CRYPTIC DIAGENETIC CHANGES IN QUATERNARY ARAGONITIC SHELLS: A TEXTURAL, CRYSTALLOGRAPHIC AND TRACE ELEMENT STUDY ON AMIANTIS PURPURATA (BIVALVIA) FROM PATAGONIA, ARGENTINA

MARÍA SOL BAYER; FERNANDO COLOMBO; NATALIA DE VINCENTIS; GONZALO DUARTE; RAUL BOLMARO; SANDRA GORDILLO

PALAIOS

SEPM-SOC SEDIMENTARY GEOLOGY

Lugar: Lawrence; Año: 2013 vol. 28 p. 438 - 451

0883-1351

Modern to Pleistocene Amiantis purpurata shells collected in Bahía San Antonio (Patagonia, Argentina) were studied by X-ray diffraction (XRD), optical and electron microscopy, electron microprobe analyses and microindentation, in order to characterize early diagenetic changes and mechanical resistance. This study minimizes bias by considering the same species from different outcrops of the same region. The sole crystalline phase is twinned aragonite showing pseudohexagonal symmetry. The regularity of the crystallographic texture decreases in older samples, but average crystallite size does not increase. The microstructure, which is dominantly crossed-lamellar, is progressively replaced by a more randomly-oriented grain aggregate. Compositional profiles across the shell show gradients in Sr, Na, S and Cl, whereas Mg and P are more evenly distributed. Each shell layer has a distinct chemical signature. A marked decrease in the concentration of all of these elements, along with flattening of profiles, is evident as age increases. Vickers microhardness is lowest in Modern specimens, showing at the same time the least chipped regions; older shells become harder and more fragile. All of these changes are attributed to post-depositional modifications by dissolution-recrystallization processes mediated by a thin-film of water in a vadose environment. Microstructural adjustments are more sluggish than chemical modifications produced by diagenetic processes, whereas microhardness rapidly reaches high values, probably due to the early degradation of organic compounds from the shell. Our study shows that aragonitic shells which retain their primary mineralogical composition have undergone subtle chemical and microstructural changes. A very small amount of calcite was produced during grinding for XRD. Care should therefore be taken when seeking calcite as evidence of diagenetic changes.