International Ocean Discovery Program (IODP) Site U1513 (33°47.6084′S, 112°29.1338′E) lies at ~2800 m water depth on the western margin of the Mentelle Basin. This Cretaceous basin is probably underlain by synrift Permian to Jurassic sediment that is part of an early rifting event that extends along the western margin of Australia. Following the separation of India from Australia/Antarctica in the Early Cretaceous, the basin underwent a period of rapid thermal subsidence with deposition of deltaic sediment, shale, and claystone sequences, followed by deep-water chalks and limestones. The current seabed is composed of Paleogene/Neogene/Quaternary oozes that sit unconformably on the Cretaceous. Objectives for coring Site U1513 were to obtain a continuous Late Cretaceous sediment record in the Mentelle Basin (adjacent to the Naturaliste Plateau) to better document the rise and fall of the Cretaceous hot greenhouse climate at southern high paleolatitudes (~60°S), characterize how oceanographic conditions changed during the Cenozoic opening of the Tasman Gateway and the restriction of the Indonesian Gateway, and recover breakup-related volcanic rocks from the base of the sedimentary succession to provide age control on the onset and duration of volcanism in the Mentelle Basin. An important goal was to obtain a complete Oceanic Anoxic Event (OAE) 2 sequence across the Cenomanian/Turonian boundary to characterize associated biotic, oceanographic, and climatic changes. The Site U1513 sequence will be compared with coeval Expedition 369 sections cored elsewhere in the Mentelle Basin and at Site U1512 from the Great Australian Bight. The sequence will also be compared with other IODP and industry data from the Western Australia margin and the Great Australian Bight to identify any regional differences in the geochemical and biological responses to the OAEs and Cretaceous and Neogene ocean circulation history. Site U1513 is located 1.1 km east-northeast of Deep Sea Drilling Project (DSDP) Leg 26 Site 258, which was spot-cored (20% recovery) in the Cretaceous section (Luyendyk and Davies, 1975). Site 258 failed to recover samples from the OAE 2 interval and stopped short of penetrating the basalts; however, it did provide valuable information about the lithologies and depths of expected key horizons. The goals at Site U1513 were to complete the gaps of Site 258, to recover a complete sequence of OAE 2, and to recover unaltered samples of the Naturaliste Plateau basalts. Coring in five holes achieved high recovery (80.8%), including a likely sequence from the OAE 2 interval, a nearly complete section of upper Neogene deposits, and samples of altered and possibly unaltered basaltic rocks. Recovered samples will provide new insights on the paleoceanographic evolution during the Cretaceous greenhouse at southern high paleolatitudes, on the timing of breakup of India from Australia/Antarctica, and on the processes of rifting formation and basin subsidence in magma-poor margins.