Arctic aquatic graminoid tundra responses to nutrient availability

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 do...

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Main Authors: Andresen, Christian G., Lougheed, Vanessa L.
Format: Text
Language:English
Published: 2020
Subjects:
Online Access:https://doi.org/10.5194/bg-2020-351
https://bg.copernicus.org/preprints/bg-2020-351/
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spelling ftcopernicus:oai:publications.copernicus.org:bgd89899 2023-05-15T14:54:40+02:00 Arctic aquatic graminoid tundra responses to nutrient availability Andresen, Christian G. Lougheed, Vanessa L. 2020-10-23 application/pdf https://doi.org/10.5194/bg-2020-351 https://bg.copernicus.org/preprints/bg-2020-351/ eng eng doi:10.5194/bg-2020-351 https://bg.copernicus.org/preprints/bg-2020-351/ eISSN: 1726-4189 Text 2020 ftcopernicus https://doi.org/10.5194/bg-2020-351 2020-10-26T17:22:13Z 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: Carex aquatilis and Arctophila fulva . 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 biomass and Normalize Difference Vegetation Index (NDVI) 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 C. aquatilis based on historical leaf nutrient data from 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, carbon and energy balance. In addition, aquatic plant NDVI spectral responses to nutrients can serve as landscape hot-spot and hot-moment indicator of landscape biogeochemical heterogeneity associated with permafrost degradation, nutrient leaching and availability. Text Arctic Arctophila fulva Barrow Carex aquatilis permafrost Thermokarst Tundra Alaska Copernicus Publications: E-Journals Arctic Barrow Peninsula ENVELOPE(-66.248,-66.248,63.051,63.051)
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description 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: Carex aquatilis and Arctophila fulva . 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 biomass and Normalize Difference Vegetation Index (NDVI) 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 C. aquatilis based on historical leaf nutrient data from 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, carbon and energy balance. In addition, aquatic plant NDVI spectral responses to nutrients can serve as landscape hot-spot and hot-moment indicator of landscape biogeochemical heterogeneity associated with permafrost degradation, nutrient leaching and availability.
format Text
author Andresen, Christian G.
Lougheed, Vanessa L.
spellingShingle Andresen, Christian G.
Lougheed, Vanessa L.
Arctic aquatic graminoid tundra responses to nutrient availability
author_facet Andresen, Christian G.
Lougheed, Vanessa L.
author_sort Andresen, Christian G.
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
publishDate 2020
url https://doi.org/10.5194/bg-2020-351
https://bg.copernicus.org/preprints/bg-2020-351/
long_lat ENVELOPE(-66.248,-66.248,63.051,63.051)
geographic Arctic
Barrow Peninsula
geographic_facet Arctic
Barrow Peninsula
genre Arctic
Arctophila fulva
Barrow
Carex aquatilis
permafrost
Thermokarst
Tundra
Alaska
genre_facet Arctic
Arctophila fulva
Barrow
Carex aquatilis
permafrost
Thermokarst
Tundra
Alaska
op_source eISSN: 1726-4189
op_relation doi:10.5194/bg-2020-351
https://bg.copernicus.org/preprints/bg-2020-351/
op_doi https://doi.org/10.5194/bg-2020-351
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