Raman spectroscopic study of the mineral composition of cirratulid tubes (Annelida, Polychaeta)

被引：22

作者：

Taylor, Paul D. ^{[1
]}

Vinn, Olev ^{[2
]}

Kudryavtsev, Anatoliy ^{[3
,4
]}

Schopf, J. William ^{[3
,5
,6
]}

机构：

[1] Nat Hist Museum, Dept Palaeontol, London SW7 5BD, England

[2] Univ Tartu, Dept Geol, EE-50411 Tartu, Estonia

[3] Univ Calif Los Angeles, Ctr Study Evolut & Origin Life, Los Angeles, CA 90095 USA

[4] Penn State Astrobiol Res Ctr, University Pk, PA 16802 USA

[5] Univ Calif Los Angeles, Dept Earth & Space Sci, Los Angeles, CA 90095 USA

[6] Univ Calif Los Angeles, Inst Mol Biol, Los Angeles, CA 90095 USA

来源：

JOURNAL OF STRUCTURAL BIOLOGY | 2010年 / 171卷 / 03期

关键词：

Biomineralization; Calcium carbonate; Cirratulid worms; Raman spectroscopy; Seawater chemistry; CARBONATE MINERALOGY; SEAWATER CHEMISTRY; ULTRASTRUCTURE; FOSSIL; BIOMINERALIZATION; GERMANY; GROWTH; GENUS;

D O I：

10.1016/j.jsb.2010.05.010

中图分类号：

Q5 [生物化学]; Q7 [分子生物学];

学科分类号：

071010 ; 081704 ;

摘要：

Raman spectroscopy was used to determine the mineralogical composition of the calcareous tubes of three species belonging to the family Cirratulidae. In all three cases, the tubes were found to be aragonitic, confirming previous inferences based on EDX and thin section studies, and corroborated by new EDX analyses revealing the presence of Sr but no Mg. Biomineralization in cirratulids is first recorded in the Oligocene epoch, at a time of aragonite seas. Similarly, the mineralogies of the earliest skeletons matched seawater chemistry in three other polychaete groups that independently evolved calcareous skeletons. Crown Copyright (C) 2010 Published by Elsevier Inc. All rights reserved.

引用

页码：402 / 405

页数：4

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