The most important factor controlling the timing of Phanerozoic mineralogical evolution in the Bivalvia appears to be thermal potentiation of calcite deposition in colder marine and estuarine environments. Cold temperature has promoted mineralogical evolution in the Bivalvia by kinetically facilitating (potentiating) initially weak biological controls for calcite, thereby exposing their genetic basis to natural selection. Calcite has evolved in bivalve shells for a variety of selective advantages, including resistance to dissolution; resistance to chemical boring by algae and gastropods; reduced shell density in swimming and soft-bottom reclining species; enhanced flexibility in simple prismatic shell layers; and fracture localization and economy of secretion in association with certain foliated structures.Endogenous calcite in bivalve shells varies from biologically induced to weakly and strongly biologically controlled. Biologically controlled calcite generally first appears in bivalve shells as an impersistent component of the outer shell layer, only later, in some groups, expanding to include the entire outer and then part or all of the middle and inner shell layers. The initial stages of mineralogical evolution are shown by certain modern Mytilidae, Veneridae and Petricolidae. In the latter two families, the calcite occurs as conellae in the outer part of the outer shell layer. Calcitic conellae in the inner shell layer of Pliocene Mercenaria are not barnacle plates, as previously indicated, but endogenous calcite comparable in origin to other venerid conellae. Their occurrence in Mercenaria may reflect thermal potentiation of weak biological controls for calcite, as well as local detachment of the secretory mantle epithelium near the pallial and adductor musculature.

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Collisionally activated dissociation of deprotonated aromatic sulfonic acids in the gas phase causes rearrangement and fragmentation to produce the corresponding phenoxide ions. The mechanism for this reaction has been investigated and the results of this study favor initial intramolecular nucleophilic addition of a sulfonate oxygen atom to the aromatic ring, a process which is followed by heterolytic cleavage of the carbonsulfur bond to rearomatize the ring. The product from this addition4imination sequence is the anion of a sulfurous acid halfester, which loses SO, to generate the corresponding phenoxide ion. 2 R = SOJH 3 R = SO,H

Neotrigonia (Molluscs, Pelecypoda). the only surviving genus of the once diverse and widespread Trigoniacea, was collected live from depths of 6–80 m on sandy mud bottoms off southeastern Australia. The two species collected. Neotrigonia gemma Iredale, 1924 and Neotrigonia margaritacea (Lamarck), 1804, are structurally similar and differ mainly in size and coloration. Neotrigonia has such primitive features as an unfused mantle and filibranchiate ctenidia. Its foot is large, active and muscular and the ctenidial ciliary pattern resembles that of the Unionacea. The shell is non‐streamlined and has pronounced radial omamentation. Neotrigonia lives infaunally near the sediment surface, filter feeds. and is capable of fairly rapid burrowing. The burrowing facility, conferred by the foot, is unexpected in light of shell morphology. This suggests that shell morphology alone is not necessarily a reliable guide to the life habits of fossil trigoniaceans.