A&A 457, 891-897 (2006)
DOI: 10.1051/0004-6361:20065434
C. Codella1 - J. Brand2 - F. Massi3 - J. G. A. Wouterloot4 - G. R. Davis4
1 - INAF - Istituto di Radioastronomia, Sezione di Firenze, Largo E. Fermi 5,
50125 Firenze, Italy
2 -
INAF - Istituto di Radioastronomia, via Gobetti 101, 40129 Bologna, Italy
3 -
INAF - Osservatorio Astrofisico di Arcetri, Largo E. Fermi 5,
50125 Firenze, Italy
4 -
Joint Astronomy Centre, 660 N. A'ohoku Place, University Park, Hilo,
HI 96720, USA
Received 13 April 2006 / Accepted 27 June 2006
Abstract
Context. The molecular and continuum surveys at NIR and (sub-)mmwavelengths recently performed in the large and distant (
1 kpc) Bok globules CB3 and CB34 are the framework of the present paper. With this multi-wavelength approach, it is possible to trace the hot jets and cold outflows driven by the (proto-)stars, to investigate how they interact with the surrounding medium, and to assess that in these globules star formation is a continuous process and not a unique event.
Aims. With the present work we continue our survey of a sample of large globules by investigating CB205. The aim is to carefully map the outflow motions and to locate the driving sources. The occurrence of outflows is used to identify the earliest star-forming regions.
Methods. Our analysis has been performed through JCMT observations at (sub)millimeter wavelengths of the continuum (850 and 450
m) and CO(2-1) and (3-2) line emission.
Results. The continuum maps reveal three Class 0 candidates located in the western region of the globule, without NIR counterparts. The line maps show a complex scenario for the high velocity components with different clumps at different velocities. The outflow activity is concentrated around the Class 0 candidates. On the other hand, the NIR objects are associated with lower velocity outflow clumps.
Conclusions. The present results confirm that for CB205, star formation is propagating through the globule. The western part hosts the latest formation episode with Class 0 candidates feeding multiple outflows. We suggest that the eastern region, which is associated with a NIR cluster, reflects a later evolutionary phase, when the outflow is fading.
Key words: stars: formation - radio lines: ISM - ISM: jets and outflows - ISM: molecules - ISM: individual objects: CB205
It is well-known that Bok globules (Bok & Reilly 1947)
are isolated dark molecular clouds closely associated
with star formation (e.g., Clemens & Barvainis 1988;
Bourke et al. 1995; Henning & Launhardt 1998,
and references therein).
Given their simple structure, Bok globules have often been used
to investigate the process of isolated single star formation.
The large majority of such molecular clouds host
low-mass star formation, as confirmed by the low luminosities
estimated for the embedded Young Stellar Objects (YSOs)
in the 1-10
range (e.g., Yun & Clemens
1990; Huard et al. 1999).
A limited number (9,
15%, according to Table 1 of Launhardt &
Henning 1997) of large globules stand out for their relatively large distances
(
1 kpc), their large sizes (
1 pc)
and high masses (>100
), and their association with
intermediate-mass (
10
)
YSOs (Huard et al. 2000).
To understand the nature of the star-forming regions (SFRs) hosted by
the large globules, Huard et al. (2000) observed three of them
(CB3, CB34, and CB205) at 850 and 450
m, detecting the youngest YSOs,
Class 0 sources, which can be recognised by bright submillimeter continuum
emission due to the large amount of surrounding dust.
Huard et al. (2000) suggested that, since sub-mm emission does not
trace the previously detected, more evolved, NIR objects, star formation
within these globules appears to be a continuous process rather than a single event.
Another precious observational tool that allows one to pinpoint Class 0 protostars is the observation of molecular outflows. As soon as a star forms, it generates fast and collimated jets that interact with the surrounding medium and create bipolar molecular outflows when the protostar is still in the main accretion phase (e.g., Bachiller 1996). With this in mind, in order to investigate the youngest stars and compare the characteristics derived from dust and gas emission, we are performing a study of the molecular content of the three large globules observed in the continuum by Huard et al. (2000). As a first step, we performed a survey of the molecular outflows in CB3 and CB34 by observing multi-line emission at mm-wavelengths (Codella & Bachiller 1999; Codella et al. 2002; Codella & Scappini 2003). Our high-angular resolution maps of the CO outflows, first detected by Yun & Clemens (1992, 1994), show that they are located in the region where the millimeter and submillimeter sources are present, offset from the position of the older NIR objects.
