The paper measured sediment organic carbon at 11 coastal and small-island locations in North Minahasa, North Sulawesi, using sediment cores sectioned at 5 cm intervals and loss-on-ignition (LOI) analysis standardized to 1 m depth . Tanah Putih Village had the highest carbon (32.7% C; 132.65 Mg C ha⁻¹) and Paniki Island the lowest (3.45%; 13.87 Mg C ha⁻¹); the authors attribute variation to soil density (0.401–0.414 g/cm³) and depth .
Unit chaos: Results are reported variously as "mgCh⁻¹", "Mg ha⁻¹", and "Mg C ha⁻¹" without reconciliation; per-location values (13.87–132.65) plus a total of 645.19 Mg C ha⁻¹ cannot be verified from the text. Internal contradiction: the text states the findings are "notably higher than" Ngurah Rai values of 83.046–216.168 Mg ha⁻¹, yet the reported range (13.87–132.65) is mostly lower — this comparison appears reversed. Typographical errors: soil density range "0.414 to 401 g/cm³" is garbled; Talise Island appears twice in an inconsistent carbon list. Missing rigor: no sample sizes per site, no replicate counts, no variance or error estimates, no statistical tests for the claimed density–carbon association (which is correlational only, per the evidence record), and no corroboration from δ¹³C or organic source differentiation despite citing such methods in the introduction. For context, peer-ranked mangrove carbon studies report ecosystem stocks of 398–501 ± 42 Mg C/ha in Hawaiian stands and below-ground stocks of 629–687 ± 29 Mg C ha⁻¹ in Vietnam — both with explicit uncertainty, which this paper lacks. Confidence: the descriptive site-level values are probably directionally sound (LOI is a standard method), but the density–carbon causal claim is unsupported and the 645.19 total cannot be independently verified. What would change this assessment: a published erratum with consistent units, per-interval raw data, and a formal correlation test.
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