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Meteoroid bombardment of the Earth-Moon system must have caused catastrophic damage to the terrestrial ecosphere. However, ancient meteoroid impacts and their relations to environmental changes are not well understood because of erosion and/or resurfacing processes on Earth. Here, we investigate the formation ages of 59 lunar craters with fresh morphologies and diameters greater than approximately 20 km and first find that 8 of 59 craters were formed simultaneously. Considering the radiometric ages of ejecta from Copernicus crater and impact glass spherules from various Apollo landing sites, we conclude that sporadic meteoroid bombardment occurred across the whole Moon at approximately 800 Ma. Based on crater scaling laws and collision probabilities with the Earth and Moon, we suggest that at least (4–5) × 10 16 kg of meteoroids, approximately 30–60 times more than the Chicxulub impact, must have plunged into the Earth-Moon system immediately before the Cryogenian, which was an era of great environmental changes.

We here show that tetradecanoyl phorbol acetate (TPA) and I-oleoyl 2-acetyl glycerol (OAG) cause the translocation of diacylglycxxol (DG) kinase from the cytosol to the membrane fractions in chick embryo fibroblast (CEF) cells. However, this translocation is not marked in erbB-transformed chick embryo fibroblast (GEV) cells. The activities of phosphatidylinositol (PI) and phosphatidylinositol4-phosphate (PIP) kinases in membrane fractions are not altered by TPA treatment in either CEF or GEV cells. Such reduced translocation of DG kinase by TPA is also observed in src-transformed cells, but not in myc-transformed cells. These results suggest that the defect in DG kinase translocation may result in failure to suppress the overactivation of protein kinase C in erbB-2 and src-transformed cells, which may lead to cell growth and transformation.

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