Is there any relationship between phytoplankton seasonal dynamics and the carbonate system?

Production of calcium carbonate by marine calcifying organisms has been shown to decrease under increasing CO2. This effect appears to be driven by a decrease in [CO32-]. The modelling study here described aims at investigating whether the success of a marine calcifying phytoplankton species, the co...

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Published in:Journal of Marine Systems
Main Authors: Merico, A, Tyrrell, T, Cokacar, Tülay
Other Authors: ,, 2639972
Format: Article in Journal/Newspaper
Language:English
Published: 2021
Subjects:
Online Access:https://hdl.handle.net/20.500.12627/169883
https://doi.org/10.1016/j.jmarsys.2005.11.004
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author Merico, A
Tyrrell, T
Cokacar, Tülay
author2 , ,
2639972
author_facet Merico, A
Tyrrell, T
Cokacar, Tülay
author_sort Merico, A
collection İstanbul Üniversitesi Açık Erişim Sistemi
container_issue 1-2
container_start_page 120
container_title Journal of Marine Systems
container_volume 59
description Production of calcium carbonate by marine calcifying organisms has been shown to decrease under increasing CO2. This effect appears to be driven by a decrease in [CO32-]. The modelling study here described aims at investigating whether the success of a marine calcifying phytoplankton species, the coccolithophore Emiliania huxleyi, may be tied to [CO32-]. The work highlights the complex interactions between the carbonate system variables and spring blooms, and the possibility of a link to the competition between calcifying vs. non-calcifying species on the Bering Sea shelf. We find that the strong seasonal cycle in [CO32-] is driven primarily by carbon drawdown during spring blooms. The interesting outcome of this work is the fact that E. huxleyi bloom timings always coincide with periods of high [CO32-], which is consistent with studies showing coccoliths malformations and a slowdown in calcification at low [CO32-]. Whether the condition of high [CO32-] can be considered a crucial ecological factor for the success of E. huxleyi, however, remains an open and important question needing further investigation. (c) 2005 Elsevier B.V. All rights reserved.
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genre Bering Sea
genre_facet Bering Sea
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spelling ftistanbuluniv:oai:http://acikerisim.istanbul.edu.tr:20.500.12627/169883 2025-05-04T14:22:10+00:00 Is there any relationship between phytoplankton seasonal dynamics and the carbonate system? Merico, A Tyrrell, T Cokacar, Tülay , , 2639972 2021-12-10T10:26:32Z https://hdl.handle.net/20.500.12627/169883 https://doi.org/10.1016/j.jmarsys.2005.11.004 eng eng JOURNAL OF MARINE SYSTEMS vv_1032021 http://hdl.handle.net/20.500.12627/169883 https://doi.org/10.1016/j.jmarsys.2005.11.004 59 120 142 Oşinografi Fiziksel Oşinografi Jeoloji Mühendisliği Health Sciences YER BİLİMİ MULTİDİSİPLİNER Yerbilimleri Temel Bilimler (SCI) DENİZ VE TATLISU BİYOLOJİSİ Bitki ve Hayvan Bilimleri Tarım ve Çevre Bilimleri (AGE) OŞİNOGRAFİ JEOLOJİ Tarımsal Bilimler Ziraat Toprak ve Bitki Besleme Toprak ve Su Muhafazası ve Amenajmanı Su Hasadı Deniz Bilimleri ve Teknolojisi Mühendislik ve Teknoloji Oceanography Stratigraphy Geotechnical Engineering and Engineering Geology Geology Economic Geology Small Animals Physical Sciences Makale 2021 ftistanbuluniv https://doi.org/20.500.12627/16988310.1016/j.jmarsys.2005.11.004 2025-04-09T05:07:14Z Production of calcium carbonate by marine calcifying organisms has been shown to decrease