The Latitudinal Patterns of Leaf and Soil C:N:P Stoichiometry in the Loess Plateau of China

Understanding the spatial patterns and the driving factors of plant leaf and soil stoichiometry are critical for improving the parameterization of future ecological models and to predict the responses of ecosystems to environmental changes. This study aimed to determine how the latitudinal patterns...

Full description

Bibliographic Details
Main Authors: Zhao Fang, Dong-Dong Li, Feng Jiao, Jing Yao, Hao-Tian Du
Format: Article
Language:English
Published: Frontiers Media S.A. 2019-03-01
Series:Frontiers in Plant Science
Subjects:
Online Access:https://www.frontiersin.org/article/10.3389/fpls.2019.00085/full
id doaj-4f472429e9ba4e69a5bd1a87e5a43982
record_format Article
spelling doaj-4f472429e9ba4e69a5bd1a87e5a439822020-11-25T02:16:40ZengFrontiers Media S.A.Frontiers in Plant Science1664-462X2019-03-011010.3389/fpls.2019.00085430448The Latitudinal Patterns of Leaf and Soil C:N:P Stoichiometry in the Loess Plateau of ChinaZhao Fang0Zhao Fang1Dong-Dong Li2Dong-Dong Li3Feng Jiao4Feng Jiao5Jing Yao6Hao-Tian Du7State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling, ChinaInstitute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, ChinaInstitute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, ChinaUniversity of Chinese Academy of Sciences, Beijing, ChinaState Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling, ChinaInstitute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, ChinaState Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling, ChinaState Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling, ChinaUnderstanding the spatial patterns and the driving factors of plant leaf and soil stoichiometry are critical for improving the parameterization of future ecological models and to predict the responses of ecosystems to environmental changes. This study aimed to determine how the latitudinal patterns of leaf and soil C:N:P stoichiometry are affected by climate and vegetation types in the dryland ecosystems. The concentrations of leaf C, N, and P in herb community as well as soil nutrient concentrations along a 500–km–long latitudinal gradient in Northern Shaanxi of the Loess Plateau, were measured. The results showed that the soil C, N, P and C:N:P ratios at all three depths (0–10, 10–20, and 20–40 cm) showed significant latitudinal trends (except for soil C:N ratios) (P < 0.01). In general, the soil C, N and C:N:P ratios decreased exponentially while soil P increased first and then decreased with the latitude. The soil C, N, C:P, and N:P ratios at all three depths (0–10, 10–20 and 20–40 cm) were positively correlated with MAT and MAP (P < 0.05), while soil P and C:N ratios at all three depths were weakly correlated with MAT and MAP (P > 0.05). In addition, leaf C:N:P stoichiometry was significantly correlated with the latitude, MAT, and MAP (except for N:P ratios) (P < 0.01), such that, leaf C, C:N, and C:P ratios decreased as the latitude increased and MAT and MAP decreased, and leaf N, P concentrations increased as the latitude increased and MAT and MAP decreased, while leaf N:P ratios were weakly correlated with the latitude, MAT, and MAP (P > 0.05). Furthermore, the leaf C:N:P stoichiometry of herbaceous communities was related to the soil properties (except for soil P), and we found that the C:P ratios between the soil and leaves were strongly correlated. Compared with the global scale, the relatively high N:P ratios indicated that the vegetation growth of the herb community in the dryland of the Loess Plateau was more susceptible to P limitation.https://www.frontiersin.org/article/10.3389/fpls.2019.00085/fullecological stoichiometryclimatic factorsherb communityvegetation typesleavessoil
collection DOAJ
language English
format Article
sources DOAJ
author Zhao Fang
Zhao Fang
Dong-Dong Li
Dong-Dong Li
Feng Jiao
Feng Jiao
Jing Yao
Hao-Tian Du
spellingShingle Zhao Fang
Zhao Fang
Dong-Dong Li
Dong-Dong Li
Feng Jiao
Feng Jiao
Jing Yao
Hao-Tian Du
The Latitudinal Patterns of Leaf and Soil C:N:P Stoichiometry in the Loess Plateau of China
Frontiers in Plant Science
ecological stoichiometry
climatic factors
herb community
vegetation types
leaves
soil
author_facet Zhao Fang
Zhao Fang
Dong-Dong Li
Dong-Dong Li
Feng Jiao
Feng Jiao
Jing Yao
Hao-Tian Du
