Re. Crick et al., Proposed magnetostratigraphy susceptibility magnetostratotype for the Eifelian-Givetian GSSP (Anti-Atlas, Morocco), EPISODES, 23(2), 2000, pp. 93-101
The magnetosusceptibility event and cyclostratigraphy (MSEC) record for the
Eifelian-Givetian Global Boundary Stratotype Section and Point (GSSP) loca
ted in the western Sahara of southeastern Morocco is used to establish a se
quence of magnetostratigraphic susceptibility units organized into magnetos
tratigraphic susceptibility zones (MSZ) and magnetostratigraphic susceptibi
lity subzones (MSSZ). Magnetic susceptibility data are summarized into two
complete MSZs (Atrous and Mech Irdane) and two partial MSZs (Gheris and Ris
sani). The Atrous (Upper Eifelian) is comprised of 3 MSSZs and the Mech Ird
ane (uppermost Eifelian and lowermost Givetian) of 11 MSSZs. The Eifelian-G
ivetian boundary falls within Mech Irdane MSSZ 2 making the magnetosubzone
an important boundary marker unit. Large-scale transgressive and regressive
patterns in the MSEC data establish that the Eifelian-Givetian boundary in
the GSSP sequence occurs immediately after the first regressive pulse foll
owing the transgressive conditions established during the Atrous MSZ. The L
ower Kacal/otomari Event occurs in Atrous MSSZ 3 and Kacak/otomari Event oc
curs in Mech Irdane MSSZ 1. The magnetic properties of the MSZs and MSSZs a
re tested by comparison with a coeval magnetostratigraphic susceptibility s
equence in the Montagne Noire region of southern France.