“…The ESR spectrum (Fig. 4a) of natural marine shell samples consist of many ESR signal but the most distinguishable ones at g x ¼2.0030, g z ¼2.0015 and g y ¼1.9980 are attributed to orthorhombic CO 2 − centers by Schramm and Rossi (1996) and Strzelczak et al (2001). Another observed ESR lines at the low field side of the natural sample spectrum with g ¼2.0056 value associated with isotropic SO 2 − center (Barabas, 1992a;Ikeya, 1993;Schramm and Rossi, 1996;Seletchi and Duliu, 2007).…”