WebProvenance of Medieval atlantes in the Ribe Cathedral, Denmark · 17 dant Reinhardtites anthophorus. Hence, our sediments subzone (Fig. 5). The presence of common R. levis and cannot be younger than UC16S2, the last consistent Lucianorhabdus spp., both of which compose a signifi- occurrence of R. anthophorus being within this latter cant part of the … WebOct 1, 2024 · The LO of Micula decussata defines the base of Zone CC14, the LO of Reinhardtites anthophorus marks the base of the Reinhardtites anthophorus Zone …
Biostratigraphic correlation of the transition of Maastrichtian ...
WebReinhardtites anthophorus. Burnett (1998) placed the Coniacian/Santonian boundary within Subzone UC11c, defined as the interval from the FAD of . L. cayeuxii. in the upper Coniacian to the LAD of . Lithastrinus sep-tenarius. in the lower Santonian. Key bioevents noted in this zone include the first appearance datums (in stratigraphic order) of WebMar 7, 2024 · Based on our biostratigraphic data, the Sepidan section is assigned from the late early Santonian (Reinhardtites anthophorus nannofossil Zone/CC15) to the latest … emily and keegan o\u0027donnell conjoined twins
COCCOLITHS AND 1NDE:X FORAMINIFERA FROM THE UPPER …
WebFeb 1, 2024 · Reinhardtites anthophorus (Deflandre, 1959) Perch-Nielsen, 1968. Reinhardtites levis Prins and Sissingh in Sissingh (1977). Retecapsa crenulata (Bramlette … WebKamptnesius magniftcus Deflandre, Broinsonia parca (Stradner), Reinhardtites anthophorus (Deflandre), Lucianoshabdus cayeuri Deflandre. Two biostratigraphic zones: Bsotnsonia parca and Quadsum trifldum have heen distinguished. Fora- minifera were examined in order to make a correlation with the coccolith zones. WebJan 30, 2013 · The following event in the marl of the section is from the first occurrence (Fo) of Q. trifidum (Stradner) Prins and Perch-Nielsen (1977) to the Last occurrences of … dpw number