Arctic aquatic graminoid tundra responses to nutrient availability

<p>Unraveling the environmental controls influencing Arctic tundra productivity is paramount for advancing our predictive understanding of the causes and consequences of warming in tundra ecosystems and associated land–atmosphere feedbacks. This study focuses on aquatic emergent tundra plants,...

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Main Authors: C. G. Andresen, V. L. Lougheed
Format: Article
Language:English
Published: Copernicus Publications 2021-04-01
Series:Biogeosciences
Online Access:https://bg.copernicus.org/articles/18/2649/2021/bg-18-2649-2021.pdf
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spelling doaj-afdc40b48fba40f5afdb0374f6c0c1d72021-04-27T07:28:05ZengCopernicus PublicationsBiogeosciences1726-41701726-41892021-04-01182649266210.5194/bg-18-2649-2021Arctic aquatic graminoid tundra responses to nutrient availabilityC. G. Andresen0C. G. Andresen1V. L. Lougheed2Geography Department, University of Wisconsin-Madison, Madison, WI, USABiological Sciences Department, University of Texas at El Paso, El Paso, TX, USABiological Sciences Department, University of Texas at El Paso, El Paso, TX, USA<p>Unraveling the environmental controls influencing Arctic tundra productivity is paramount for advancing our predictive understanding of the causes and consequences of warming in tundra ecosystems and associated land–atmosphere feedbacks. This study focuses on aquatic emergent tundra plants, which dominate productivity and methane fluxes in the Arctic coastal plain of Alaska. In particular, we assessed how environmental nutrient availability influences production of biomass and greenness in the dominant aquatic tundra species: <i>Arctophila fulva</i> and <i>Carex aquatilis</i>. We sampled a total of 17 sites distributed across the Barrow Peninsula and Atqasuk, Alaska, following a nutrient gradient that ranged from sites with thermokarst slumping or urban runoff to sites with relatively low nutrient inputs. Employing a multivariate analysis, we explained the relationship of soil and water nutrients to plant leaf macro- and micro-nutrients. Specifically, we identified soil phosphorus as the main limiting nutrient factor given that it was the principal driver of aboveground biomass (<span class="inline-formula"><i>R</i><sup>2</sup>=0.34</span>, <span class="inline-formula"><i>p</i>=0.002</span>) and normalized difference vegetation index (NDVI) (<span class="inline-formula"><i>R</i><sup>2</sup>=0.47</span>, <span class="inline-formula"><i>p</i>=0.002</span>) in both species. Plot-level spectral NDVI was a good predictor of leaf P content for both species. We found long-term increases in N, P and Ca in <i>C. aquatilis</i> based on historical leaf nutrient data from the 1970s of our study area. This study highlights the importance of nutrient pools and mobilization between terrestrial–aquatic systems and their potential influence on productivity and land–atmosphere carbon balance. In addition, aquatic plant NDVI spectral responses to nutrients can serve as landscape hot-spot and hot-moment indicators of landscape biogeochemical heterogeneity associated with permafrost degradation, nutrient leaching and availability.</p>https://bg.copernicus.org/articles/18/2649/2021/bg-18-2649-2021.pdf
collection DOAJ
language English
format Article
sources DOAJ
author C. G. Andresen
C. G. Andresen
V. L. Lougheed
spellingShingle C. G. Andresen
C. G. Andresen
V. L. Lougheed
Arctic aquatic graminoid tundra responses to nutrient availability
Biogeosciences
author_facet C. G. Andresen
C. G. Andresen
V. L. Lougheed
author_sort C. G. Andresen
title Arctic aquatic graminoid tundra responses to nutrient availability
title_short Arctic aquatic graminoid tundra responses to nutrient availability
title_full Arctic aquatic graminoid tundra responses to nutrient availability
title_fullStr Arctic aquatic graminoid tundra responses to nutrient availability
title_full_unstemmed Arctic aquatic graminoid tundra responses to nutrient availability
title_sort arctic aquatic graminoid tundra responses to nutrient availability
publisher Copernicus Publications
series Biogeosciences
issn 1726-4170
1726-4189
publishDate 2021-04-01
description <p>Unraveling the environmental controls influencing Arctic tundra productivity is paramount for advancing our predictive understanding of the causes and consequences of warming in tundra ecosystems and associated land–atmosphere feedbacks. This study focuses on aquatic emergent tundra plants, which dominate productivity and methane fluxes in the Arctic coastal plain of Alaska. In particular, we assessed how environmental nutrient availability influences production of biomass and greenness in the dominant aquatic tundra species: <i>Arctophila fulva</i> and <i>Carex aquatilis</i>. We sampled a total of 17 sites distributed across the Barrow Peninsula and Atqasuk, Alaska, following a nutrient gradient that ranged from sites with thermokarst slumping or urban runoff to sites with relatively low nutrient inputs. Employing a multivariate analysis, we explained the relationship of soil and water nutrients to plant leaf macro- and micro-nutrients. Specifically, we identified soil phosphorus as the main limiting nutrient factor given that it was the principal driver of aboveground biomass (<span class="inline-formula"><i>R</i><sup>2</sup>=0.34</span>, <span class="inline-formula"><i>p</i>=0.002</span>) and normalized difference vegetation index (NDVI) (<span class="inline-formula"><i>R</i><sup>2</sup>=0.47</span>, <span class="inline-formula"><i>p</i>=0.002</span>) in both species. Plot-level spectral NDVI was a good predictor of leaf P content for both species. We found long-term increases in N, P and Ca in <i>C. aquatilis</i> based on historical leaf nutrient data from the 1970s of our study area. This study highlights the importance of nutrient pools and mobilization between terrestrial–aquatic systems and their potential influence on productivity and land–atmosphere carbon balance. In addition, aquatic plant NDVI spectral responses to nutrients can serve as landscape hot-spot and hot-moment indicators of landscape biogeochemical heterogeneity associated with permafrost degradation, nutrient leaching and availability.</p>
url https://bg.copernicus.org/articles/18/2649/2021/bg-18-2649-2021.pdf
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