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This special issue of Journal of Geosciences contains several papers drawing attention to the genetic, spatial and temporal relationships of granitic pegmatites and related granites – one of the paramount problems of granitic pegmatite genesis. Wise and Brown address the granite–pegmatite link at the famous Sebago system, southern Maine, USA. The authors show mineralogical, petrological and geochemical data that suggest that pegmatitic leucogranites are the likely parent to most LCT granitic pegmatites in this region, although another fertile granite–pegmatite system may be responsible for some anomalous pegmatite dikes showing NYF affinity. Swanson and Veal describe relationships between pegmatites and host granitoids in the high-pressure (0.7–1.1 GPa) Spruce Pine district, North Carolina, USA. They focus on the textural transition from granitoids to pegmatites and argue that the transition was controlled mainly by different nucleation rates as related to water content of the melts. Colombo et al. focus on mineralogy and crystal chemistry of micas from the A-type El Portezuelo granite and related miarolitic pegmatites at Catamarca, northwestern Argentina. The micas (biotite, muscovite, zinnwaldite) exhibit compositional evolution characteristic of NYF-type granite– miarolitic pegmatite systems. Beal and Lentz present detailed mineralogical and isotopic study of aquamarine beryl in A-type pegmatite–aplite dykes and associated quartz veins and greisen at the Zealand Station Be–Mo deposit, New Brunswick, Canada. High δ18O values of quartz and beryl indicate a considerable crustal component to the magmas and low δD values of the channel water in beryl reflect crystallization from a volatile-undersaturated magmatic source before pegmatite dyke emplacement. Uher et al. describe primary and secondary compositional trends in beryl in LCT pegmatites of the beryl–columbite subtype in western Carpathians, Slovakia. In the primary trend, Cs, Cs/Na, Mg and Mg/Fe decrease in most beryl crystals from less evolved to more fractionated pegmatites. In the secondary trend, there is decreasing Cs and increasing Mg/Fe that may represent a late replacement. These contributions demonstrate the complexity of granite–pegmatite links through mineralogical, geochemical and isotopic data and field relationships. The papers enhance our understanding of the processes that lead to the links.

Foreword to the special volume on "Mineralogical, geochemical and isotopic links between granitic pegmatites and their parental granites"