  We consistently observe a unique pattern in remanence in a number of
canted-antiferromagnets (AFM) and piezomagnets. A part of the remanence is
$\textit{quasi-static}$ in nature and vanishes above a critical magnetic field.
Present work is devoted to exploring this $\textit{quasi-static}$ remanence
($\mu$) in a series of isostructural canted-AFMs and piezomagnets that possess
progressively increasing N\'eel temperature ($T{_N}$). Comprehensive
investigation of remanence as a function of $\textit{magnetic-field}$ and
$\textit{time}$ in CoCO$_{3}$, NiCO$_{3}$ and MnCO$_{3}$ reveals that the
magnitude of $\mu$ increases with decreasing $T{_N}$, but the stability with
time is higher in the samples with higher $T{_N}$. Further to this, all three
carbonates exhibit a universal scaling in $\mu$, which relates to the
concurrent phenomenon of piezomagnetism. Overall, these data not only establish
that the observation of $\textit{quasi-static}$ remanence with
$\textit{counter-intuitive}$ magnetic-field dependence can serve as a
foot-print for spin-canted systems, but also confirms that simple remanence
measurements, using SQUID magnetometry, can provide insights about the extent
of spin canting - a non trivial parameter to determine. In addition, these data
suggest that the functional form of $\mu$ with $\textit{magnetic-field}$ and
$\textit{time}$ may hold key to isolate Dzyaloshinskii Moriya Interaction
driven spin-canted systems from Single Ion Anisotropy driven ones. We also
demonstrate the existence of $\mu$ by tracking specific peaks in neutron
diffraction data, acquired in remnant state in CoCO$_{3}$.
