Thermal acclimation and adaptation of key phytoplankton groups and interactions with other global change variables ...

Several functional groups of marine phytoplankton groups play especially critical roles in global primary productivity, carbon export and biogeochemistry. In particular, diatoms substantially contribute to primary production, carbon sequestration and the food web. Diazotrophic cyanobacteria are equa...

Full description

Bibliographic Details
Main Author: Qu, Pingping author
Format: Thesis
Language:English
Published: University of Southern California Digital Library (USC.DL) 2019
Subjects:
Online Access:https://dx.doi.org/10.25549/usctheses-c89-184704
https://digitallibrary.usc.edu/asset-management/2A3BF1WJEKX3
id ftdatacite:10.25549/usctheses-c89-184704
record_format openpolar
spelling ftdatacite:10.25549/usctheses-c89-184704 2024-03-31T07:54:46+00:00 Thermal acclimation and adaptation of key phytoplankton groups and interactions with other global change variables ... Qu, Pingping author 2019 https://dx.doi.org/10.25549/usctheses-c89-184704 https://digitallibrary.usc.edu/asset-management/2A3BF1WJEKX3 en eng University of Southern California Digital Library (USC.DL) Biology Marine Biology and Biological Oceanography degree program Doctor of Philosophy degree College of Letters, Arts and Sciences school thesis Dissertation Thesis 2019 ftdatacite https://doi.org/10.25549/usctheses-c89-184704 2024-03-04T12:39:54Z Several functional groups of marine phytoplankton groups play especially critical roles in global primary productivity, carbon export and biogeochemistry. In particular, diatoms substantially contribute to primary production, carbon sequestration and the food web. Diazotrophic cyanobacteria are equally important as a source of new nitrogen (N) through nitrogen fixation. The relationship between environmental forcing and these key marine phytoplankton groups needs more attention, especially in the context of future global change. ? Elevated atmospheric concentrations of the greenhouse gas carbon dioxide (CO?) are bringing about ocean acidification and giving rise to sea surface warming. By the end of this century, atmospheric CO? concentration is predicted to rise from current levels of ?415 parts per million (ppm) to 800-1150 ppm, while average surface seawater temperatures will increase by 2-4?. Global warming will also result in indirect changes, such as intensified stratification of seawater, increased ... Thesis Ocean acidification DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Biology Marine Biology and Biological Oceanography degree program
Doctor of Philosophy degree
College of Letters, Arts and Sciences school
spellingShingle Biology Marine Biology and Biological Oceanography degree program
Doctor of Philosophy degree
College of Letters, Arts and Sciences school
Qu, Pingping author
Thermal acclimation and adaptation of key phytoplankton groups and interactions with other global change variables ...
topic_facet Biology Marine Biology and Biological Oceanography degree program
Doctor of Philosophy degree
College of Letters, Arts and Sciences school
description Several functional groups of marine phytoplankton groups play especially critical roles in global primary productivity, carbon export and biogeochemistry. In particular, diatoms substantially contribute to primary production, carbon sequestration and the food web. Diazotrophic cyanobacteria are equally important as a source of new nitrogen (N) through nitrogen fixation. The relationship between environmental forcing and these key marine phytoplankton groups needs more attention, especially in the context of future global change. ? Elevated atmospheric concentrations of the greenhouse gas carbon dioxide (CO?) are bringing about ocean acidification and giving rise to sea surface warming. By the end of this century, atmospheric CO? concentration is predicted to rise from current levels of ?415 parts per million (ppm) to 800-1150 ppm, while average surface seawater temperatures will increase by 2-4?. Global warming will also result in indirect changes, such as intensified stratification of seawater, increased ...
format Thesis
author Qu, Pingping author
author_facet Qu, Pingping author
author_sort Qu, Pingping author
title Thermal acclimation and adaptation of key phytoplankton groups and interactions with other global change variables ...
title_short Thermal acclimation and adaptation of key phytoplankton groups and interactions with other global change variables ...
title_full Thermal acclimation and adaptation of key phytoplankton groups and interactions with other global change variables ...
title_fullStr Thermal acclimation and adaptation of key phytoplankton groups and interactions with other global change variables ...
title_full_unstemmed Thermal acclimation and adaptation of key phytoplankton groups and interactions with other global change variables ...
title_sort thermal acclimation and adaptation of key phytoplankton groups and interactions with other global change variables ...
publisher University of Southern California Digital Library (USC.DL)
publishDate 2019
url https://dx.doi.org/10.25549/usctheses-c89-184704
https://digitallibrary.usc.edu/asset-management/2A3BF1WJEKX3
genre Ocean acidification
genre_facet Ocean acidification
op_doi https://doi.org/10.25549/usctheses-c89-184704
_version_ 1795035943214776320