Environmental changes during the middle to late Norian: An integrated record from the Southern Tethys, Ras Al-Khaimah, United Arab Emirates

The record of environmental and climatic change through the late Norian stage in paleoequatorial settings has so far received limited attention. Here we present new geochemical and sedimentological data to investigate the depositional and environmental changes through the late Norian into the earliest Rhaetian in the marine carbonate Milaha and Ghalilah Formation exposed in Wadi Milaha, Ras Al-Khaimah, UAE. The upper part of the Milaha Formation studied in Wadi Milaha, comprises sediments deposited in a shallow marine environment, with some evidence of high-energy shoal deposition. Restricted conditions are present in the basal and middle part of the Asfal member of the Ghalilah formation, followed by high diversity faunal content, indicating the development of open marine conditions in the late Norian-early Rhaetian. Development of the restricted conditions upwards suggests changes in the relative sea level. Our results show that the succession is comprised of regressive-transgressive cycles, which include minor depositional cycles influenced by changes in clastic input. Sedimentological and elemental data indicate fluctuations in clastic input throughout the sedimentary succession studied. The increase in siliciclastic input coincides with a major regressive sea level cycle during the middle-late Norian. Our results suggest that the increased coarse terrigenous input is likely due to enhanced weathering and an associated warming episode during the late Norian. Very low correlation of δ 13 C carb and δ 18 O indicates little diagenetic influence on the isotopic record. The δ 13 C carb records an overall negative trend during the middle-late Norian with small-scale fluctuations of −2.8‰ magnitude and coincides with increased clastic input. A small positive excursion in δ 13 C carb is recorded at the Norian-Rhaetian boundary. The observed variations in sedimentary succession, relative sea level, and bulk carbonate carbon isotopic record are similar to those of other Tethyan sections. This comprehensive and comparably high-resolution record very likely indicates far-reaching or global ecological changes during the middle-late Norian. • Study area occupied a paleo-equatorial position during the mid-late Norian • Sedimentological investigations allowed the interpretation of sea level cycles • Enhanced siliciclastic input suggest intensification of hydrological cycle • Comparison of the carbon isotope trends suggests ecological changes in late Norian