Next, we investigated the CB205 globule, also known as L810, which lies
at a distance of 2 kpc (Launhardt & Henning 1997).
IRAS 19433+2743 is embedded in CB205, surrounded by a NIR nebulosity
(Yun et al. 1993). The nebulosity is elongated in the N-S direction
and contains at least 10 stars (Massi et al. 2004).
The sub-mm observations by Huard et al. (2000) show
two sources: SMM1, bright and extended, which coincides with the NIR cluster,
and SMM2, which is fainter and located
44
to the SW, thus
tracing another site of star formation. The maps of Huard et al.
(2000) clearly show a ring-like and clumpy structure that connects
SMM1 and SMM2, and that suggests the possible presence of additional
embedded objects without NIR counterparts.
From CO observations with rather limited resolution
(
45
-48
),
Xie & Goldsmith (1990) and Yun & Clemens (1994) have
detected a single molecular outflow centred on the NIR nebula and with overlapping lobes.
Their maps show that the main axis of the outflow has the same orientation (N-S) as the
NIR nebula, thus suggesting a close connection between
the shape of the nebula, the presence of the outflow, and its driving source.
However, Clemens et al. (1996) showed that the outflow lobes
are offset by about 30
to the West with respect to the IRAS position,
calling for further high angular resolution observations to clarify the outflow morphology.
We have thus investigated CB205 through a survey
in the CO J = 2-1 and 3-2 emission lines. We also performed
submillimeter continuum observations.
The main aims of this work are: (i) to map the outflow at higher angular
resolution and to identify the driving source(s), as was already
done for the other two large globules CB3 and CB34,
and (ii) to use the occurrence of outflows
to identify the youngest YSOs and thus to verify
whether CB205 is associated with different YSOs' generations.
In September 2003, the 450
m and 850
m continuum emissions towards CB205
have been simultaneously observed with the Submillimeter Common-User Bolometer
Array (SCUBA; Holland et al. 1999) mounted on the 15-m James Clerk Maxwell
Telescope (JCMT) at Mauna Kea (Hawaii, USA).
A standard 64-point jiggle map has been made, which covers an area 2
3
in diameter, sampling the region centred at the position of IRAS 19433+2743:
= 19
45
23
8,
= +27
50
57
9.
Calibration has been performed by using water vapour monitor data at 186 GHz,
scaled to give the optical depth at 225 GHz, and average ratios of
(450
m) and
(850
m) to
(225 GHz). The final
transition from instrumental parameters to Jy beam-1 has been derived
from a map of Mars made with the same chopping angle (120
).
Note that at 850
m a few bad bolometers have been blanked
during the data reduction: this affects the
eastern part of the map, producing a sharp decrease in the intensity on one
side of the main peak (see Fig. 1).
To increase the sensitivity of the maps, we have coadded the present
data with those provided by the JCMT archives and published by Huard et al.
(2000). The final rms values are
120 mJy beam-1 at 450
m and
16 mJy beam-1 at 850
m, while
the HPBWs are 10
and 16
,
respectively.
The pointing uncertainty,
2
,
has been estimated by observing
nearby source K3-50.
Maps of the CO J = 2-1 (230.538 GHz) and J = 3-2 (345.796 GHz)
emission were made with the 15-m JCMT during two runs in April and September 2003.
The maps are centred at the IRAS 19433+2743 position, and
the observations were performed in raster mode with
a spacing of 10
for the CO J = 2-1 line,
whereas for the J = 3-2 emission we used a sampling of 8
except
for the central part of CB205, where a smaller value (4
)
has been used. The CO-free reference position was at offset (0
,
-600
).
We used the heterodyne receivers A3 (J = 2-1, HPBW = 21
)
and B3 (J = 3-2, HPBW = 14
).
The backend was the Digital Autocorrelation Spectrometer,
set up with a bandwidth of 500 MHz and a consequent spectral
resolution of 0.41 and 0.27 km s-1 at 231 and 346 GHz, respectively.
The integration time (ON-source) per point for
the J = 2-1 and 3-2 observations was respectively 120 s and 40 s.
