
  <dc:relation>info:eu-repo/semantics/altIdentifier/pmid/29532926</dc:relation>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:source>American journal of botany. - 2018</dc:source>
  <dc:subject xmlns:ns1="xml" ns1:lang="en">
Cantisolanum
</dc:subject>
  <dc:subject xmlns:ns2="xml" ns2:lang="en">
Solanispermum
</dc:subject>
  <dc:subject xmlns:ns3="xml" ns3:lang="en">Commelinales, commelinid monocots</dc:subject>
  <dc:subject xmlns:ns4="xml" ns4:lang="en">London Clay flora</dc:subject>
  <dc:subject xmlns:ns5="xml" ns5:lang="en">Lutetian</dc:subject>
  <dc:subject xmlns:ns6="xml" ns6:lang="en">Ypresian</dc:subject>
  <dc:subject xmlns:ns7="xml" ns7:lang="en">Zingiberales</dc:subject>
  <dc:subject xmlns:ns8="xml" ns8:lang="en">scanning electron microscopy</dc:subject>
  <dc:subject xmlns:ns9="xml" ns9:lang="en">seed fossils</dc:subject>
  <dc:subject xmlns:ns10="xml" ns10:lang="en">x-ray microcomputed tomography</dc:subject>
  <dc:subject xmlns:ns11="xml" ns11:lang="en">Biological Evolution</dc:subject>
  <dc:subject xmlns:ns12="xml" ns12:lang="en">England</dc:subject>
  <dc:subject xmlns:ns13="xml" ns13:lang="en">Fossils</dc:subject>
  <dc:subject xmlns:ns14="xml" ns14:lang="en">Magnoliopsida</dc:subject>
  <dc:subject xmlns:ns15="xml" ns15:lang="en">Microscopy, Electron, Scanning</dc:subject>
  <dc:subject xmlns:ns16="xml" ns16:lang="en">Phylogeny</dc:subject>
  <dc:subject xmlns:ns17="xml" ns17:lang="en">Solanaceae</dc:subject>
  <dc:subject xmlns:ns18="xml" ns18:lang="en">X-Ray Microtomography</dc:subject>
  <dc:title xmlns:ns19="xml" ns19:lang="en">A new commelinid monocot seed fossil from the early Eocene previously identified as Solanaceae.</dc:title>
  <dc:type>http://purl.org/coar/resource_type/c_6501</dc:type>
</oai_dc:dc>
