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Proteins from the organic matrix of core-top and fossil planktonic foraminifera

Journal Article · · Geochimica et Cosmochimica Acta; (USA)
 [1];  [2]
  1. Univ. of South Florida, Tampa (USA)
  2. Univ. of Miami, FL (USA)
Organic constituents isolated from the tests (shells) of six species of core-top planktonic foraminifera, ranging in age between 2 and 4 Ka BP, consist of heterogeneous mixture of proteins and polypeptides. At least seven discrete polypeptides are present as indicated by reverse phase HPLC and by gel electrophoresis. High percentages of aspartic acid and glutamic acid characterize one class of protein, while glycine, serine, and alanine-rich proteins dominate in a second class. Similar HPLC chromatographic elution profiles are observed for all species analyzed, varying only in intensity of the peaks and in amino acid composition from species to species. The approximate molecular weights of two major fossil proteins ranged between 50,000 and 70,000 daltons. A comparison of 2-4 and 300 Ka BP samples shows that while most of the polypeptides are present in both samples, some acidic polypeptides are not present in the older sample. These data suggest that some of the acidic polypeptides may be more soluble than other fractions and are lost more quickly from the test. The remaining hydrophobic, possibly more insoluble, polypeptides may be preserved in much older speciments and may be useful in tracing phylogeny of the planktonic foraminifera. Amino acid analyses of total test extracts before and after dialysis demonstrate that some acidic amino acids, particularly aspartic acid, and possibly peptides less than 6,000-8,000 daltons are lost during dialysis. These data caution against the use of total amino acid compositions in biogeochemical studies.
OSTI ID:
5982203
Journal Information:
Geochimica et Cosmochimica Acta; (USA), Journal Name: Geochimica et Cosmochimica Acta; (USA) Vol. 54:8; ISSN GCACA; ISSN 0016-7037
Country of Publication:
United States
Language:
English

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