Sedimentary and diagenetic markers of the restriction in a marine basin: the Lorca Basin (SE Spain) during the Messinian

The Lorca Basin (southeastern Spain) is part of a chain of small marginal N eogene basins located in the structurally active Betic area. The Upper Mioc ene (Messinian) sequence is composed of a thick diatomite-bearing series (T ripoli Unit) overlain by the Main Evaporites, analogous to the classical su ccession that records the main events during the Salinity Crisis in the Med iterranean region. The shallow restricted conditions of this region amplifi ed the sedimentary responses to local and global forcings. An integrated ap proach using sedimentology, micropalaeontology, stable isotope geochemistry and organic geochemistry has been applied to the Tortonian/Messinian succe ssion of the Lorca Basin, in order to obtain a continuous record of the env ironmental changes. The sediments record two major events which affected th e whole Mediterranean: (1) high levels of productivity that led to the form ation of the diatomite-bearing deposits in the early Messinian (Tripoli); a nd (2) the Messinian Salinity Crisis with its two major stages, represented by the Halite and Gypsum Units, both mainly precipitated from marine-deriv ed brines. The rapid reflooding of the Mediterranean by normal marine water s at the base of the Pliocene did not reach the Lorca Basin, nor other basi ns of this part of the Betic area. Instead, continental sediments were depo sited as a consequence of the regional uplift of SE Iberia, which started c lose to the Messinian/Pliocene boundary. The most prominent feature of this basin concerns the record of its restriction by the time of the deposition of the Tripoli Unit, which led to intercalations of precursor evaporitic l ayers, consisting of Ca-sulphate deposited in sub-aqueous and sabkha condit ions, interbedded with diatomites. This alternation of evaporites and diato mites proves that the Lorca Basin was periodically restricted and reflooded by marine waters, a possible cause for this being relative sea-level fluct uations in the Mediterranean. This strengthens evidence of diachronism that suggests that the onset of the first Messinian evaporitic deposition was n ot synchronous, but was dependent on bathymetry and local tectonics. High p roductivity during the early Messinian in this basin is demonstrated by the thick deposits of diatomites. However, stagnation episodes may have occurr ed during this interval, as suggested by the preservation of high amounts o f organic matter (organic-rich shales) and the extent of bacterial sulphate reduction which apparently occurred during early diagenesis. The formation of organo-sulphur compounds, replacement of sulphates by carbonates and th e high levels of elemental sulphur are by-products of diagenetic processes occurring in a restricted hypersaline environment. (C) 1998 Elsevier Scienc e B.V. All rights reserved.