The system temperature during the observations
was about 280 K for the A3 receiver and about 690 K
for the B3 receiver. Pointing was checked by observing
W75N and NGC 7538 IRS1, and found to be accurate to within
3
.
The main beam efficiencies adopted to convert the antenna temperature into
brightness temperature are 0.69 (at 230 GHz) and 0.63 (at 346 GHz); the
average sensitivities (1
)
are about 80 and 200 mK, respectively.
![]() |
Figure 1:
850 |
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The possibility that CB205 is hosting an aggregate of YSOs
can be verified using Fig. 1, which shows the dust continuum maps
at 850 and 450
m (present plus Huard et al. 2000 data, see Sect. 2.1).
The observed dust distributions of Fig. 1 obviously reproduce
the images by Huard et al. (2000) showing
a ring-like structure, but in addition the higher sensitivity
allows us to identify two new unresolved sources detected with S/N
10.
These are labeled SMM3 and 4 in Fig. 1.
The brightest source, SMM1, previously detected by Huard et al. (2000), is
extended and associated with the brightest NIR objects, called A and B
by Massi et al. (2004).
The higher angular resolution of the 450
m observations
shows that the extended structure of SMM1 is due to its association
with at least two objects: SMM1a, centred on
the brightest NIR counterparts, and SMM1b, which is
definitely fainter and located
15
in the northern direction.
At 850 and 450
m, we also confirm the occurrence of the
fainter SMM2 source, located
44
SW from SMM1.
The coordinates and the peak flux densities of the four
submillimeter sources are listed in Table 1.
SMM2 and SMM4 have no NIR or optical counterparts, thus they are likely
Class 0 objects. The nature of SMM3 is more uncertain since along its
line-of-sight an optical star (#16; Neckel & Staude 1990)
is visible, but it has no NIR counterpart. Further high-angular resolution
observations at submillimeter wavelengths are needed in order to unambiguosly
classify SMM3.
Table 1: List of coordinates and peak fluxes of the sub-mm objects detected in CB205.
![]() |
Figure 2:
Channel maps of the CO J = 2-1 emission towards CB205. Each panel
shows the emission integrated over a velocity interval of 1 km s-1
centred at the value given in the left corner.
The thick box indicates the ambient velocity range (+15.7 km s-1;
1996). The origin is located at the IRAS 19433+2743 position.
The five filled triangles indicate the locations of the 850 |
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Figure 3:
Channel maps of the CO J = 3-2 emission towards CB205. Each panel
shows the emission integrated over a velocity interval of 1 km s-1centred at the value given in the left corner. Symbols are drawn as in
Fig. 2. The contours range from 0.75 K km s-1 ( |
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An estimate of the total mass of the objects
has been derived from the 850
m total flux using
the standard method (e.g., Huard et al. 1999),
and assuming a dust opacity
=
[
(GHz)/230]
and
= 0.005 cm2 g-1 (Kramer et al. 1998),
implying a gas-to-dust ratio of 100, a dust emissivity index
= 1.3,
and a dust temperature
= 25 K (Huard et al. 2000).
Since SMM2, SMM3, and SMM4 are not resolved,
the total flux has been estimated by using the flux in the beam at these positions.
The masses derived for SMM1=SMM1a+SMM1b, 11
,
and SMM2, 5
,
are
in agreement with those given by Huard et al. (2000).
The masses derived for SMM3 and SMM4, although
they have to be taken with caution,
are
3
.
We used the 450
m total flux integrated
over the HPBW to give a rough estimate
of the SMM1a (
8
)
and SMM1b (
3
)
masses.
The main uncertainties in mass estimates are due to the
assumption of dust temperature: if we assume
in the 20-30 K range
the total mass can vary up to a factor 1.4.
In conclusion, the present continuum observations confirm
that SMM2, already
classified by Huard et al. (2000) as Class 0, does not represent
an isolated case and that the western part
of the globule, away from the NIR cluster, hosts a very young generation
of star formation, probably represented by three Class 0 candidates.
That star formation occurs in the western region of CB205 and
is also supported by the detection of an H2O maser between SMM1 and SMM2
as well as by the occurrence of a secondary peak appearing in NH3(1,1) and
CS(2-1) maps, tracing high-density (
104 cm-3) material
(Neckel et al. 1985; Clemens et al. 1996).
