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              <p>The Proto-Paratethys, a shallow epicontinental sea, extended from Cretaceous to Paleogene times across Eurasiafrom the Mediterranean Tethys to the Tarim Basin in western China. Transgressive and regressive episodes ofthe Proto-Paratethys Sea have been previously recognized but their timing, extent and depositional environmentsremain poorly constrained especially for the Cretaceous and early Paleogene. This hampers understanding of theirdriving mechanisms (geodynamic and/or eustatic) and paleoclimatic consequences on regional aridification andmonsoons.As part of the ERC “MAGIC” project, we report an integrated sedimentologic and stratigraphic analysis of theProto-Paratethys from its initial Cretaceous onset to the final Paleogene retreat from multiple investigated sectionsin the western border of Tarim Basin. Facies associations include field observations and microfacies analyses fromcarbonate samples. New bio- and magneto-stratigraphic results from key intervals are also provided to testify thepreviously constructed regional stratigraphic framework.The previously controversial number of marine incursions in the Tarim Basin is resolved to 6 (3 Cretaceous and 3Paleogene) also recognized in the neighboring Tajik and Turan Basins to the west and the present-day Alai Valley.The eastward extent of these marine incursions varied through time with a maximum extent during late Paleocene- early Eocene. The first marine incursion is a Cenomanian transgression recorded in the marls and calcareousmudstones of the Kukebai Formation. The next two are Coniacian and Campanian transgressions recognized inthe carbonate units of the Yigeziya Formation. The first Paleogene incursion is characterized by thick evaporitesof  the  Paleocene  Aertashi  Formation  overlain  by  the  marine  shales  of  the  Lower  Qimugen  Formation.  Thelatter represents the maximum extent and the deepest environments of the Proto-Paratethys. The marine Kalatarlimestones and silty shales of the Wulagen Formation are associated with the penultimate transgression whereasthe silty shales of the Bashibulake Formation were laid down during the last smaller marine incursion.Generally,  transgressive  intervals  are  composed  of  restricted  marine  bay  environments,  shoal  &amp;  oyster-richbioherms giving rise to upper offshore to shoreface transition silty shales. The regressive intervals are composed ofintertidal flats, supratidal sabkhas and salinas, fluvial, playa and lake environments of alluvial plain. The temporaland spatial extent of the transgressive and regressive intervals enable to discriminate the major drivers of marinefluctuations with their potential consequences on Asian aridification and monsoons.</p>
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