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DIATOM METHODS | δ18O Records.

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DIATOM METHODS | δ18O Records. / Leng, M.J.; Barker, Philip.
Encyclopedia of Quaternary Science. ed. / Scott A. Elias. Elsevier, 2006. p. 485-494.

Research output: Contribution in Book/Report/Proceedings - With ISBN/ISSN › Entry for encyclopedia/dictionary

Harvard

Leng, MJ & Barker, P 2006, DIATOM METHODS | δ18O Records. in SA Elias (ed.), Encyclopedia of Quaternary Science. Elsevier, pp. 485-494. https://doi.org/10.1016/B0-44-452747-8/00242-8

APA

Leng, M. J., & Barker, P. (2006). DIATOM METHODS | δ18O Records. In S. A. Elias (Ed.), Encyclopedia of Quaternary Science (pp. 485-494). Elsevier. https://doi.org/10.1016/B0-44-452747-8/00242-8

Vancouver

Leng MJ, Barker P. DIATOM METHODS | δ18O Records. In Elias SA, editor, Encyclopedia of Quaternary Science. Elsevier. 2006. p. 485-494 doi: 10.1016/B0-44-452747-8/00242-8

Author

Leng, M.J. ; Barker, Philip. / DIATOM METHODS | δ18O Records. Encyclopedia of Quaternary Science. editor / Scott A. Elias. Elsevier, 2006. pp. 485-494

Bibtex

@inbook{d312cd24d2f74fd0bd111fa59cbc3ba9,
title = "DIATOM METHODS | δ18O Records.",
abstract = "Diatom siica is a form of biogenic opal that contains oxygen isotopes which can be used in lacustrine and marine paleoenvironmental studies. Diatom δ18O is a useful indicator of paleoenvironmental conditions, reflecting either the temperature or the oxygen isotope composition of the water in which the diatoms grew. In lakes, the latter is a function of evaporation or changes in the source of rainfall. Analysis of diatom δ18O requires highly concentrated samples of almost pure diatom frustules.",
author = "M.J. Leng and Philip Barker",
note = "d18O records from diatoms.",
year = "2006",
doi = "10.1016/B0-44-452747-8/00242-8",
language = "English",
isbn = "978-0-444-52747-9",
pages = "485--494",
editor = "Elias, {Scott A.}",
booktitle = "Encyclopedia of Quaternary Science",
publisher = "Elsevier",

}

RIS

TY - CHAP

T1 - DIATOM METHODS | δ18O Records.

AU - Leng, M.J.

AU - Barker, Philip

N1 - d18O records from diatoms.

PY - 2006

Y1 - 2006

N2 - Diatom siica is a form of biogenic opal that contains oxygen isotopes which can be used in lacustrine and marine paleoenvironmental studies. Diatom δ18O is a useful indicator of paleoenvironmental conditions, reflecting either the temperature or the oxygen isotope composition of the water in which the diatoms grew. In lakes, the latter is a function of evaporation or changes in the source of rainfall. Analysis of diatom δ18O requires highly concentrated samples of almost pure diatom frustules.

AB - Diatom siica is a form of biogenic opal that contains oxygen isotopes which can be used in lacustrine and marine paleoenvironmental studies. Diatom δ18O is a useful indicator of paleoenvironmental conditions, reflecting either the temperature or the oxygen isotope composition of the water in which the diatoms grew. In lakes, the latter is a function of evaporation or changes in the source of rainfall. Analysis of diatom δ18O requires highly concentrated samples of almost pure diatom frustules.

U2 - 10.1016/B0-44-452747-8/00242-8

DO - 10.1016/B0-44-452747-8/00242-8

M3 - Entry for encyclopedia/dictionary

SN - 978-0-444-52747-9

SP - 485

EP - 494

BT - Encyclopedia of Quaternary Science

A2 - Elias, Scott A.

PB - Elsevier

ER -