Salt marsh vegetation change during a half-century of experimental nutrient addition and climate-driven controls in Great Sippewissett Marsh.

Coastal wetland Ecophenotypes Long-term experiment Nitrogen supply Plant ecological engineers Sea level rise

Journal

The Science of the total environment
ISSN: 1879-1026
Titre abrégé: Sci Total Environ
Pays: Netherlands
ID NLM: 0330500

Informations de publication

Date de publication:
01 Apr 2023
Historique:
received: 14 11 2022
revised: 06 01 2023
accepted: 07 01 2023
pubmed: 13 1 2023
medline: 16 2 2023
entrez: 12 1 2023
Statut: ppublish

Résumé

Vegetative cover was mapped annually, 1976-2022, in experimental plots in Great Sippewissett Marsh, Cape Cod, USA, chronically fertilized at different doses, and subject to changes in sea level and other climate-related variables. Dominant species within areas of higher elevation in the plots followed different decadal trajectories: rise in sea level diminished cover of Spartina patens; higher N supplies increased cover of Distichlis spicata. The opportunistic growth response of D. spicata to high N supplies unexpectedly fostered increased platform accretion, a feature that persisted for succeeding decades and led to further changes in vegetation: D. spicata functioned as an effective ecosystem engineer with long-term ecological consequences. Shrubs usually found in upper marsh margins expanded into areas where D. spicata had stimulated accretion, then shaded and excluded D. spicata, but subsequently lost cover as sea level rise continued. Increased N supply converted stands of Spartina alterniflora, the dominant low marsh species, from short to taller ecophenotypes; sea level rise had minor effects on S. alterniflora, but during 2019-2022 appeared to reach a tipping point that fostered taller S. alterniflora and bare space even in un-fertilized control plots, and in Great Sippewissett Marsh in general. Model results anticipate that-in spite of potential accretion enhanced by vegetation and ecosystem engineer effects-there will be loss of high marsh, transient increases of low marsh, followed by loss of low marsh, and eventual conversion to shallow open water by the end of the century. Dire local projections match those of the plurality of recent reports from salt marshes around the world. Proposed management strategies may only delay unfortunate outcomes rather than maintain wetlands. Concerted reductions of warming from greenhouse gases, and lower N loads seem necessary to address the coming crises in wetlands-and many other environmental threats.

Identifiants

pubmed: 36634783
pii: S0048-9697(23)00161-4
doi: 10.1016/j.scitotenv.2023.161546
pii:
doi:

Substances chimiques

Water 059QF0KO0R

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Pagination

161546

Informations de copyright

Copyright © 2023 Elsevier B.V. All rights reserved.

Déclaration de conflit d'intérêts

Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

Auteurs

I Valiela (I)

The Ecosystems Center, Marine Biological Laboratory, Woods Hole, MA 02543, USA.

K Chenoweth (K)

The Ecosystems Center, Marine Biological Laboratory, Woods Hole, MA 02543, USA. Electronic address: kchenoweth@mbl.edu.

J Lloret (J)

The Ecosystems Center, Marine Biological Laboratory, Woods Hole, MA 02543, USA.

J Teal (J)

Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA.

B Howes (B)

School of Marine Science and Technology, University of Massachusetts, Dartmouth, New Bedford, MA 02744, USA.

D Goehringer Toner (D)

School of Marine Science and Technology, University of Massachusetts, Dartmouth, New Bedford, MA 02744, USA.

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