Marine Ecology Progress Series

Inter-Research
Marine Ecology Progress Series

IR Home



MEPS
Home
Editors
Forthcoming
Information
Subscribe


Journals
Home
MEPS
AME
CR
DAO
ESEP
Search
Subscribe

Book Series
EE Books
Top Books
ESEP Books
Order

EEIU Brochures
(pdf format)

Discussion Forums
Home

Research
Endangered Species Programs

Institutions
International Ecology Institute
Eco-Ethics International Union

Foundation
Otto Kinne Foundation

MEPS 255:15-25 (2003)

Abstract

Stable carbon isotope evidence for coupling between sedimentary bacteria and seagrasses in a sub-tropical lagoon

W. Brian Jones1, Luis A. Cifuentes1,*, James E. Kaldy2

1Oceanography Department, Texas A&M University, MS 3146, College Station, Texas 77843, USA
2Pacific Coastal Ecology Branch, Western Ecology Division, US Environmental Protection Agency, 2111 SE Marine Science Center Dr., Newport, Oregon 97366, USA

*Corresponding author. Email: lcifuentes@ocean.tamu.edu

ABSTRACT: We measured stable carbon isotope ratios (d13C) in phospholipid fatty acids (PLFAs) to identify the primary carbon source utilized by sedimentary bacteria in Lower Laguna Madre, Texas, which is a seagrass dominated lagoon. Comparisons were made between 3 differing habitat types consisting of a bare area, a transitional area, and a vegetated area. Using PLFA concentrations, we estimated that bacterial abundance was significantly higher in the vegetated habitat compared with bare or transitional habitats. Seagrass Thalassia testudinum above-ground tissues averaged -10.8 ± 0.3‰ and benthic microalgae, based on 20:5D3 PLFA, averaged -20.5 ± 0.6‰. The d13C of total organic carbon (TO13C) from all habitats and depths were within ±2‰ of T. testudinum above-ground tissues, suggesting that the majority of sedimentary organic carbon originated from this source. The d13C of the ubiquitous 16:0 PLFA indicated more complexity in surface vegetated sediments and at depth (ca. 19 cm) in bare and transitional habitats. In turn, the d13C of branched, iso- and anteiso-15:0 (i&a15:0) PLFAs found only in bacteria were within ±3‰ of TO13C in all habitats and at all depths. Our work confirmed coupling between sedimentary bacteria and seagrasses occurs in oligotrophic systems with few allochthonous inputs.

KEY WORDS: Seagrasses · Carbon cycling · Bacteria · Phospholipid fatty acids · Stable carbon isotope ratio

Full text in pdf format

Published in MEPS Vol. 255 (2003) on June 24
Print ISSN: 0171-8630; Online ISSN: 1616-1599. Copyright © Inter-Research, Oldendorf/Luhe, 2003

Copyright © 2003; Inter-Research
Webmaster: webmaster@int-res.com