In view of this, SMM2, SMM3, and SMM4 are good candidates
for the driving sources of the outflow motions in CB205, which we shall discuss
next.
In Figs. 2 and 3 we present the channel maps
of the CO(2-1) and (3-2) emissions, respectively.
The ambient LSR velocity is +15.7 km s-1, from the
NH3(1,1) spectra reported by Lemme et al. (1996).
At ambient velocities, we observe an apparent anticorrelation
between the CO emission and the dust continuum maps. This could
be an optical depth effect: CO emission is able to trace just the external part
of the molecular cloud, missing
the high-density interior, and consequently it cannot reproduce the
850
m map. On the other hand, a quite complex scenario emerges for the high-velocity gas,
with several clumps at different velocities. The CO(2-1) maps indicate the
presence of two blue-shifted clumps (hereafter called B1 and B2) and three red-shifted clumps (R1, R2, and R3). In addition, the higher angular resolution CO(3-2) maps, obtained with
a very close spacing (
HPBW/3), allow us to identify a third blue-shifted
clump, called B3. The positions of the clumps are: B1(-10
,
-20
), B2 and
R2(-20
,
+20
), B3(0
,
0
),
R1(-20
,
-20
), and R3(+20
,
-20
).
The clumps B1 and R2 are the only clumps that have been resolved, with a beam-deconvolved size of
20
(
0.25 pc at 2000 pc).
Thus, the single bipolar outflow with large red and blue lobes detected by
Xie & Goldsmith (1990) and Yun & Clemens (1994)
is resolved out into a number of separate outflow lobes here, suggesting a multiple outflow activity.
Figure 4 shows the superposition of the CO(3-2) channel maps at +9.7 and
+17.7 km s-1 giving a summary of the distribution of the red- (dotted
line) and blue-shifted (continuous line) clumps. For the sake of clarity and
to bring out the peak positions of B1 and B2, the contours of the blue
emission are drawn with smaller steps.
Given the high degree of confusion, it is quite risky to
derive outflow geometries and to identify the driving sources.
In fact, the observed outflow lobes could be the result of several overlapping
outflows in the western part of the mm-continuum core of CB205 and, as a consequence,
the driving sources should be looked for among SMM2, SMM3, and SMM4.
However, focusing the attention on the clumps with the highest
velocity detected in the CO(2-1) spectra, observed with a higher
sensitivity, one may note that (i) B2 and R2 are spatially
coincident, and (ii) R1 and B1 are nearly overlapping.
One possible interpretation is that of a single outflow
extending
80
(
0.8 pc at a distance of 2 kpc)
along the NS direction. If the outflow is not highly collimated, and if the
flow axis has a small inclination to the plane of the sky, then the
propagating bow shocks can cause both red- and blue-shifted emission on
the same side of the driving source, thus explaining the overlap of red and
blue lobes seen in Fig. 4. The best candidate for the driving source
in this scenario would be SMM3.
Alternatively, the four lobes with the highest velocities
might be tracing two outflows with their flow axes located roughly along
the line-of-sight; in this case SMM3 could contain the driving YSOs of the northern outflow
(R2, B2), while SMM2 would be the best candidate for the YSO associated with
the southern one (R1, B1). Interferometry, or even single-dish observations of emission from higher
excitation CO transitions would be instructive to resolve possible jet-like
structures and thus help to unravel this situation.
On the eastern side of the dust continuum core, as clearly shown by the higher-sensitivity CO(2-1) data, SMM1a and SMM1b are associated with lower-velocity emission, and in particular with the clumps B3 and R3. The lack of high velocity emission at the SMM1a,b positions could be due to geometrical effects, or it could reflect a different, later evolutionary phase of the driving YSO, when the outflow is fading.
In conclusion, we suggest that the western region of the globule is hosting the main outflow activity and thus the actual star-forming process. The observed high-velocity outflowing gas cannot be the cause of the extended NIR nebulosity, located along the N-S direction and centred on the IRAS point source position. Thus the NIR nebula could eventually be connected with a later phase of outflow activity, as was possibly also indicated by the relatively lower velocity clumps.
