 
  Aims. We aim to extend our current observational understanding of the integrated planet Earth spectropolarimetry from the optical to the near-infrared wavelengths. Major biomarkers like O2 and water vapor are strong flux absorbents in the Earth’s atmosphere, and some linear polarization of the reflected stellar light is expected to occur at these wavelengths. Methods. Simultaneous optical (0.4−0.9 μm) and near-infrared (0.9−2.3 μm) linear spectropolarimetric data of the earthshine were acquired by observing the nightside of the waxing Moon. The data have sufficient spectral resolution (2.51
            
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![Figure caption: Data of LMC extreme stars are shown as solid, grey circles in the Spitzer color-magnitude diagram ([3.6]-[8.0] vs. [8.0]). The position of the models during the AGB evolution are also shown (where different colors correspond to different s Figure caption: Data of LMC extreme stars are shown as solid, grey circles in the Spitzer color-magnitude diagram ([3.6]-[8.0] vs. [8.0]). The position of the models during the AGB evolution are also shown (where different colors correspond to different s](/sites/default/files/styles/crop_square_2_2_to_320px/public/images/news/resultados131_142.jpg?itok=1coYJ9I3) 
