n. suberinite
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西北中生界煤系烃源岩中普遍含有木栓质体，它来源于植物周皮的木栓化细胞壁。
Suberinite occurs commonly in Mesozoic coal measures and terrestrial organic matter source rocks in Northwest China, which is formed from suberized cell walls, particularly in plant periderm.
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木栓质体是指褐煤中保存的由植物的根、表皮、茎和枝等外部周皮组织所形成的显微组分。木栓质体和细胞壁、细胞腔皆与栓质化物质的树皮体相当。
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