Rapid tectonic and climate changes can
markedly influence lake extent and character, with distinct expression along-
and across-strike. Ghinassi et al.
suggest that although the morphological along-strike variability of lacustrine
coasts is relatively well understood, the nature and signature of this
variability on the sedimentological and stratigraphic record of lacustrine
systems is poorly documented. This study documents how lacustrine water-level
oscillations are recorded in different depositional systems along strike in
late Holocene shoreline deposits of Lake Hayk of Ethiopia. The results
illustrate low-relief margins with fluvial-deltaic systems and high-relief
margins with collvial fan deltas and stromatolitic biostromes. The data reveal
possible pitfalls of classical stratigraphic approaches used to establish
along-strike correlation between lacustrine sedimentary successions, important
for paleoenvironmental studies, subsurface exploration and stratigraphic
investigations.
Lacustrine facies in response to millennial-century scale climate changes (Lake Hayk, northern Ethiopia) by Massimiliano Ghinassi, Filippo D’Oriano, Marco Benvenuti,
Mariaelena Fedi and Stanley Awramik
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