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Table 4

Line measurements for the stacking detection shown in Fig. 7, based on the red (v> −300 km s-1) velocities of both regions (excluding the M31-I (3) detection and M31-2c-a(1) tentative 13CO(2–1) detection).

Pos. V Stack V0 (km s-1) Δv (km s-1) TPeak (mK) Iline (K km s-1)

13CO C18O 13CO C18O 13CO C18O 13CO C18O
(2–1) (2–1) (2–1) (2–1) (2–1) (2–1) (2–1) (2–1)

Stack (red) –144.2 –212 –212 50* 50* 1.65 0.95 0.088 ± 0.015 0.051 ± 0.015
31 0.15 ± 0.03
SE stack (red) –226. –218. –218. 39* 39* 2.26 1.28 0.094 ± 0.015 0.053 ± 0.015
39 0.14 ± 0.04

Pos. V Stack V0 (km s-1) Δv (km s-1) TPeak (mK) Iline (K km s-1)

HCO+ HCN HCO+ HCN HCO+ HCN HCO+ HCN
(1–0) (1–0) (1–0) (1–0) (1–0) (1–0) (1–0) (1–0)

SE Stack (blue) –523 –524.5 89 89 ± 25 1.17 < 0.075 0.11 ± 0.03
SE Stack (red) –234 –231 –231 78 ± 29 78 0.74 0.85 0.061 ± 0.026 0.070 ± 0.024

Notes. We present the central velocities, velocity dispersions, peak temperatures, and integrated lines. V0 is the averaged velocity of the spectra used for each stacking. Similar stacking based on the 12CO(2–1) velocities is performed for HCN and HCO+ spectra of the south-east (SE) positions. As shown in Fig. A.2, redshifted (blueshifted) velocities are considered separately.

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