28
Views
9
CrossRef citations to date
0
Altmetric
Original Articles

Utility of microforaminifera test linings in palynological preparations

&
Pages 77-84 | Published online: 24 Aug 2010
 

Abstract

In this study we examine the nature of microforaminifera test linings found in palynological preparations and demonstrate the potential of these palynomorphs for paleoenvironmental interpretation. Sediment samples from four marsh salinity zones of the Barataria Basin, Mississippi Delta, were processed by conventional palynological techniques which included HC1 and acetolysis treatments. Taxonomic identification was not attempted, but it is assumed that Rotalidae forams, Miliammina fusca and Ammonia beccari, are important constituents of the test lining assemblages. Multi‐chambered forms were classed by morphotype, size, number of chambers, spacing of chambers, and condition. The absence of a relationship between size and chamber number within each morphotype implies the presence of multiple species populations. There is also no relationship between foram concentration and salinity. Using stepwise discriminant analysis, six classes were selected which enable successful discrimination among the four salinity zones.

Notes

Present Address: Ontario Veterinary College, University of Guelph, Guelph, Ontario N1G 2W1, Canada

Corresponding author

Reprints and Corporate Permissions

Please note: Selecting permissions does not provide access to the full text of the article, please see our help page How do I view content?

To request a reprint or corporate permissions for this article, please click on the relevant link below:

Academic Permissions

Please note: Selecting permissions does not provide access to the full text of the article, please see our help page How do I view content?

Obtain permissions instantly via Rightslink by clicking on the button below:

If you are unable to obtain permissions via Rightslink, please complete and submit this Permissions form. For more information, please visit our Permissions help page.