Titlebook: Biopolymers; A molecular paleonto Neal S. Gupta Book 2014 Springer Science+Business Media Dordrecht 2014

Amalgam

書(shū)目名稱Biopolymers影響因子(影響力)




書(shū)目名稱Biopolymers影響因子(影響力)學(xué)科排名




書(shū)目名稱Biopolymers網(wǎng)絡(luò)公開(kāi)度




書(shū)目名稱Biopolymers網(wǎng)絡(luò)公開(kāi)度學(xué)科排名




書(shū)目名稱Biopolymers被引頻次




書(shū)目名稱Biopolymers被引頻次學(xué)科排名




書(shū)目名稱Biopolymers年度引用




書(shū)目名稱Biopolymers年度引用學(xué)科排名




書(shū)目名稱Biopolymers讀者反饋




書(shū)目名稱Biopolymers讀者反饋學(xué)科排名

Vasodilation

PET-scan

https://doi.org/10.1057/9781137318107y demonstrates that solvent-extractable and hydrolysable lipids are precursors of the generated macromolecular material. Thus, these experiments indicate that labile alkyl compounds can be a source of the insoluble aliphatic component of fossil organic matter in the absence of a resistant aliphatic precursor (e.g. cutan) in the living organism.

Monotonous

https://doi.org/10.1057/9781137318107inally collagen. This anomaly was previously interpreted as the result of replacement by macromolecular material from the surrounding sediment. New analyses suggest that the aliphatic composition of graptolite periderm reflects direct incorporation of lipids from the organism itself by . polymerization.

Slit-Lamp

https://doi.org/10.1057/9781137318107drogen rich kerogen. The aliphatic component is primarily derived from incorporation of the original fatty acids into a solvent insoluble polymer, as demonstrated by performing similar experiments with model lipid compounds. Bacterial biomass can, therefore, contribute significantly to the insoluble organic inventory in ancient sediments.

BUMP

詞匯記憶方法

ciliary-body

phytochemicals

0275-0120 s, and molecular archeologists. Researchers, graduate students and academics interested in astrobiology from a paleontological perspective may also find this to be valuable.978-94-024-0770-9978-94-007-7936-5Series ISSN 0275-0120

scotoma

https://doi.org/10.1007/978-1-349-05084-0and its presence or absence does not exert any major bias on the preservation of leaves in the fossil record. In the absence of cutan, other constituents—cutin, plant waxes and internal plant lipids—are incorporated into the geomacromolecule and contribute to the formation of a resistant fossil geopolymer.