Outside-In Evolution with a Twist: Metallicity Gradients and Asymmetries in the SMC
M. Navabi, R. Carrera, N. E. D. Noël, M. De Leo
TL;DR
Using Ca II triplet spectroscopy of 3,697 SMC red giants, the study derives homogeneous metallicities and constructs a two-dimensional metallicity map. It reveals a global negative radial gradient of $[Fe/H]$ consistent with outside-in evolution, with a tentative positive gradient in the central region suggesting radial migration or central enrichment. Azimuthal variations show flatter gradients in the east/south and steeper ones in the north/west, aligning with tidal effects from the LMC, while eastern distance/velocity bifurcations do not correspond to metallicity differences, implying a common chemical origin. A notable metal-poor population is present in the outskirts, especially to the east, yet depth variations do not drive the main trends, underscoring a complex, interaction-influenced chemical structure for the SMC.
Abstract
Taking advantage of the near-infrared calcium triplet lines, we determine metallicities for a sample of more than 3,500 red giant stars in the field of the Small Magellanic Cloud (SMC). We find a median metallicity of [Fe/H]=-1.05$\pm$0.01 dex with a negative metallicity gradient of -0.064$\pm$0.007 dex deg$^{-1}$ between 1.2°~to 6.0°consistent with an outside-in evolution scenario. For the first time, we detect hints of a positive metallicity gradient within 1.2°, likely reflecting radial migration or centralised chemical enrichment. Azimuthal metallicity asymmetries are detected, with flatter gradients in the eastern and southern quadrants and steeper ones in the north and west. They are consistent with tidal interaction effects from the Large Magellanic Cloud (LMC). Finally, in spite of a clear distance and velocity bifurcations in the east, they seem to share a common chemical origin, in agreement with other studies.
