2D Surface Brightness Modelling of Large 2MASS Galaxies II: The Role of Classical Bulges and Pseudobulges on Galaxy Scaling Relations and its implication for Supermassive Black Hole Formation
Emmanuel R\'ios-L\'opez, Omar L\'opez-Cruz, Christopher A\~norve,, Mabel Valerdi, Victoria R. Dufrane, Erick A. Rodr\'iguez-Hern\'andez

TL;DR
This study uses detailed 2D surface brightness modeling of 119 galaxies to analyze the roles of classical bulges and pseudobulges in galaxy scaling relations and black hole formation, revealing differences in their properties and evolutionary implications.
Contribution
It provides a comprehensive analysis of bulge types in galaxy scaling relations using NIR imaging, highlighting the distinct behaviors of classical bulges and pseudobulges and their impact on black hole correlations.
Findings
Classical bulges follow the same scaling relations as ellipticals.
Pseudobulges are often outliers in these relations.
Classical bulges are more luminous than pseudobulges.
Abstract
We have generated 2D-multicomponent surface brightness (SB) modelling for 100 galaxies in the Large Galaxy Atlas (LGA) together with 19 nearby cD galaxies using the near-infrared (NIR) images from 2MASS (J, H and Ks ). Our final sample of 119 galaxies includes cD galaxies, Virgo cluster galaxies, group galaxies, and field galaxies. We revisited known scaling relations (SRs) involving structural parameters, as well as those involving supermassive black holes (SMBHs) and ultramassive black holes (UMBHs). Refining the SRs, we also revisited the bulge classification and considered the Fundamental Plane (FP) and its projections, as well as other SRs, such as the colour-magnitude relation (CMR), Tully-Fisher relation (TFR) and luminosity concentration relation (LCR). Classical bulges follow the same relations as elliptical galaxies, while pseudobulges are usually outliers. The NIR colours of…
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Taxonomy
TopicsAstronomy and Astrophysical Research · Galaxies: Formation, Evolution, Phenomena · Astrophysical Phenomena and Observations
