Paleoecological evidence for decadal increase in phytoplankton biomass off northwestern Australia in response to climate change

Ocean warming can modify the phytoplankton biomass on decadal scales. Significant increases in sea surface temperature (SST) and rainfall in the northwest of Australia over recent decades are attributed to climate change. Here, we used four biomarker proxies (TEX86 index, long‐chain n‐alkanes, brass...

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Published inEcology and evolution Vol. 8; no. 4; pp. 2097 - 2107
Main Authors Yuan, Zineng, Liu, Dongyan, Keesing, John K., Zhao, Meixun, Guo, Shixin, Peng, Yajun, Zhang, Hailong
Format Journal Article
LanguageEnglish
Published England John Wiley & Sons, Inc 01.02.2018
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Abstract Ocean warming can modify the phytoplankton biomass on decadal scales. Significant increases in sea surface temperature (SST) and rainfall in the northwest of Australia over recent decades are attributed to climate change. Here, we used four biomarker proxies (TEX86 index, long‐chain n‐alkanes, brassicasterol, and dinosterol) to reconstruct approximately 60‐year variations of SST, terrestrial input, and diatom and dinoflagellate biomass in the coastal waters of the remote Kimberley region. The results showed that the most significant increases in SST and terrestrial input occurred since 1997, accompanied by an abrupt increase in diatom and dinoflagellate biomasses. Compared with the results before 1997, the average TEX86H temperature during 1997–2011 increased approximately 1°C, rainfall increased 248.2 mm, brassicasterol and dinosterol contents increased 8.5 and 1.7 times. Principal component analysis indicated that the warming SST played a more important role in the phytoplankton increase than increased rainfall and river discharge. An abrupt increase in phytoplankton occurred since the 1990s, accompanied by significant increases in temperature and terrestrial input. Warming temperature played a more important role for the decadal phytoplankton increase than rainfall. Applicability of TEX86H biomarker proxy for SST off northwestern Australia was validated.
AbstractList AbstractOcean warming can modify the phytoplankton biomass on decadal scales. Significant increases in sea surface temperature (SST) and rainfall in the northwest of Australia over recent decades are attributed to climate change. Here, we used four biomarker proxies (TEX86 index, long‐chain n‐alkanes, brassicasterol, and dinosterol) to reconstruct approximately 60‐year variations of SST, terrestrial input, and diatom and dinoflagellate biomass in the coastal waters of the remote Kimberley region. The results showed that the most significant increases in SST and terrestrial input occurred since 1997, accompanied by an abrupt increase in diatom and dinoflagellate biomasses. Compared with the results before 1997, the average TEX86H temperature during 1997–2011 increased approximately 1°C, rainfall increased 248.2 mm, brassicasterol and dinosterol contents increased 8.5 and 1.7 times. Principal component analysis indicated that the warming SST played a more important role in the phytoplankton increase than increased rainfall and river discharge.
Ocean warming can modify the phytoplankton biomass on decadal scales. Significant increases in sea surface temperature (SST) and rainfall in the northwest of Australia over recent decades are attributed to climate change. Here, we used four biomarker proxies (TEX86 index, long-chain n-alkanes, brassicasterol, and dinosterol) to reconstruct approximately 60-year variations of SST, terrestrial input, and diatom and dinoflagellate biomass in the coastal waters of the remote Kimberley region. The results showed that the most significant increases in SST and terrestrial input occurred since 1997, accompanied by an abrupt increase in diatom and dinoflagellate biomasses. Compared with the results before 1997, the average TEX86H temperature during 1997-2011 increased approximately 1°C, rainfall increased 248.2 mm, brassicasterol and dinosterol contents increased 8.5 and 1.7 times. Principal component analysis indicated that the warming SST played a more important role in the phytoplankton increase than increased rainfall and river discharge.Ocean warming can modify the phytoplankton biomass on decadal scales. Significant increases in sea surface temperature (SST) and rainfall in the northwest of Australia over recent decades are attributed to climate change. Here, we used four biomarker proxies (TEX86 index, long-chain n-alkanes, brassicasterol, and dinosterol) to reconstruct approximately 60-year variations of SST, terrestrial input, and diatom and dinoflagellate biomass in the coastal waters of the remote Kimberley region. The results showed that the most significant increases in SST and terrestrial input occurred since 1997, accompanied by an abrupt increase in diatom and dinoflagellate biomasses. Compared with the results before 1997, the average TEX86H temperature during 1997-2011 increased approximately 1°C, rainfall increased 248.2 mm, brassicasterol and dinosterol contents increased 8.5 and 1.7 times. Principal component analysis indicated that the warming SST played a more important role in the phytoplankton increase than increased rainfall and river discharge.
Abstract Ocean warming can modify the phytoplankton biomass on decadal scales. Significant increases in sea surface temperature (SST) and rainfall in the northwest of Australia over recent decades are attributed to climate change. Here, we used four biomarker proxies (TEX86 index, long‐chain n‐alkanes, brassicasterol, and dinosterol) to reconstruct approximately 60‐year variations of SST, terrestrial input, and diatom and dinoflagellate biomass in the coastal waters of the remote Kimberley region. The results showed that the most significant increases in SST and terrestrial input occurred since 1997, accompanied by an abrupt increase in diatom and dinoflagellate biomasses. Compared with the results before 1997, the average TEX86H temperature during 1997–2011 increased approximately 1°C, rainfall increased 248.2 mm, brassicasterol and dinosterol contents increased 8.5 and 1.7 times. Principal component analysis indicated that the warming SST played a more important role in the phytoplankton increase than increased rainfall and river discharge.
