CVClient

Yu Hirano

  (平野 侑)

Profile Information

Affiliation
Assistant Professor, School of Human Science and Environment, University of Hyogo
Degree
Ph.D.(Mar, 2024, Tokyo University of Agriculture)

ORCID ID
 https://orcid.org/0000-0002-2372-0153
J-GLOBAL ID
202401015172202627
researchmap Member ID
R000070483

私は、マレーシア・ボルネオ島の熱帯雨林をメインサイトとして、樹木生理生態学および生態系生態学に関する実証研究を行なってきました。特にマレーシアでは、生態生理学的特性から熱帯樹種の適応メカニズムを理解すること、そして熱帯生態系に特徴的な高い種多様性と非常に大きなバイオマスを維持するメカニズムを解明していきたいと考えています。また国内でも、マングローブや温帯二次林、高山生態系などで、葉形質と被食率の関係性、根の生理学的特性(根滲出速度や細根由来の酵素活性、栄養塩吸収速度など)に関する研究を行なってきています。


Committee Memberships

 1

Papers

 3
  • Yu R. Hirano, Naoki Makita, Ko Hinokidani, Ryota Aoyagi, Nobuo Imai
    Ecosystems, 28, Oct, 2025  Peer-reviewedLead authorCorresponding author
  • Yu Hirano, Motoki Marui, Shuhei Tachikake, Taku Kato, Nobuo Imai
    Journal of Forest Research, 29(3) 204-213, Nov 12, 2023  Peer-reviewedLead author
  • Yu Hirano, Kanehiro Kitayama, Nobuo Imai
    Ecology and Evolution, 12(3), Mar 7, 2022  Peer-reviewedLead author
    Abstract Soil organic phosphorus (P) compounds can be the main P source for plants in P‐limited tropical rainforests. Phosphorus occurs in diverse chemical forms, including monoester P, diester P, and phytate, which require enzymatic hydrolysis by phosphatase into inorganic P before assimilation by plants. The interactions between plant interspecific differences in organic P acquisition strategies via phosphatase activities with root morphological traits would lead to P resource partitioning, but they have not been rigorously evaluated. We measured the activities of three classes of phosphatases (phosphomonoesterase, PME; phosphodiesterase, PDE; and phytase, PhT), specific root length (SRL), root diameter, and root tissue density in mature tree species with different mycorrhizal associations (ectomycorrhizal [ECM] or arbuscular mycorrhizal [AM]) and different successional status (climax or pioneer species) in Sabah, Malaysia. We studied nitrogen (N)‐ and P‐fertilized plots to evaluate the acquisition strategies for organic P under P‐limited conditions 7 years after fertilization was initiated. P fertilization reduced the PME activity in all studied species and reduced PhT and PDE activities more in climax species than in the two pioneer species, irrespective of the mycorrhizal type. PDE activity increased in some climax species after N fertilization, suggesting that these species allocate excess N to the synthesis of PDE. Moreover, PME and PhT activities, but not PDE activity, correlated positively with SRL. We suggest that climax species tend to be more strongly dependent on recalcitrant organic P (i.e., phytate and/or diester P) than pioneer species, regardless of the mycorrhizal type. We also suggest that trees in which root PME or PhT activity is enhanced can increase their SRL to acquire P efficiently. Resource partitioning of soil organic P would occur among species through differences in their phosphatase activities, which plays potentially ecologically important role in reducing the competition among coexisting tree species in lowland tropical rainforests.

Misc.

 2

Books and Other Publications

 1

Professional Memberships

 5

Research Projects

 5