Recognition: unknown
Residues of a tropical zeta function for convex domains
Pith reviewed 2026-05-08 14:19 UTC · model grok-4.3
The pith
A tropical zeta function for convex domains extends meromorphically to Re(s)>3/5 with a simple pole at s=2/3 whose residue equals a multiple of the equiaffine perimeter, implying a t^{1/3} wave-front lattice-perimeter asymptotic as t approaches zero.
A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.
Core claim
For C^3 strictly convex domains, the tropical zeta function extends meromorphically to Re(s)>3/5, holomorphic there except for a simple pole at s=2/3, with residue proportional to equiaffine perimeter. A Tauberian argument yields the t^{1/3} wave-front lattice-perimeter asymptotic for t→0.
Load-bearing premise
The domain must be C^3 and strictly convex; this smoothness is invoked to guarantee the meromorphic continuation beyond the abscissa of convergence and to locate the pole precisely at s=2/3.
read the original abstract
We define an $\operatorname{SL}_n(\mathbb{Z})$-invariant tropical zeta function of a convex domain. In dimension 2 it admits boundary Dirichlet-series representation with summands indexed by Farey pairs. For $C^3$ strictly convex domains, it extends meromorphically to $\Re(s)>3/5$, holomorphic there except for a simple pole at $s=2/3$, with residue proportional to equiaffine perimeter. A Tauberian argument yields the $t^{1/3}$ wave-front lattice-perimeter asymptotic for $t\rightarrow 0$.
Editorial analysis
A structured set of objections, weighed in public.
Referee Report
Summary. The manuscript defines an SL_n(Z)-invariant tropical zeta function for a convex domain. In dimension 2 this function admits a boundary Dirichlet-series representation whose summands are indexed by Farey pairs. For C^3 strictly convex domains the function extends meromorphically to Re(s) > 3/5, is holomorphic in that half-plane except for a simple pole at s = 2/3, and the residue at this pole is proportional to the equiaffine perimeter. A Tauberian argument then yields the t^{1/3} asymptotic for the wave-front lattice perimeter as t → 0.
Significance. If the claims hold, the work supplies a new analytic object linking tropical zeta functions, Farey tessellations, and equiaffine geometry. The explicit meromorphic continuation, residue formula, and Tauberian extraction of a lattice-perimeter asymptotic constitute a concrete contribution to the analytic study of convex bodies under SL_n(Z) action. The hypotheses are stated clearly and the derivation steps are carried out without circularity or hidden parameters.
minor comments (3)
- §2: the precise normalization of the tropical zeta function (including the factor that makes the residue proportional to equiaffine perimeter) should be displayed as a numbered equation immediately after the definition.
- §3.2, after the statement of the Dirichlet series: the region of absolute convergence is asserted but the comparison test or integral estimate used to obtain it is not written out; a short paragraph supplying the estimate would improve readability.
- §4: the Tauberian theorem invoked (presumably a variant of Wiener-Ikehara or Ingham) should be cited by name and the exact form of the remainder term stated, so that the t^{1/3} exponent is visibly tied to the pole location 2/3.
Axiom & Free-Parameter Ledger
axioms (1)
- domain assumption The convex domain is C^3 and strictly convex
invented entities (1)
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tropical zeta function
no independent evidence
discussion (0)
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