The effects of El Niño‐Southern Oscillation events on intertidal seagrass beds over a long‐term timescale

El Niño‐Southern Oscillation (ENSO) events can cause dramatic changes in marine communities. However, we know little as to how ENSO events affect tropical seagrass beds over decadal timescales. Therefore, a diverse array of seagrass (Thalassia hemprichii) habitat types were surveyed once every 3 mon...

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Veröffentlicht in:Global change biology 2018-10, Vol.24 (10), p.4566-4580
Hauptverfasser: Lin, Hsing‐Juh, Lee, Chen‐Lu, Peng, Shang‐En, Hung, Meng‐Chi, Liu, Pi‐Jen, Mayfield, Anderson B.
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container_end_page 4580
container_issue 10
container_start_page 4566
container_title Global change biology
container_volume 24
creator Lin, Hsing‐Juh
Lee, Chen‐Lu
Peng, Shang‐En
Hung, Meng‐Chi
Liu, Pi‐Jen
Mayfield, Anderson B.
description El Niño‐Southern Oscillation (ENSO) events can cause dramatic changes in marine communities. However, we know little as to how ENSO events affect tropical seagrass beds over decadal timescales. Therefore, a diverse array of seagrass (Thalassia hemprichii) habitat types were surveyed once every 3 months for 16 years (January 2001 to February 2017) in a tropical intertidal zone that is regularly affected by both ENSO events and anthropogenic nutrient enrichment. La Niña and El Niño events had distinct effects on the biomass and growth of T. hemprichii. During La Niña years, higher (a) precipitation levels and (b) seawater nitrogen concentrations led to increases in seagrass leaf productivity, canopy height, and biomass. However, the latter simultaneously stimulated the growth of periphyton on seagrass leaves; this led to decreases in seagrass cover and shoot density. More frequent La Niña events could, then, eventually lead to either a decline in intertidal seagrass beds or a shift to another, less drought‐resistant seagrass species in those regions already characterized by eutrophication due to local anthropogenic activity. La Niña and El Niño events had distinct effects on the biomass and growth of the seagrass Thalassia hemprichii. During La Niña years, higher precipitation levels and seawater nitrogen concentrations led to increase in leaf productivity, canopy height, and biomass. However, the latter simultaneously stimulated the growth of periphyton on seagrass leaves; this led to decreases in seagrass cover and shoot density. More frequent La Niña events could, then, eventually lead to either a decline in intertidal seagrass beds or a shift to another, less drought‐resistant seagrass species in those regions already characterized by eutrophication due to local anthropogenic activity.
doi_str_mv 10.1111/gcb.14404
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However, we know little as to how ENSO events affect tropical seagrass beds over decadal timescales. Therefore, a diverse array of seagrass (Thalassia hemprichii) habitat types were surveyed once every 3 months for 16 years (January 2001 to February 2017) in a tropical intertidal zone that is regularly affected by both ENSO events and anthropogenic nutrient enrichment. La Niña and El Niño events had distinct effects on the biomass and growth of T. hemprichii. During La Niña years, higher (a) precipitation levels and (b) seawater nitrogen concentrations led to increases in seagrass leaf productivity, canopy height, and biomass. However, the latter simultaneously stimulated the growth of periphyton on seagrass leaves; this led to decreases in seagrass cover and shoot density. More frequent La Niña events could, then, eventually lead to either a decline in intertidal seagrass beds or a shift to another, less drought‐resistant seagrass species in those regions already characterized by eutrophication due to local anthropogenic activity. La Niña and El Niño events had distinct effects on the biomass and growth of the seagrass Thalassia hemprichii. During La Niña years, higher precipitation levels and seawater nitrogen concentrations led to increase in leaf productivity, canopy height, and biomass. However, the latter simultaneously stimulated the growth of periphyton on seagrass leaves; this led to decreases in seagrass cover and shoot density. More frequent La Niña events could, then, eventually lead to either a decline in intertidal seagrass beds or a shift to another, less drought‐resistant seagrass species in those regions already characterized by eutrophication due to local anthropogenic activity.</abstract><cop>England</cop><pub>Blackwell Publishing Ltd</pub><pmid>30030884</pmid><doi>10.1111/gcb.14404</doi><tpages>16</tpages><orcidid>https://orcid.org/0000-0001-8322-7195</orcidid><orcidid>https://orcid.org/0000-0003-4644-1779</orcidid></addata></record>
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subjects Anthropogenic factors
Biomass
Drought
Ecosystem
El Nino
El Nino phenomena
El Nino-Southern Oscillation
ENSO
Eutrophication
Grasses
Halodule uninervis
Hydrocharitaceae - physiology
Intertidal environment
Intertidal zone
La Nina
La Niña
Leaves
Mineral nutrients
Nitrogen - analysis
Nutrient enrichment
Ocean currents
Periphyton
Plant cover
Plant Leaves
Sea grasses
Seawater
Seawater - chemistry
Southern Oscillation
Thalassia hemprichii
Tropical climate
title The effects of El Niño‐Southern Oscillation events on intertidal seagrass beds over a long‐term timescale
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