The Magellanic Puzzle: origin of the periphery
Pol Massana, David L. Nidever, Knut Olsen

TL;DR
This study investigates the metallicity distribution and structural features of the Magellanic Clouds using Gaia DR3 data, revealing new insights into their evolutionary history and the origins of surrounding debris.
Contribution
It provides a detailed analysis of the metallicity gradients and periphery structures of the Magellanic Clouds, challenging previous assumptions about the debris origins.
Findings
Both Clouds have similar radial metallicity gradients with distinct plateaus.
Outer peripheries show consistent metallicities, indicating past interactions.
Magellanic debris is mainly composed of LMC material, not SMC, contrary to prior beliefs.
Abstract
In this paper, we analyse the metallicity structure of the Magellanic Clouds using parameters derived from the Gaia DR3 low-resolution XP spectra, astrometry and photometry. We find that the qualitative behavior of the radial metallicity gradients in the LMC and SMC are quite similar, with both of them having a metallicity plateau at intermediate radii and a second at larger radii. The LMC has a first metallicity plateau at [Fe/H]-0.8 for 37, while the SMC has one at [Fe/H]-1.1 at 35. The outer LMC periphery has a fairly constant metallicity of [Fe/H]-1.0 (1018), while the outer SMC periphery has a value of [Fe/H]-1.3 (610). The sharp drop in metallicity in the LMC at 8 and the marked difference in age distributions in these two regions suggests that there were two important…
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