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Advances in the aquatic sciences
RESEARCH ARTICLE

Rainfall and its possible hysteresis effect on the proportional cover of tropical tidal-wetland mangroves and saltmarsh–saltpans

Norman C. Duke https://orcid.org/0000-0003-2081-9120 A E , Colin Field B , Jock R. Mackenzie A , Jan-Olaf Meynecke C and Apanie L. Wood D
+ Author Affiliations
- Author Affiliations

A James Cook University, TropWATER – Centre for Tropical Water and Aquatic Ecosystem Research, Townsville, Qld 4811, Australia.

B University of Technology, Sydney, NSW 2007, Australia.

C Griffith Centre for Coastal Management and Australian Rivers Institute, Griffith University, Gold Coast, Qld 4222, Australia.

D MangroveWatch Ltd, PO Box 1250, Elanora, Qld 4221, Australia.

E Corresponding author. Email: norman.duke@jcu.edu.au

Marine and Freshwater Research 70(8) 1047-1055 https://doi.org/10.1071/MF18321
Submitted: 31 August 2018  Accepted: 4 January 2019   Published: 21 February 2019

Abstract

Mangrove–saltmarsh tidal wetlands are highly dynamic ecosystems, responding and adapting to climate and physical conditions at all spatial and temporal scales. Knowledge of the large-scale ecosystem processes involved and how they might be influenced by climate variables is highly relevant today. For tidal-wetland sites well within the latitudinal range of the mostly tropical mangrove communities, we confirm that average annual rainfall influences vegetative cover, as well as species composition and biomass of tidal wetlands. On the basis of 205 largely unmodified, tropical and subtropical estuaries of northern Australia, a sigmoidal relationship, with a centroid inflection point ~1368 mm, was derived between rainfall and the relative amounts of high-biomass mangroves and low-biomass saltmarsh–saltpan vegetation. The presence and probability of observed combinations of these community types were quantified using the wetland cover index, which is the ratio of total mangrove area to that of mangroves plus intertidal saltmarsh and saltpans. Accordingly, periodic changes in rainfall trends are likely manifest as either encroachment or dieback of mangroves along the ecotones separating them from tidal saltmarsh–saltpans. Presented is a new conceptual framework and model that describes how such ecosystem-scale processes take place in tropical and subtropical tidal wetlands.

Additional keywords : climate change, ecosystem state change, ecotone shift, tidal saltmarsh, wetland cover index.


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