A tale of three tails: A misaligned streamer and mysterious structures around [BHB2007]1
Aashish Gupta, Antonio S. Hales, L. Ilsedore Cleeves, Felipe Alves, Trisha Bhowmik, Nicolás Cuello, Josep M. Girart, Zhi-Yun Li, Anna Miotello, Zhaohuan Zhu, Alice Zurlo
TL;DR
This study uses ALMA Band 6 observations to map CO isotopologues around the YSO [BHB2007]-1, revealing three streamer-like structures (A, B, and C) connected to the disk. While A and B appear unbound despite kinematic ties to the disk, structure C is well described by a gravitationally bound infalling trajectory, suggesting a cloudlet-capture event that can inject mass and angular momentum comparable to the disk itself. Using the TIPSY streamer modeling framework, the authors reconstruct a 3D trajectory for C, estimate its infall time (~1.7 × 10^4 yr), and derive a mass infall rate of ~75 M_Jup Myr^-1, implying potential to double the planet-forming mass budget and tilt the disk by ~69°. The results support a dynamic, environment-driven picture of star and planet formation, where interactions with surrounding clouds can induce disk misalignments and influence planetary system architectures.
Abstract
Recent discoveries of streamer-like structures around protostellar sources challenge the traditional picture of isolated, axisymmetric star formation. Here, we present new ALMA observations of [BHB2007]1, a flat-spectrum source connected to at least three such elongated structures. Two of these features are symmetrically located to the north and south of the disk, with velocities aligned with the disk on their respective sides. However, their unbound kinematics and curved morphology make it difficult to determine their origin. Possible explanations include outflows, interactions with the nearby BHB2 system, and hyperbolic infall, but none fully account for all observed properties. In contrast, a newly identified collimated structure to the west shows clear evidence of gravitationally bound infall. Estimates of its mass, mass infall rate, and angular momentum suggest that this infalling streamer would roughly double the mass budget available to form planets and tilt the disk by a few tens of degrees. Furthermore, its misalignment with the midplane of the disk and the lack of diffuse envelope emission indicate that the streamer may have formed due to gravitational capture of cloud material unrelated to the source's natal core. Together, these findings support a more dynamic picture of star formation, one where environmental interactions continue to shape conditions for building planetary systems.