under increasing CO2. This effect appears to be driven by a decrease in [CO32-]. The modelling study here described aims at investigating whether the success of a marine calcifying phytoplankton species, the coccolithophore Emiliania huxleyi, may be tied to [CO32-]. The work highlights the complex interactions between the carbonate system variables and spring blooms, and the possibility of a link to the competition between calcifying vs. non-calcifying species on the Bering Sea shelf. We find that the strong seasonal cycle in [CO32-] is driven primarily by carbon drawdown during spring blooms. The interesting outcome of this work is the fact that E. huxleyi bloom timings always coincide with periods of high [CO32-], which is consistent with studies showing coccoliths malformations and a slowdown in calcification at low [CO32-]. Whether the condition of high [CO32-] can be considered a crucial ecological factor for the success of E. huxleyi, however, remains an open and important question needing further investigation. (c) 2005 Elsevier B.V. All rights reserved. Article in Journal/Newspaper Bering Sea İstanbul Üniversitesi Açık Erişim Sistemi Bering Sea Journal of Marine Systems 59 1-2 120 142
spellingShingle Oşinografi
Fiziksel Oşinografi
Jeoloji Mühendisliği
Health Sciences
YER BİLİMİ
MULTİDİSİPLİNER
Yerbilimleri
Temel Bilimler (SCI)
DENİZ VE TATLISU BİYOLOJİSİ
Bitki ve Hayvan Bilimleri
Tarım ve Çevre Bilimleri (AGE)
OŞİNOGRAFİ
JEOLOJİ
Tarımsal Bilimler
Ziraat
Toprak ve Bitki Besleme
Toprak ve Su Muhafazası ve Amenajmanı
Su Hasadı
Deniz Bilimleri ve Teknolojisi
Mühendislik ve Teknoloji
Oceanography
Stratigraphy
Geotechnical Engineering and Engineering Geology
Geology
Economic Geology
Small Animals
Physical Sciences
Merico, A
Tyrrell, T
Cokacar, Tülay
Is there any relationship between phytoplankton seasonal dynamics and the carbonate system?
title Is there any relationship between phytoplankton seasonal dynamics and the carbonate system?
title_full Is there any relationship between phytoplankton seasonal dynamics and the carbonate system?
title_fullStr Is there any relationship between phytoplankton seasonal dynamics and the carbonate system?
title_full_unstemmed Is there any relationship between phytoplankton seasonal dynamics and the carbonate system?
title_short Is there any relationship between phytoplankton seasonal dynamics and the carbonate system?
title_sort is there any relationship between phytoplankton seasonal dynamics and the carbonate system?
topic Oşinografi
Fiziksel Oşinografi
Jeoloji Mühendisliği
Health Sciences
YER BİLİMİ
MULTİDİSİPLİNER
Yerbilimleri
Temel Bilimler (SCI)
DENİZ VE TATLISU BİYOLOJİSİ
Bitki ve Hayvan Bilimleri
Tarım ve Çevre Bilimleri (AGE)
OŞİNOGRAFİ
JEOLOJİ
Tarımsal Bilimler
Ziraat
Toprak ve Bitki Besleme
Toprak ve Su Muhafazası ve Amenajmanı
Su Hasadı
Deniz Bilimleri ve Teknolojisi
Mühendislik ve Teknoloji
Oceanography
Stratigraphy
Geotechnical Engineering and Engineering Geology
Geology
Economic Geology
Small Animals
Physical Sciences
topic_facet Oşinografi
Fiziksel Oşinografi
Jeoloji Mühendisliği
Health Sciences
YER BİLİMİ
MULTİDİSİPLİNER
Yerbilimleri
Temel Bilimler (SCI)
DENİZ VE TATLISU BİYOLOJİSİ
Bitki ve Hayvan Bilimleri
Tarım ve Çevre Bilimleri (AGE)
OŞİNOGRAFİ
JEOLOJİ
Tarımsal Bilimler
Ziraat
Toprak ve Bitki Besleme
Toprak ve Su Muhafazası ve Amenajmanı
Su Hasadı
Deniz Bilimleri ve Teknolojisi
Mühendislik ve Teknoloji
Oceanography
Stratigraphy
Geotechnical Engineering and Engineering Geology
Geology
Economic Geology
Small Animals
Physical Sciences
url https://hdl.handle.net/20.500.12627/169883
https://doi.org/10.1016/j.jmarsys.2005.11.004