Fe and Zn effects on the Si Cycle and diatom community structure in two contrasting high and low-silicate HNLC areas

We compared the importance of Fe, Zn and Si availability for diatom growth and silicification through microcosm enrichment experiments in two contrasting HNLC systems of the Sub-Arctic and Sub-Antarctic Pacific. The Bering Sea was characterized by low Fe

Bibliographic Details
Published in:Deep Sea Research Part I: Oceanographic Research Papers
Main Authors: LeBlanc, K, Hare, C, Boyd, P W, Bruland, K W, Sohst, B, Pickmere, Stuart, Lohan, M C, Buck, K, Ellwood, Michael, Hutchins, D A
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier
Subjects:
Keywords: Dissolution
Iron
Organic acids
Plants (botany)
Silicates
Trace elements
Zinc
Diatoms
HNLC
HNLSiLC
Trace metal limitation
Oceanography
community structure
diatom
nutrient availability
silicate
Bering Sea
oceanic regions
Pacifi Diatoms
Arctic
Antarctic
Pacific
Antarc*
Online Access:http://hdl.handle.net/1885/28320
https://doi.org/10.1016/j.dsr.2005.06.005
https://openresearch-repository.anu.edu.au/bitstream/1885/28320/5/ellwood23.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/28320/7/01_LeBlanc_Fe_and_Zn_effects_on_the_Si_2005.pdf.jpg
Description
Summary:We compared the importance of Fe, Zn and Si availability for diatom growth and silicification through microcosm enrichment experiments in two contrasting HNLC systems of the Sub-Arctic and Sub-Antarctic Pacific. The Bering Sea was characterized by low Fe

Similar Items