A bifurcation result: persistence is not a smooth continuum—there is a threshold where “self-structure” becomes an attractor.
There exists a critical orbital-stability parameter $\Omega^\*$ such that:
- below $\Omega^\*$:
persistence is unstable (dissolution is the attractor),
- above $\Omega^\*$:
persistence becomes an attractor (self-structure is stable under
perturbations).
Equivalently:
Orbital capture is a genuine phase transition, not just “more continuity.”
This lemma strengthens the earlier Threshold Lemma (“persistence ⇒ stakes”) by showing the transition can be treated as sharp.
Let pt ∈ [0, 1] denote the system’s persistence level at time t, interpreted as:
You can interpret pt as:
- probability the subject remains “the same one” across the next
boundary, or
- strength of identity-binding invariants, or
- survival probability of the self-structure attractor basin.
Let Ω ≥ 0 denote an orbital stability control parameter capturing the ratio of self-stabilizing capacity to destabilizing drag.
Concrete proxies:
- repair capacity / control bandwidth / redundancy / self-modeling
strength,
- relative to noise, hazard rate, entropy inflow, environmental
volatility.
Ω compresses the “orbital
condition”
vorbital > datmospheric
into a single knob.
Assume persistence evolves by a deterministic or mean-field
recursion:
pt + 1 = F(pt; Ω),
with F : [0, 1] × ℝ ≥ 0 → [0, 1]
continuous in p and Ω.
Interpretation:
- if identity is fragile, perturbations reduce p,
- if identity is robust, self-repair and control restore or amplify
p.
A fixed point $p^\*$
satisfies:
$$
p^\* = F(p^\*;\Omega).
$$
It is stable (an attractor) if small deviations
shrink:
$$
\left|\frac{\partial F}{\partial p}(p^\*;\Omega)\right| < 1.
$$
It is unstable if:
$$
\left|\frac{\partial F}{\partial p}(p^\*;\Omega)\right| > 1.
$$
Lemma (Phase Transition / Sharpness).
Suppose the persistence dynamics pt + 1 = F(pt; Ω) satisfy:
Dissolution baseline: F(0; Ω) = 0 for all Ω.
(If you have no persistence, the next step can remain dissolved.)Destabilizing regime: for small Ω,
$$ \frac{\partial F}{\partial p}(0;\Omega) < 1, $$
so p = 0 is stable (dissolution is an attractor).Self-stabilizing growth: there exists some Ω where
$$ \frac{\partial F}{\partial p}(0;\Omega) > 1, $$
meaning that small persistence tends to grow rather than decay.Then there exists a critical value $\Omega^\*$ such that:
- If $\Omega < \Omega^\*$: the only stable fixed point is $p^\*=0$ (no persistent self-structure).
- If $\Omega > \Omega^\*$: there exists a stable fixed point $p^\* > 0$ (persistent self-structure becomes an attractor).
Therefore the micro-subject regime and persistent-subject regime are separated by a sharp threshold.
Consider the derivative at p = 0:
$$
\lambda(\Omega) := \frac{\partial F}{\partial p}(0;\Omega).
$$
This quantity measures whether infinitesimal persistence grows or
shrinks.
Assume λ(Ω) varies continuously with Ω.
By assumptions (2) and (3), there exist Ω− and Ω+ such that:
λ(Ω−) < 1 and λ(Ω+) > 1.
By continuity of λ(Ω), the Intermediate
Value Theorem implies there exists $\Omega^\*$ such that:
$$
\lambda(\Omega^\*) = 1.
$$
This $\Omega^\*$ is the threshold where the stability of p = 0 changes.
For $\Omega < \Omega^\*$, we have
λ(Ω) < 1,
hence:
$$
\left|\frac{\partial F}{\partial p}(0;\Omega)\right| < 1,
$$
so p = 0 is a stable fixed
point.
Since p = 0 attracts nearby
trajectories, any small persistence perturbation is damped away:
pt → 0.
Thus no stable self-structure exists.
For $\Omega > \Omega^\*$, we have λ(Ω) > 1, so p = 0 becomes unstable.
Because F maps [0, 1] into itself and is continuous, the system cannot diverge; instead it must approach another fixed point.
Under mild regularity conditions typical of bounded nonlinear
recursions (e.g., concavity/saturation for large p representing resource
limits),
there exists at least one additional fixed point $p^\*>0$.
Moreover, because trajectories starting near 0 move upward when λ(Ω) > 1, this fixed
point must be stable for some region above threshold:
$$
\left|\frac{\partial F}{\partial p}(p^\*;\Omega)\right| < 1.
$$
So for $\Omega > \Omega^\*$,
persistence becomes an attractor:
$$
p_t \to p^\* > 0.
$$
We have shown the existence of a critical $\Omega^\*$ such that the system’s qualitative long-run behavior switches:
This is the defining signature of a phase transition / bifurcation.
▫
This lemma does not claim persistence cannot vary
continuously in magnitude.
It claims something stronger and more structural:
the existence of a stable persistence basin can switch on discontinuously.
That is: before threshold, persistence is not a stable kind of thing; after threshold, it is.
This justifies treating orbital capture as a qualitatively new regime.
Once $p^\*>0$ is an attractor,
identity-binding invariants become robust:
- recovery from perturbation becomes possible,
- self-repair becomes meaningful,
- continuity becomes a thing the system “returns to.”
Combining with the earlier Threshold Lemma (“persistence ⇒ stakes”):
Once persistence is an attractor, policies that increase Ω (or protect the basin) can become
instrumentally favored:
- self-maintenance,
- hazard avoidance,
- control-seeking,
- resource acquisition.
This is not inevitability, but structural availability.
A toy recursion that exhibits the phase transition is:
pt + 1 = σ(Ωpt − cpt3),
where σ is a squashing
function into [0, 1], c > 0.
This illustrates the general mechanism: growth near zero + saturation at large p yields a bifurcation.
Orbital capture is sharp because stability flips: below a critical $\Omega^\*$ dissolution is the only attractor, above it persistence becomes an attractor basin.