The origin and evolution of solar system bodies, including water on the Earth, have been discussed based on the assumption that the relevant ingredients were simply silicates and ices. However, large amounts of organic matter have been found in cometary and interplanetary dust, which are recognized as remnants of interstellar/precometary grains. Precometary organic matter may therefore be a potential source of water; however, to date, there have been no experimental investigations into this possibility. Here, we experimentally demonstrate that abundant water and oil are formed via the heating of a precometary-organic-matter analog under conditions appropriate for the parent bodies of meteorites inside the snow line. This implies that H2O ice is not required as the sole source of water on planetary bodies inside the snow line. Further, we can explain the change in the oxidation state of the Earth from an initially reduced state to a final oxidized state. Our study also suggests that petroleum was present in the asteroids and is present in icy satellites and dwarf planets.

Many macromolecular antitumor drugs were developed based on the enhanced permeability and retention (EPR) effect, for example, albumin-bound paclitaxel nanoparticles (nab-PTX and Abraxane) and pegylated liposomal doxorubicin (Doxil). However, these EPR effect-based therapeutic systems are less effective in malignant tumors with low vascular permeability, such as pancreatic tumors. Because the EPR effect depends on nanoparticles’ size, we first determined nanoparticles’ size associated with a high tumor-targeting rate in a human pancreatic tumor xenograft model with low vascular permeability. Abraxane appears to behave as an albumin monomer (7 nm) in the blood circulation following intravenous injection. The in vitro and in vivo tumor-targeted delivery and antitumor activity of PTX-loaded albumin nanoparticles were significantly improved by optimizing the mean nanoparticle diameter to 30 nm. Furthermore, nitric oxide was added to 30 nm PTX-loaded albumin nanoparticles to examine the feasibility of albumin nanoparticles as a platform for multiple drug delivery. Their antitumor effect was evaluated in an orthotopic transplantation mouse model of a human pancreatic tumor. The nitric oxide PTX-loaded 30 nm albumin nanoparticle treatment on model mice achieved a significantly higher survival rate than Abraxane treatment. These findings suggest that 30 nm albumin nanoparticles have a high therapeutic effect as a useful platform for multiple drugs against human pancreatic tumors.

Early evolution of Solar System small bodies proceeded through interactions of mineral and water. Melting of water ice accreted with mineral particles to the parent body results in the formation of secondary minerals, the so-called aqueous alteration. Formation of phyllosilicates from anhydrous silicates is a typical alteration effect recorded in primitive meteorites. In addition to mineral and water, organic matter could have been also a significant component in meteorite parent bodies. However, the role of organic matter in the alteration of silicates is not well understood. We conducted a heating experiment of anhydrous silicate (olivine) with a mixture of organic compounds which simulated primordial organic matter in the Solar System. Dissolution and precipitation features were confirmed on the olivine surface after heating at 300 °C for 10 days, and proto-phyllosilicates were formed in the precipitation area. Magnesite was also detected as concomitant mineral phase. These minerals could be the evidence of aqueous alteration and carbonation of olivine induced by water generated through decomposition of the organic compounds with hydroxy groups. Our result showed that the in situ formation of hydrated silicates through a mineral–organic interaction without the initial presence of water. It further implies that formation of phyllosilicates on the olivine surface in contact with organic matter can occur in meteorite parent bodies which formed inside the H2O snow line but accreted with organic matter, initially without water. Water formed through decomposition of organic matter could be one candidate for hydrous silicate formation, for example, in ordinary chondrites from S-type asteroids inside the H2O snow line. Although the origin of water in ordinary chondrites is under debate, water generation from organic matter may also explain the D-rich water in ordinary chondrites because primordial organic matter is known to be D rich.

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