author_sort Zhao Fang
title The Latitudinal Patterns of Leaf and Soil C:N:P Stoichiometry in the Loess Plateau of China
title_short The Latitudinal Patterns of Leaf and Soil C:N:P Stoichiometry in the Loess Plateau of China
title_full The Latitudinal Patterns of Leaf and Soil C:N:P Stoichiometry in the Loess Plateau of China
title_fullStr The Latitudinal Patterns of Leaf and Soil C:N:P Stoichiometry in the Loess Plateau of China
title_full_unstemmed The Latitudinal Patterns of Leaf and Soil C:N:P Stoichiometry in the Loess Plateau of China
title_sort latitudinal patterns of leaf and soil c:n:p stoichiometry in the loess plateau of china
publisher Frontiers Media S.A.
series Frontiers in Plant Science
issn 1664-462X
publishDate 2019-03-01
description Understanding the spatial patterns and the driving factors of plant leaf and soil stoichiometry are critical for improving the parameterization of future ecological models and to predict the responses of ecosystems to environmental changes. This study aimed to determine how the latitudinal patterns of leaf and soil C:N:P stoichiometry are affected by climate and vegetation types in the dryland ecosystems. The concentrations of leaf C, N, and P in herb community as well as soil nutrient concentrations along a 500–km–long latitudinal gradient in Northern Shaanxi of the Loess Plateau, were measured. The results showed that the soil C, N, P and C:N:P ratios at all three depths (0–10, 10–20, and 20–40 cm) showed significant latitudinal trends (except for soil C:N ratios) (P < 0.01). In general, the soil C, N and C:N:P ratios decreased exponentially while soil P increased first and then decreased with the latitude. The soil C, N, C:P, and N:P ratios at all three depths (0–10, 10–20 and 20–40 cm) were positively correlated with MAT and MAP (P < 0.05), while soil P and C:N ratios at all three depths were weakly correlated with MAT and MAP (P > 0.05). In addition, leaf C:N:P stoichiometry was significantly correlated with the latitude, MAT, and MAP (except for N:P ratios) (P < 0.01), such that, leaf C, C:N, and C:P ratios decreased as the latitude increased and MAT and MAP decreased, and leaf N, P concentrations increased as the latitude increased and MAT and MAP decreased, while leaf N:P ratios were weakly correlated with the latitude, MAT, and MAP (P > 0.05). Furthermore, the leaf C:N:P stoichiometry of herbaceous communities was related to the soil properties (except for soil P), and we found that the C:P ratios between the soil and leaves were strongly correlated. Compared with the global scale, the relatively high N:P ratios indicated that the vegetation growth of the herb community in the dryland of the Loess Plateau was more susceptible to P limitation.
topic ecological stoichiometry
climatic factors
herb community
vegetation types
leaves
soil
url https://www.frontiersin.org/article/10.3389/fpls.2019.00085/full
work_keys_str_mv AT zhaofang thelatitudinalpatternsofleafandsoilcnpstoichiometryintheloessplateauofchina
AT zhaofang thelatitudinalpatternsofleafandsoilcnpstoichiometryintheloessplateauofchina
AT dongdongli thelatitudinalpatternsofleafandsoilcnpstoichiometryintheloessplateauofchina
AT dongdongli thelatitudinalpatternsofleafandsoilcnpstoichiometryintheloessplateauofchina
AT fengjiao thelatitudinalpatternsofleafandsoilcnpstoichiometryintheloessplateauofchina
AT fengjiao thelatitudinalpatternsofleafandsoilcnpstoichiometryintheloessplateauofchina
AT jingyao thelatitudinalpatternsofleafandsoilcnpstoichiometryintheloessplateauofchina
AT haotiandu thelatitudinalpatternsofleafandsoilcnpstoichiometryintheloessplateauofchina
AT zhaofang latitudinalpatternsofleafandsoilcnpstoichiometryintheloessplateauofchina
AT zhaofang latitudinalpatternsofleafandsoilcnpstoichiometryintheloessplateauofchina
AT dongdongli latitudinalpatternsofleafandsoilcnpstoichiometryintheloessplateauofchina
AT dongdongli latitudinalpatternsofleafandsoilcnpstoichiometryintheloessplateauofchina
AT fengjiao latitudinalpatternsofleafandsoilcnpstoichiometryintheloessplateauofchina
AT fengjiao latitudinalpatternsofleafandsoilcnpstoichiometryintheloessplateauofchina
AT jingyao latitudinalpatternsofleafandsoilcnpstoichiometryintheloessplateauofchina
AT haotiandu latitudinalpatternsofleafandsoilcnpstoichiometryintheloessplateauofchina
_version_ 1724889867372986368