Finally, Fig. 5 shows the CO(2-1) and (3-2) spectra observed towards the outflow clumps. The profiles are skewed to the red with respect to the ambient velocity (dashed lines), measured through NH3 emission by Lemme et al. (1996). This is likely to be self-absorption, due to the high opacity expected for the CO emission in combination with a temperature gradient in the core. If we assume that the temperature increases in the central part of the region hosting the YSOs, this suggests that the outer layers of the cloud, as traced by CO, are expanding.
Rotation or the presence of different clumps at different velocities are
unlikely explanations of the profile shapes: the CO channel maps do not show
any dynamical signature of the former, while the spectra outside the
mm-continuum core, at RA and/or Dec offsets
40
,
show symmetric profiles, centred on the
systemic velocity. In addition, Xie & Goldsmith (1990)
show that the 12CO(1-0) spectrum taken at the (0
,
0
) position peaks slightly red-wards with respect to the 13CO(1-0) line, supporting the opacity effect.
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Figure 4:
Summary of the distributions of the blue- (continuous
lines and black labels) and red-shifted (dotted lines and gray labels) clumps.
The map reports the zoom
of the CO(3-2) channel maps at +9.7 and +17.7 km s-1 (see Fig. 3).
To point out the peak positions of B1 and B2, the blue emission is drawn
starting from the 5 |
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By comparing the spectra of two rotational CO lines, J = 2-1 and 3-2 in
this case, it is possible to derive an excitation temperature (e.g.,
Bachiller & Tafalla 1999) and,
since CO is expected to be thermalised, obtain kinetic temperatures.
Given the complex geometry associated with the multiple outflows, two representative positions
in the blue and the red lobes have been considered. Following the CO channel maps, we have chosen the brightest clumps, i.e., B1 and R2. To allow
the spectra to be compared, the different angular resolutions of the two transitions have been taken into account, convolving the J = 3-2 emission
to the HPBW of the 2-1 (21
). The convolved CO(3-2) emission is
weaker by
10%, indicating dilution and confirming that the
high-velocity CO clumps are smaller than the JCMT HPBW at the CO(2-1) frequency. Figure 6 (right panel) shows the behaviour of R32, defined as the ratio between the observed brightness temperatures of the J = 3-2 and 2-1 transitions, as a function of the excitation temperature (
)
in the optically thick (continuous line) and optically
thin (dashed line) regimes. If the CO emission is optically thin and
is the same for both transitions, R32 = 2.25 e
;
for optically thick CO emission,
R32 = 1.5 (e
-1)(e
-1)-1.
In practice, for reasonable values of the temperature, in the thick case
R32 < 1, while in the thin limit the curve tends monotonically to
2.25 when
tends to infinity. The intermediate cases fall in between the two curves. The left panels of Fig. 6 show R32 (black line) as a function of velocity towards the red- (R2 clump; upper panel) and blue-shifted (B1 clump; lower panel) lobes. For reference the CO(3-2) profiles are also shown (not to scale; grey line).
The ratio R32 at the ambient velocity, marked by the grey vertical line,
assumes values of around 0.7-0.8 that can be explained by optically thick
emission at
10-15 K. On either side, R32 decreases
monotonically with velocity to values of around 0.4; this could be due to a variation of the excitation temperature with velocity, or, more reasonably,
it could reflect a thinner emission due to the smaller
amount of gas outflowing at high velocities. If we assume the optically thin
regime at the highest velocities, we derive temperatures around 10 K.
Note that the JCMT archives provide some 13CO(2-1) spectra observed in
1990 around the R3 position. A comparison with the CO(2-1) profiles
indicates that the CO emission at the systemic velocity is optically
thick (
(12CO)
3
(13CO);
> 10). This supports the assumption of the optically
thick regime at these velocities for the B1 and R2 clumps also. Unfortunately,
the 13CO(2-1) spectra do not allow us to derive an opacity estimate at
high velocities.
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Figure 5:
Examples of the CO(2-1) and (3-2) profiles observed towards the
high-velocity clumps located in CB205 and revealed by the channel maps
(Fig. 2). Transition and angular offset are indicated.
Note that B2 and R2 are positionally coincident and that the R2, B2 CO(3-2) spectrum suggests a blue-shifted peak at |
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Figure 6:
The black line shows the intensity ratio
|
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To understand the physics of the outflow gas, we need to estimate
mass, energy, and momentum, which in turn depend on optical depth and
excitation temperature. Given
the complexity of the CB205, we have chosen to sample the whole region
associated with the outflow region. Moreover, we used
the derived excitation temperature (10 K), and we conservatively
assumed an optical depth
in the range 0.1-1.
