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PreprintCC BY 4.0arXiv

Constraining the timescale of activity in Mrk 1018

Abstract

We present analysis of an extended emission line region projected 3.77 kpc from the nucleus of the canonical changing-look AGN Mrk~1018, found in MUSE integral-field observations from the Close AGN Reference Survey. Emission-line ratios show that the region exhibits AGN ionisation but has a very low velocity dispersion, 77 ± 1 kms−1, ruling out an ionised outflow. The lower limit on the light travel time is 12,300 ± 2,300 yr, implying that the nucleus has therefore been active for at least this long. This is much longer than the duration of either observed changing-look transition, which occurred over several years. This implies that Mrk 1018's multi-year variations are occurring within a longer term active phase.

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BibTeX
@misc{mcelroy2026constraining,
  title = {{Constraining the timescale of activity in Mrk 1018}},
  author = {Rebecca McElroy and Scott M. Croom and Thomas Dunn},
  howpublished = {arXiv},
  year = {2026},
  month = nov,
  doi = {10.48550/arxiv.2611.07533},
  eprint = {2611.07533},
  archivePrefix = {arXiv},
  url = {https://arxiv.org/abs/2611.07533},
  note = {CC BY 4.0},
}
RIS
TY  - UNPB
TI  - Constraining the timescale of activity in Mrk 1018
AU  - Rebecca McElroy
AU  - Scott M. Croom
AU  - Thomas Dunn
PY  - 2026
DA  - 2026/11/05
PB  - arXiv
DO  - 10.48550/arxiv.2611.07533
UR  - https://arxiv.org/abs/2611.07533
AB  - We present analysis of an extended emission line region projected 3.77 kpc from the nucleus of the canonical changing-look AGN Mrk~1018, found in MUSE integral-field observations from the Close AGN Reference Survey. Emission-line ratios show that the region exhibits AGN ionisation but has a very low velocity dispersion, 77 ± 1 kms^−1, ruling out an ionised outflow. The lower limit on the light travel time is 12,300 ± 2,300 yr, implying that the nucleus has therefore been active for at least this long. This is much longer than the duration of either observed changing-look transition, which occurred over several years. This implies that Mrk 1018's multi-year variations are occurring within a longer term active phase.
ER  -