In addition, the set of links between coarse sequences and original sequence identifiers and their difference scripts is written to disk in a binary format.
We interpret the basal part of the coarse shelly sequence in SAT 8 (2.82 2.76) to be a deposit of EWE II (cf. KLB 1, chapter 5.1.1); the age control is from an overlying bed (2.72 m b.s). of 3039 2857 cal BP.
The shelf-margin system tract is characterized by a low-stand wedge and land-stand fans that are rich in pebbly sandstone conglomerates and breciated or slumped rudist fragments (especially in the IZ sections, Fig. 4, 4 8) with a Ta Tb-dominated coarse Baume sequence Ta Tb-dominated with deep marine planktonicoarse marl facies.
On top of the lagoonal mud and a former surface, a coarse-grained sequence was found which is thinning landward.
On top of the lagoonal mud, a coarse-grained sequence was found, comprising up to four different subunits (I, II, III, IV).
The Gyra fan consists of a coarse-grained sequence of fully marine origin on top of lagoonal mud and a palaeosol, respectively.
A more detailed look at the XRF measurements of cores LEF 44, 45, 47 and 50, however, reveals several further geochemical characteristics within the coarse-grained sequence.
In all cores from the Gyra fan and the adjacent lagoon, the coarse-grained sequence is covered by greyish or brownish, homogeneous sediments, mainly consisting of clay and silt.
Compared to core LEF 44, this coarse-grained sequence is considerably thinner at coring sites LEF 45 and 50, the latter situated some 200 m to the south in the Lefkada Lagoon (Figs. 3,7).
