Correlative use of transmission electron microscopy (TEM) and atom-probe tomography (APT) provides complementary structural and chemical information with a unique combination of atomic-level spatial resolution and single-atom analytical sensitivity [1,2]. Correlated TEM/APT studies are state of the art in material science [3]. In our effort to broaden the application of APT in cosmochemistry [4], we expand our range of projects from meteoritic nanodiamonds [5] and presolar silicon carbide [6,7] to other samples. Here, we present new data from a correlated TEM/APT study of an iron meteorite [8].Iron meteorites are Fe-Ni alloys with minor amounts of Co, P, S, and C. They crystallized with extremely slow cooling rates (0.2 to 6000 K/Ma) within the metallic cores of asteroids during which the characteristic Widmanstätten pattern forms by nucleation and growth of Ni-poor kamacite (α-bcc, ferrite) from taenite (γ-fcc, austenite). The phase transformation occurring below 400˚C involves a eutectoid reaction that results in formation of tetrataenite (FeNi) at the kamacite-taenite (K-T)_interface. The microstructure of the K-T interface and tetrataenite has been studied in detail using TEM [9]. One of our motivations is to take advantage of the superior spatial resolution and sensitivity of APT to study the composition of the K-T region on the nanoscale within fast cooled iron meteorites.We prepared a polished section from the Bristol IVA iron meteorite (Field Museum specimen ME2248),. Bristol cooled at a relatively fast rate (~250 K/Ma; [10]) and experienced comparably low shock pressures (˂13 GPa; [10]). We used a Zeiss EVO 60 SEM equipped with an Oxford AZtec SDD EDS system to image the polished section. A Zeiss 1540 XB FIB-SEM was utilized to prepare sharp nanotips for APT from a 105 µm 2 lamella perpendicular to the K-T interface. The nanotips were attached to a copper half-grid with five presharpened posts. The grid was attached to a tomographic tip, fitted to a tomographic TEM holder (Hummingbird Scientific). TEM analysis was performed using a FEI Tecnai F20ST TEM prior to APT. APT was performed using a Cameca LEAP 4000XSi.The TEM image of a tip (Fig. 1a) shows the presence of a clear interface, which was identified as the kamacite/taenite interface with EDS and electron diffraction. The 3-D tomographic reconstruction (Fig. 1b) shows isoconcentration surfaces for Ni and Co; 3-D surfaces delineating regions with a concentration greater than a given threshold value for each element. The reconstruction shows clearly that Fe-rich (magenta dots) and Ni-rich (green) isoconcentration surface regions are separated by an interface, which represents the K-T interface, also seen in the TEM image (Fig. 1a). In a concentration profile obtained from the atom-probe data perpendicular to the K-T interface, the Fe concentration