The standard procedure given, e.g., by Lada (1985) or
Margulis & Lada (1985) has been
used. We integrated the emission in bins of 2 km s-1at each position, taking the difference between the mean velocity
of each bin and the systemic velocity as the outflow velocity. As we are only interested in the
outflowing gas, the central part of the emission line was excluded.
For each bin, we then calculated the CO column densities (
)
and the mass,
assuming a CO to H2 abundance ratio of 10-4. Likewise, we derive
the momentum P
v and the energy E
v2 for each bin. The total mass, momentum, and energy of the outflow are
then derived by summing over all bins and all positions. A dynamical timescale
(age) for the outflow is defined as
,
with R the size of
the flow and V the characteristic outflow velocity. The outflow's mechanical
luminosity is then
,
and the mass loss rate
M =
.
We find a total mass of 2-4
(for
), equally
distributed between the red- and blue-shifted emission,
whereas the momentum
8-12
km s-1.
An average dynamical timescale of about 5
104 yr has been deduced,
from which it follows that
0.08-0.11
,
and
M
(6-8)
yr-1.
The parameters have been derived separately from the
J = 3-2 and 2-1 lines: the estimates are the same only if
(3-2)
(2-1).
This result gives us some indications about the density of the outflowing
gas: by means of statistical-equilibrium calculations and
assuming the derived
= 10 K,
we verified that the constraint on the
optical depths is satisfied when the H2 density
is in the range
103-105 cm-3.
Finally, to estimate the uncertainties introduced
by the lack of geometrical
correction, we have assumed a quite extreme situation, where the flow axis
is close to the plane of sky, with an inclination
i = 20
,
and then we have corrected the outflow velocity
by
.
This leads to P
23-34
km s-1,
,
and M
(16-22)
yr-1, for
.
If we compare the derived outflow properties
with those reported by the literature
(e.g. Cabrit & Bertout 1992; Shepherd & Churchwell 1996)
we can roughly estimate the bolometric luminosity (
)
of the driving YSO(s). In particular, the
-
and the
M-
relationships indicate a driving YSO with
in the range between
10
(no geometrical correction) and
100
(i = 20
)
for the CB205 outflows. The estimates have to be considered upper limits, because we are
observing multiple outflows and multiple YSOs.
Note that close to the SW edge of the globule, a very narrow (1.3 km s-1) spectral component at +20.1 km s-1 appears. Considering its narrowness, it is plausible that rather than an outflowing component, this could simply be due to a quiescent cloud in the foreground or background of CB205. To derive an estimate of the contribution of this spectral component to the outflow parameters derived for the red-shifted emission, we have recalculated the energetics by excluding the spectra of the SW edge of CB205: the conclusion reported above about the YSOs luminosities remains the same, since mass, momentum, luminosity, and mass-loss rate are reduced by a factor between 10% and 20%.
As a first step in investigating the interaction of the outflows
with the ambient medium, we used the JCMT antenna to search for emission
from SiO, which is a standard tracer of shocked gas. We selected the
high-excitation (
= 31 K) J = 5-4 transition at 217.1 GHz
(HPBW = 22
).
The SiO emission has been searched for towards the brightest clumps,
B1 and R2, without success and with an rms of
14 mK. Only through
maps of all outflows in different SiO transitions
will we be able to clarify if this lack of detection is due to an excitation
effect or to a real low SiO abundance.
We have investigated the SFR associated with the large globule CB205 through continuum and molecular line observations at (sub-)millimeter wavelengths. The main findings are:
Acknowledgements
We are grateful to R. Cesaroni for his critical reading of the manuscript. The JCMT is operated by the Joint Astronomy Centre on behalf of the Particle Physics and Astronomy Research Council of the United Kingdom, the Netherlands Organisation for Scientific Research, and the National Research Council of Canada. The data reported in the present paper have been obtained thanks to the M03BI06 and M03AD14 JCMT projects. JCMT archive data were obtained from the Canadian Astronomy Data Netherlands Organisation for Scientific Research Centre, which is operated by the Herzberg Institute of Astrophysics, National Research Council of Canada.