Primitive extraterrestrial materials record the early evolution of the solar system that predated planet formation. They also preserve the interstellar heritage from prior to the Sun's birth in the form of presolar grains and potentially as isotopic signatures of light elements in organic matter and specific molecules. It is one of the key issues in cosmochemistry to link the birth and evolution of the solar system to the evolution of the interstellar medium (ISM) and the Galaxy. To address this issue, an interdisciplinary approach linking analysis of extraterrestrial materials including samples returned by spacecraft, laboratory experiments, astronomical observations, and theoretical studies is crucial.This special issue arose from a session "Refractory Grains, Volatiles, and Organic Molecules Inherited from the Interstellar Medium" at the Goldschmidt Conference (Aug. 25-30, 2013, Florence Italy) and consists of six articles covering a wide array of topics and disciplines to explore various perspectives of cosmochemistry; astronomical observation, laboratory experiments, extraterrestrial organic chemistry, astrophysical modeling, in-situ isotopic analyses, chronology, and sample-return mission. Dartois et al. (2014) summarize observational and laboratory studies on interstellar carbonaceous dust to explore the link between ISM carbonaceous dust and insoluble organic matter (IOM) found in chondrites and interplanetary dust particles (IDPs). Several forms of carbonaceous solids are observed in the ISM (polyaromatic hydrocarbons (PAHs), amorphous carbons, hydrogenated amorphous carbons (a-C:H), fullerenes, and ices that further turn into macromolecular organic residues after ice-sublimation), among which PAHs, a-C:H and/or macromolecular organic residues would be the main precursor of solar system carbonaceous materials. PAHs and a-C:H are more aromatic and contain less oxygen and nitrogen than solar-system IOM. Organic matter formed by photolysis and/or radiolysis of ice in laboratories do not match the entire infrared spectral features of IOMs either. These lines of evidences indicate that further evolution of organic materials may have occurred in the early stage of solar-system formation from ISM carbonaceous dust as a precursor.The evolution of organic matter in the early solar system may also be recorded in soluble organic components extracted from primitive meteorites. Yamashita and Naraoka (2014) report two homologous series of alkylpyridines (C n H 2n-5 N and C n H 2n-7 N) identified in the methanol extract of the Murchison meteorite by liquid chromatography/high-resolution mass spectrometry. The organic components consisting of C, H, and N are likely to have escaped chemical oxidation during parent body alteration and may thus record the early stage of formation of meteoritic organic components. Laboratory simulation experiments involving HCHO, CH 3 CHO, and NH 3 produced alkylpyridines, which provided a plausible synthetic pathway for meteoritic alkylpyridines via aldol condensation and Chichibabin-typ...