ULTRASTRUCTURAL AND PALEOBIOCHEMICAL CORRELATIONS AMONG FOSSIL LEAF TISSUES FROM THE ST-MARIES RIVER (CLARKIA) AREA, NORTHERN IDAHO, USA
ULTRASTRUCTURAL AND PALEOBIOCHEMICAL CORRELATIONS AMONG FOSSIL LEAF TISSUES FROM THE ST-MARIES RIVER (CLARKIA) AREA, NORTHERN IDAHO, USA
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DOI:
10.2307/2442769
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发表时间:
1981-01-01
影响因子:
3
通讯作者:
BROWN, RM
中科院分区:
文献类型:
--
作者:
NIKLAS, KJ;BROWN, RM
Miocene angiosperm leaf tissues of Betula, Hydrangea, Platanus, Quercus, Castanea, Persea and gymnospermous tissues from offshore and onshore lacustrine sediments, respectively, reveal various states of ultrastructural detail in preservation which correlate with their paleobiochemical profiles. Excellent cytologic preservation of membrane-bound organelles in offshore tissue samples is correlated with relatively mild chlorophyll and fatty acid degradation (chlorins, unsaturated hydrocarbons), while progressive deterioration of ultrastructure seen in onshore specimens is concomitant with extensive chlorophyll degradation and saturation of hydrocarbons. Comparative studies between fossils found in pyroclastic (Succor Creek Flora, Miocene) and lacustrine (Clarkia Flora) environments indicate that the degree of pre- and post-depositional hydration of tissues is a less significant factor in determining preservation than redox potential and secondary metabolites (tannic acids, chlorophyll derivatives). A sequence of organelle degradation in leaf tissues is given; apparently chloroplasts and cell walls are the most stable cellular constituents, while the endoplasmic reticulum, nuclei and mitochondria are the most labile.