Mangrove ecosystem changes during the Holocene at Spanish Lookout Cay, Belize

Monacci, Natalie M. and Meier-Grünhagen, Ursula and Finney, Bruce P. and Behling, Hermann and Wooller, Matthew J. (2009) Mangrove ecosystem changes during the Holocene at Spanish Lookout Cay, Belize. Palaeogeography, Palaeoclimatology, Palaeoecology, 280 (1-2). pp. 37-46. ISSN 00310182

[img] PDF - Published Version
Restricted to Full text available on request

Download (1130Kb) | Request a copy

    Abstract

    Mangroves are halophytic plants living at the land–sea interface and are therefore natural trackers of sealevel. Multiple proxies of a continuous (8 m) mangrove peat core (BT-79) from Spanish Lookout Cay, Belize illustrate mangrove ecosystem changes during the Holocene. Radiocarbon measurements show this site was colonized by mangroves ~8000 cal. yrs BP, with a significant decrease in the peat accumulation rate from ~6000 to 1000 cal. yrs BP. Stratigraphic characteristics of this peat core such as bulk density, magnetic susceptibility, and loss on ignition show relative uniformity, inferring an uninterrupted mangrove ecosystem during a majority of the Holocene. This is supported by pollen data from BT-79 that show that the site has been consistently dominated by Rhizophora mangle (red mangrove), with Avicennia germinans (black mangrove) and Laguncularia racemosa (white mangrove) present as well. Subfossil R. mangle leaves are used for stable nitrogen, carbon, and oxygen isotope (δ15N, δ13C, and δ18O) analyses. δ15N and δ13C values provide a proxy of this plant's past physiology and stand structure showing that dwarf (δ15Nb−3‰) and tall (δ13Cb −27‰) R. mangle stands were previously present at the site, which are a result of nutrient limitations that we equate with seawater inundation. δ18O values show differences in source water of R. mangle, with higher values attributed to the source water being composed of a greater proportion of seawater relative to precipitation. A decrease in inundation at the site is shown by lower δ18O values (b19‰) from ~7000 to ~1000 cal. yrs BP that covary with the decreased sedimentation rate. Existing Caribbean sea-level data do not show evidence of a decrease in the rate of relative sea-level rise or fluctuations that we take to be the major causes of environmental changes at site BT-79.

    Item Type: Peer-reviewed Journal Article
    Related URLs:
    Unique ID or DOI: 10.1016/j.palaeo.2009.05.013
    Publisher: Elsevier
    Keywords: Belize,Holocene,Mangroves,Paleoecology,Sea-level,Stable isotopes
    Subjects: (C) Ecosystems > (CB) Marine > (CBE) Mangroves
    Publication Sources: (3) Other Source > (3C) Other Universities
    Date Deposited: 15 Dec 2010 13:30
    Last Modified: 20 Jan 2011 14:26
    URI: http://eprints.uberibz.org/id/eprint/1132

    Actions (login required)

    View Item