On the Reconstruction of Paleosalinities
219
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4
7
0
8
9
10 A
~
~
~ -1
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28
B
Fig. 9. Results for core GeoB 1523-1 vs. age of the core, isotopic stages are numbered at the top, glacials are indicated by light grey, interglacials by white_ (a) &"0 for G. sacculifer, only every second data point of the original
curve (DUrkoop et al. 1997) is shown; (b) temperature estimates for summer and winter calculated by MacMA T;
(c) &" 0 of sea-water as reconstructed from & 18 0 for G. sacculif er and MacMA T summer temperatures; (d) global
& 18 0 W curve (e) Paleosalinity estimates from & 18 0 W (curve a), paleosalinities of curve b employed SIMMAX summer temperature estimates by Hale and Pflaumann (this volume); (I) Annual mean paleosalinity estimates from
MAT; G: Annual mean paleosalinity estimates from ANN.