<documentid="919F4A3AE2EB14015C1AA0357F3645E8"ID-DOI="10.5281/zenodo.13183351"ID-ISSN="2533-4069"ID-Zenodo-Dep="13183351"IM.bibliography_approvedBy="felipe"IM.illustrations_approvedBy="felipe"IM.materialsCitations_approvedBy="felipe"IM.metadata_approvedBy="felipe"IM.taxonomicNames_approvedBy="felipe"IM.treatmentCitations_approvedBy="felipe"IM.treatments_approvedBy="felipe"checkinTime="1722606197785"checkinUser="felipe"docAuthor="Kvaček, Zlatko & Teodoridis, Vasilis"docDate="2011"docId="C64487CCFFD4FF91FECFFCAD340919DD"docLanguage="en"docName="ActaMusNatPraSerB.67.3-4.83-144.pdf"docOrigin="Acta Musei Nationalis Pragae Series B 67 (3 - 4)"docStyle="DocumentStyle:2E5EC822A0C9CE74494687E2DCEF8E0C.4:ActaMusNatPraSerB.2007-2013.journal_article.0cover.type2"docStyleId="2E5EC822A0C9CE74494687E2DCEF8E0C"docStyleName="ActaMusNatPraSerB.2007-2013.journal_article.0cover.type2"docStyleVersion="4"docTitle="Nymphaea polyrhiza SAPORTA"docType="treatment"docVersion="2"lastPageNumber="90"masterDocId="3A7DFFB4FFD3FF96FFC7FF8E356D1C1F"masterDocTitle="The Late Eocene Flora Of Kučlín Near Bílina In North Bohemia Revisited"masterLastPageNumber="144"masterPageNumber="83"pageNumber="90"updateTime="1722656648556"updateUser="ExternalLinkService"zenodo-license-document="CC-BY-NC-ND-3.0">
<mods:affiliationid="EF9E3E7817B0882D86EC0099314B65A9">Institute of Geology and Palaeontology, Faculty of Science, Charles University in Prague, Albertov 6, 128 43 Prague 2, Czech Republic; e-mail: kvacek @ natur. cuni. cz</mods:affiliation>
<mods:affiliationid="7728525FE850B99F1E7D04240C79C309">Department of Biology and Environmental Education Studies, Faculty of Education, Charles University in Prague, M. D. Rettigové 4,116 39 Prague 1, Czech Republic; e-mail: vasilis. teodoridis @ pedf. cuni. cz</mods:affiliation>
<paragraphid="4E5236DAFFD4FF91FF50FBD7378F18AF"blockId="7.[113,748,1113,1200]"pageId="7"pageNumber="90">Rounded to polygonal irregularly shaped traces of attachments of petioles to rhizomes leaving characteristic grouping of rounded variously sized traces on the surface.</paragraph>
is most probable but the remains can hardly characterize individual natural species. Similar petiole outlines with vascular bundle marks have been attributed to
<collectingRegionid="8C29F838FFD4FF91FECDFACC34041946"box="[266,361,1346,1369]"country="United States of America"name="Montana"pageId="7"pageNumber="90">Montana</collectingRegion>
and
<collectingRegionid="8C29F838FFD4FF91FE62FACC34981946"box="[421,501,1346,1369]"country="United States of America"name="Oregon"pageId="7"pageNumber="90">Oregon</collectingRegion>
(
<bibRefCitationid="2A7C4B2BFFD4FF91FDC0FACC37FA1946"author="Becker, H. F."box="[519,663,1346,1369]"pageId="7"pageNumber="90"pagination="1 - 142"refId="ref35609"refString="Becker, H. F. (1969): Fossil plants of the Tertiary Beaverhead Basin in Southwestern Montana. - Palaeontographica B, 127: 1 - 142."type="journal article"year="1969">Becker 1969</bibRefCitation>
;
<bibRefCitationid="2A7C4B2BFFD4FF91FD61FACC34311965"author="Meyer, H. W. & Manchester, S. R."pageId="7"pageNumber="90"pagination="1 - 195"refId="ref42339"refString="Meyer, H. W., Manchester, S. R. (1997): The Oligocene Bridge Creek Flora of the John Day Formation, Oregon. Univ. California Publ. Geol. Sci., 141: 1 - 195."type="journal article"year="1997">
<paragraphid="4E5236DAFFD4FF91FF50FA04378119BE"blockId="7.[113,748,1418,1474]"box="[151,748,1418,1441]"pageId="7"pageNumber="90">M a t e r i a l: BP 55.2345.1, 56.1236.1, NM G 8635,</paragraph>
<paragraphid="4E5236DAFFD4FF91FFB6FA25340919DD"blockId="7.[113,748,1418,1474]"box="[113,356,1451,1474]"pageId="7"pageNumber="90">NM G 8657a, G 4836.</paragraph>