Dabrio, Cristino JoséPolo, María Dolores2017-04-042017-04-041995http://hdl.handle.net/10272/13548A brief description of detail stratigraphy of the Late-Neogene Terminal Carbonate Complex and the Sorbas Member, and the precise role of the stromatolite layers that occur interbedded. The vicinity to the sources of coarse-gained sediment input, mobility of the sea-bottom, and the topographic elevation reached by the sea during high stands of4th/5th order oscillations control the development of stromatolites. Recognition of high-frequency (fourth and fifth-order cycles) inside a third-order (TB 3.4)'eustatic cyclespaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Mixed shelfFringing reefsStromatolitesTalus slopeEustatic oscillationsLate NeogeneSouth-eastern Spainjournal articleopen access