The Baynunah Formation contains the only known late Miocene terrestrial fossils from the Arabian Peninsula. Based on renewed field work since 2002, we present paleoenvironmental and dietary reconstructions from carbon isotope data from plant wax biomarkers and carbon and oxygen isotope data from fossil tooth enamel in combination with previously published fossil tooth enamel and pedogenic carbonate isotope data. The organic and isotopic data indicate that the highly seasonal ecosystem supported a herbivore community that relied heavily on C4 vegetation. Carbon isotope and molecular abundance data from n-alkanes indicate mostly mixed C3-C4 and C4-dominated ecosystems. Carbon isotope data from fossil teeth indicate a range of C3, mixed C3-C4, and C4 diets, with suids, deinotherids, and rhinocerotids browsing, and bovids, elephantids, and equids mixed feeding to grazing. Hippopotamids show the most positive carbon and most negative oxygen values, with narrow ranges indicating year-round grazing and semi- aquatic habits. The Baynunah sivatheres represent the earliest evidence for a C4-dominanted diet among giraffids. Equid intratooth oxygen isotope profiles indicate a highly seasonal hydroclimate regime, reflecting strong monsoonal conditions with a single rainy season. Corresponding carbon profiles record large seasonal changes in equid diets, with mainly grazing in the wet season and increased browsing in the dry season. Baynunah ecosystems comprised savanna habitats (woody grasslands) with the proboscidean trackway site of Mleisa 1 likely being a seasonally flooded C4 grassland.