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Calcareous aeolianite (kurkar) and red loamy paleosol (hamra) units form ridges in the northern coastal plain of Israel. The kurkar ridges with hamra units have been thought to be indicators of past sea levels and of palaeoclimate, though there has been no clear chronology that could correlate units from one ridge to another or to global palaeoclimate and sea level change.We obtained detailed stratigraphy...
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