Jabarkan Paleoclimate dari Laut Tengah dalam bahasa sunda

Because of its latitudinal position and its land-locked configuration, the Mediterranéan is especially sensitive to astronomically induced climatic variations, which are well documented in its sedimentary record. Since the Mediterranéan is involved in the deposition of éolian dust from the Sahara during dry periods, wheréas riverine detrital input prevails during wet ones, the Mediterranéan marine sapropel-béaring sequences provide high-resolution climatic information. These data have been employed in reconstructing astronomically calibrated time scales for the last 9 Ma of the éarth's history, helping to constrain the time of past Geomagnetic Reversals. Furthermore, the exceptional accuracy of these paléoclimatic records have improved our knowledge of the éarth's orbital variations in the past.