z-logo
open-access-imgOpen Access
Nutrient co‐limitation in the subtropical Northwest Pacific
Author(s) -
Browning Thomas J.,
Liu Xin,
Zhang Ruifeng,
Wen Zuozhu,
Liu Jing,
Zhou Yaqian,
Xu Feipeng,
Cai Yihua,
Zhou Kuanbo,
Cao Zhimian,
Zhu Yuanli,
Shi Dalin,
Achterberg Eric P.,
Dai Minhan
Publication year - 2022
Publication title -
limnology and oceanography letters
Language(s) - English
Resource type - Journals
ISSN - 2378-2242
DOI - 10.1002/lol2.10205
Subject(s) - phytoplankton , nutrient , environmental science , oceanography , nitrogen , productivity , biomass (ecology) , phosphorus , chlorophyll a , subtropics , limiting , iron fertilization , ecology , biology , chemistry , botany , geology , mechanical engineering , engineering , macroeconomics , organic chemistry , economics
Nutrients limiting phytoplankton growth in the ocean are a critical control on ocean productivity and can underpin predicted responses to climate change. The extensive western subtropical North Pacific is assumed to be under strong nitrogen limitation, but this is not well supported by experimental evidence. Here, we report the results of 14 factorial nitrogen–phosphorus–iron addition experiments through the Philippine Sea, which demonstrate a gradient from nitrogen limitation in the north to nitrogen–iron co‐limitation in the south. While nitrogen limited sites responded weakly to nutrient supply, co‐limited sites bloomed with up to ~60‐fold increases in chlorophyll a biomass that was dominated by initially undetectable diatoms. The transition in limiting nutrients and phytoplankton growth capacity was driven by a gradient in deep water nutrient supply, which was undetectable in surface concentration fields. We hypothesize that this large‐scale phytoplankton response gradient is both climate sensitive and potentially important for regulating the distribution of predatory fish.

The content you want is available to Zendy users.

Already have an account? Click here to sign in.
Having issues? You can contact us here