Dbk: Created page with "This term was applied by Christensen (1991) to that part of the ''G. quadrata'' Zone in southern England that post-dates the ''A. cretaceus'' Subzone. '''Base''': In southern..."

2013-09-26T13:19:04Z

Created page with "This term was applied by Christensen (1991) to that part of the ''G. quadrata'' Zone in southern England that post-dates the ''A. cretaceus'' Subzone. '''Base''': In southern..."

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This term was applied by Christensen (1991) to that part of the ''G. quadrata'' Zone in southern England that post-dates the ''A. cretaceus'' Subzone.

'''Base''': In southern England, the base of the interval is placed at the Whitecliff Flint (Bailey ''et al''., 1983).

'''Top''': In southern England, the top of the interval is placed at the Farlington Marls (Wood, 1995).

'''Range of index species''': There is no index species, the interval equating with strata between the top of the range of ''Applinocrinus cretaceus'' and the Farlington Marls.

'''Key fauna''':
{| class="Wikitable"
| Bivalvia: || inoceramid shell debris (locally abundant)
|-
| Belemnoidea: ||''Belemnitella mucronata''
|-
| ||''Gonioteuthis quadrata''
|-
| Echinoidea: || ''Echinocorys brydonei''
|}
'''Bio-markers''': There are no bio-markers for the lower part of the interval. At the top of the interval, between the Scratchell's Marls and the Farlington Marls, ''Echinocorys'' ''brydonei'', ''Gonioteuthis'' and ''Belemnitella'' co-occur (Wood, WH/95/31R; Bailey ''et al''., 1983).

'''Age''': Campanian

[[category:Standard zonation | 028]]

Post Applinocrinus beds - Revision history

Dbk: Created page with "This term was applied by Christensen (1991) to that part of the ''G. quadrata'' Zone in southern England that post-dates the ''A. cretaceus'' Subzone. '''Base''': In southern..."