GLORIA

GEOMAR Library Ocean Research Information Access

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • Zhang, Kerong  (5)
  • Biodiversity Research  (5)
Material
Publisher
Person/Organisation
Language
Years
FID
  • Biodiversity Research  (5)
  • 1
    Online Resource
    Online Resource
    Wiley ; 2018
    In:  Global Change Biology Vol. 24, No. 1 ( 2018-01), p. 536-551
    In: Global Change Biology, Wiley, Vol. 24, No. 1 ( 2018-01), p. 536-551
    Abstract: Knowledge of nutrient storage and partitioning in forests is imperative for ecosystem models and ecological theory. Whether the nutrients (N, P, K, Ca, and Mg) stored in forest biomass and their partitioning patterns vary systematically across climatic gradients remains unknown. Here, we explored the global‐scale patterns of nutrient density and partitioning using a newly compiled dataset including 372 forest stands. We found that temperature and precipitation were key factors driving the nutrients stored in living biomass of forests at global scale. The N, K, and Mg stored in living biomass tended to be greater in increasingly warm climates. The mean biomass N density was 577.0, 530.4, 513.2, and 336.7 kg/ha for tropical, subtropical, temperate, and boreal forests, respectively. Around 76% of the variation in biomass N density could be accounted by the empirical model combining biomass density, phylogeny (i.e., angiosperm, gymnosperm), and the interaction of mean annual temperature and precipitation. Climate, stand age, and biomass density significantly affected nutrients partitioning at forest community level. The fractional distribution of nutrients to roots decreased significantly with temperature, suggesting that forests in cold climates allocate greater nutrients to roots. Gymnosperm forests tended to allocate more nutrients to leaves as compared with angiosperm forests, whereas the angiosperm forests distributed more nutrients in stems. The nutrient‐based Root:Shoot ratios (R:S), averaged 0.30 for R:S N , 0.36 for R:S P , 0.32 for R:S K , 0.27 for R:S Ca , and 0.35 for R:S Mg , respectively. The scaling exponents of the relationships describing root nutrients as a function of shoot nutrients were more than 1.0, suggesting that as nutrient allocated to shoot increases, nutrient allocated to roots increases faster than linearly with nutrient in shoot. Soil type significantly affected the total N, P, K, Ca, and Mg stored in living biomass of forests, and the Acrisols group displayed the lowest P, K, Ca, and Mg.
    Type of Medium: Online Resource
    ISSN: 1354-1013 , 1365-2486
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2018
    detail.hit.zdb_id: 2020313-5
    SSG: 12
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    In: Biological Conservation, Elsevier BV, Vol. 158 ( 2013-02), p. 205-213
    Type of Medium: Online Resource
    ISSN: 0006-3207
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2013
    detail.hit.zdb_id: 1496231-7
    SSG: 12
    SSG: 23
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    Online Resource
    Online Resource
    Elsevier BV ; 2013
    In:  Soil Biology and Biochemistry Vol. 57 ( 2013-02), p. 803-813
    In: Soil Biology and Biochemistry, Elsevier BV, Vol. 57 ( 2013-02), p. 803-813
    Type of Medium: Online Resource
    ISSN: 0038-0717
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2013
    detail.hit.zdb_id: 1498740-5
    detail.hit.zdb_id: 280810-9
    SSG: 12
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
    Online Resource
    Online Resource
    Wiley ; 2020
    In:  Global Ecology and Biogeography Vol. 29, No. 12 ( 2020-12), p. 2176-2189
    In: Global Ecology and Biogeography, Wiley, Vol. 29, No. 12 ( 2020-12), p. 2176-2189
    Abstract: Community‐level biomass‐to‐nutrient ratios and elemental stoichiometry of forests can provide insights for understanding the efficiency of nutrient use and the adaptation strategies of trees. However, the global‐scale pattern of biomass:N:K:Ca:Mg:P ratios in forest stands and its responses to environmental drivers remain unknown. Location World‐wide. Time period 1959–2015. Major taxa studied Trees in forests. Methods We synthesized data from 356 forests distributed globally to study the biogeographical variations in biomass‐to‐nutrient ratios and elemental stoichiometry. Results Our results revealed that the biomass:N, biomass:P, biomass:K, biomass:Ca and biomass:Mg ratios of living trees in forests averaged 330.2 ± 11.1, 3847.1 ± 164.6, 615.3 ± 26.1, 393.2 ± 15.0 and 2221.5 ± 92.0, respectively. The biomass:N, biomass:K, biomass:Mg, P:K, P:Mg and Ca:Mg ratios decreased with mean annual temperature and increased from low to high latitude, whereas the N:P and K:Ca ratios displayed the opposite trends. The biomass:P, N:P and K:Ca ratios increased significantly with increasing mean annual precipitation (MAP), whereas the P:K, P:Mg and Ca:Mg ratios decreased with the MAP. The biomass:N and biomass:Ca ratios decreased significantly with increasing soil N and Ca stocks, respectively. Forest stand age significantly affected biomass‐to‐nutrient ratios, with the older forests displaying higher biomass:N and biomass:P. The scaling relationships indicated that, on average, as biomass increased, biomass:N would increase, because N rose more slowly than linearly with biomass, whereas the Ca and Mg increased proportionally with biomass. Main conclusions Our findings proved that the community‐level biomass‐to‐nutrient ratios and stoichiometry were affected by climate, soil, stand age and taxonomy of trees.
    Type of Medium: Online Resource
    ISSN: 1466-822X , 1466-8238
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2020
    detail.hit.zdb_id: 1479787-2
    detail.hit.zdb_id: 2021283-5
    SSG: 12
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 5
    In: Global Change Biology, Wiley, Vol. 21, No. 7 ( 2015-07), p. 2762-2772
    Abstract: Knowledge of soil organic matter ( SOM ) dynamics following deforestation or reforestation is essential for evaluating carbon (C) budgets and cycle at regional or global scales. Worldwide land‐use changes involving conversion of vegetation with different photosynthetic pathways (e.g. C 3 and C 4 ) offer a unique opportunity to quantify SOM decomposition rate and its response to climatic conditions using stable isotope techniques. We synthesized the results from 131 sites (including 87 deforestation observations and 44 reforestation observations) which were compiled from 36 published papers in the literatures as well as our observations in China's Qinling Mountains. Based on the 13 C natural abundance analysis, we evaluated the dynamics of new and old C in top soil (0–20 cm) following land‐use change and analyzed the relationships between soil organic C ( SOC ) decomposition rates and climatic factors. We found that SOC decomposition rates increased significantly with mean annual temperature and precipitation in the reforestation sites, and they were not related to any climatic factor in deforestation sites. The mean annual temperature explained 56% of variation in SOC decomposition rates by exponential model ( y  = 0.0014 e 0.1395 x ) in the reforestation sites. The proportion of new soil C increased following deforestation and reforestation, whereas the old soil C showed an opposite trend. The proportion of new soil C exceeded the proportion of old soil C after 45.4 years' reforestation and 43.4 years' deforestation, respectively. The rates of new soil C accumulation increased significantly with mean annual precipitation and temperature in the reforestation sites, yet only significantly increased with mean annual precipitation in the deforestation sites. Overall, our study provides evidence that SOC decomposition rates vary with temperature and precipitation, and thereby implies that global warming may accelerate SOM decomposition.
    Type of Medium: Online Resource
    ISSN: 1354-1013 , 1365-2486
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2015
    detail.hit.zdb_id: 2020313-5
    SSG: 12
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...