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(a)
(b)
(c)
(d)
(e)
(f)
(g)
(h)
Fig. 2 Comparison of Terminations I and II based on terrestrial and aquatic proxies from the
Sofular cave in northwestern Anatolia and sediment cores from the southeastern Black Sea: a soil
productivity and vegetation density as estimated from stalagmite
δ
13
C (Fleitmann et al.
2009
);
b arboreal pollen indicating spread of forests in Northern Anatolia (Shumilovskikh et al.
2012
,
2013b
); c
δ
18
O isotopes from Sofular Cave (Badertscher et al.
2011
) and from ostracods/bivalves
in the Black Sea cores 22-GC3/8 (Shumilovskikh et al.
2013a
) and 24-GC3 reflecting changes in
the basins hydrology (arrows) indicate postglacial melt water events (Badertscher et al.
2011
);
d Ca XRF re
ect changes in the carbonate content of the sediment (Shumilovskikh et al.
2012
)
with the Sr/Ca XRF ratio indicating its calcitic or aragonitic composition; e dinocyst concen-
trations indicating Black Sea productivity changes (Shumilovskikh et al.
2012
), and dinocyst
composition re
fl
ecting sea-surface salinity (SSS) (Shumilovskikh et al.
2013a
); f ice-rafted debris
(IRD) suggesting coastal ice formation during extreme winters (Nowaczyk et al.
2012
); g June
insolation at 30
fl
°
N; h global sea level changes (Rohling et al.
2009
)
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