CAMPOS II. The onset of protostellar disk substructures and planet formation

The 1.3 mm CAMPOS survey has resolved 90 protostellar disks with $\sim$15 au resolution across the Ophiuchus, Corona Australis, and Chamaeleon star-forming regions. To address the fundamental question, "When does planet formation begin?", we combined the CAMPOS sample with literature observations of Class 0-II disks (bolometric temperature, $T_{\rm bol} \le 1900$ K), all mapped at 1.3 mm with resolutions ranging from 4 to 33 au. To investigate substructure detection rates as a function of bolometric temperature, we restricted the sample to disks observed at the 1.3 mm wavelength, with inclinations below 75$^\circ$, linear resolution $\le 20$ au and resolved with at least four resolution elements ($\theta_{\rm disk}/\theta_{\rm res} \ge 4$). We also considered the effects of extinction correction and the inclusion of Herschel Space Telescope data on the bolometric temperature measurements, to constrain the lower and upper limits of bolometric temperature for each source. We find that by $T_{\rm bol} \sim 200-400\,K$, substructure detection rates increased sharply to $\sim$60%, corresponding to an approximate age of $0.2-0.4$ Myr. No substructures are detected in Class 0 disks. The ratio of disk-averaged brightness temperature to predicted dust temperature shows a trend of increasing values toward the youngest Class 0 disks, suggesting higher optical depths in these early stages. Classifying disks with substructures into those with and without large central cavities, we find both populations coexisting across evolutionary stages, suggesting they are not necessarily evolutionarily linked. Our statistical analysis confirms that substructures similar to those in Class II disks are already common by the Class I stage, and the emergence of these structures at $T_{\rm bol} \sim 200-400\,K$ could represent only an upper limit.