Ocean warming can modify the phytoplankton biomass on decadal scales. Significant increases in sea surface temperature (SST) and rainfall in the northwest of Australia over recent decades are attributed to climate change. Here, we used four biomarker proxies (TEX 86 index, long‐chain n ‐alkanes, brassicasterol, and dinosterol) to reconstruct approximately 60‐year variations of SST, terrestrial input, and diatom and dinoflagellate biomass in the coastal waters of the remote Kimberley region. The results showed that the most significant increases in SST and terrestrial input occurred since 1997, accompanied by an abrupt increase in diatom and dinoflagellate biomasses. Compared with the results before 1997, the average TEX 86 H temperature during 1997–2011 increased approximately 1°C, rainfall increased 248.2 mm, brassicasterol and dinosterol contents increased 8.5 and 1.7 times. Principal component analysis indicated that the warming SST played a more important role in the phytoplankton increase than increased rainfall and river discharge.
Ocean warming can modify the phytoplankton biomass on decadal scales. Significant increases in sea surface temperature (SST) and rainfall in the northwest of Australia over recent decades are attributed to climate change. Here, we used four biomarker proxies (TEX 86 index, long‐chain n ‐alkanes, brassicasterol, and dinosterol) to reconstruct approximately 60‐year variations of SST, terrestrial input, and diatom and dinoflagellate biomass in the coastal waters of the remote Kimberley region. The results showed that the most significant increases in SST and terrestrial input occurred since 1997, accompanied by an abrupt increase in diatom and dinoflagellate biomasses. Compared with the results before 1997, the average temperature during 1997–2011 increased approximately 1°C, rainfall increased 248.2 mm, brassicasterol and dinosterol contents increased 8.5 and 1.7 times. Principal component analysis indicated that the warming SST played a more important role in the phytoplankton increase than increased rainfall and river discharge.
Ocean warming can modify the phytoplankton biomass on decadal scales. Significant increases in sea surface temperature (SST) and rainfall in the northwest of Australia over recent decades are attributed to climate change. Here, we used four biomarker proxies (TEX86 index, long‐chain n‐alkanes, brassicasterol, and dinosterol) to reconstruct approximately 60‐year variations of SST, terrestrial input, and diatom and dinoflagellate biomass in the coastal waters of the remote Kimberley region. The results showed that the most significant increases in SST and terrestrial input occurred since 1997, accompanied by an abrupt increase in diatom and dinoflagellate biomasses. Compared with the results before 1997, the average TEX86H temperature during 1997–2011 increased approximately 1°C, rainfall increased 248.2 mm, brassicasterol and dinosterol contents increased 8.5 and 1.7 times. Principal component analysis indicated that the warming SST played a more important role in the phytoplankton increase than increased rainfall and river discharge. An abrupt increase in phytoplankton occurred since the 1990s, accompanied by significant increases in temperature and terrestrial input. Warming temperature played a more important role for the decadal phytoplankton increase than rainfall. Applicability of TEX86H biomarker proxy for SST off northwestern Australia was validated.
Ocean warming can modify the phytoplankton biomass on decadal scales. Significant increases in sea surface temperature (SST) and rainfall in the northwest of Australia over recent decades are attributed to climate change. Here, we used four biomarker proxies (TEX index, long-chain -alkanes, brassicasterol, and dinosterol) to reconstruct approximately 60-year variations of SST, terrestrial input, and diatom and dinoflagellate biomass in the coastal waters of the remote Kimberley region. The results showed that the most significant increases in SST and terrestrial input occurred since 1997, accompanied by an abrupt increase in diatom and dinoflagellate biomasses. Compared with the results before 1997, the average TEX86H temperature during 1997-2011 increased approximately 1°C, rainfall increased 248.2 mm, brassicasterol and dinosterol contents increased 8.5 and 1.7 times. Principal component analysis indicated that the warming SST played a more important role in the phytoplankton increase than increased rainfall and river discharge.
Author Yuan, Zineng
Liu, Dongyan
Zhang, Hailong
Keesing, John K.
Peng, Yajun
Guo, Shixin
Zhao, Meixun
AuthorAffiliation 4 CSIRO Oceans and Atmosphere Research University of Western Australia Oceans Institute Western Australian Marine Science Institution Indian Ocean Marine Research Centre Crawley WA Australia
2 Shandong Provincial Key Laboratory of Coastal Zone Environmental Processes Yantai Shandong China
1 Key Laboratory of Coastal Zone Environmental Processes and Ecological Remediation Yantai Institute of Coastal Zone Research Chinese Academy of Sciences Yantai Shandong China
6 Laboratory of Marine Ecology and Environmental Science Qingdao National Laboratory for Marine Science and Technology Qingdao China
5 Key Laboratory of Marine Chemistry Theory and Technology Ocean University of China Ministry of Education Qingdao China
3 State Key Laboratory of Estuarine and Coastal Research East China Normal University Shanghai China
7 School of Management Science Guizhou University of Finance and Economics Guiyang Guizhou China
AuthorAffiliation_xml – name: 3 State Key Laboratory of Estuarine and Coastal Research East China Normal University Shanghai China
– name: 5 Key Laboratory of Marine Chemistry Theory and Technology Ocean University of China Ministry of Education Qingdao China
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– name: 7 School of Management Science Guizhou University of Finance and Economics Guiyang Guizhou China
– name: 4 CSIRO Oceans and Atmosphere Research University of Western Australia Oceans Institute Western Australian Marine Science Institution Indian Ocean Marine Research Centre Crawley WA Australia
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Issue 4
Keywords ocean warming
diatom
Cygnet Bay
dinoflagellate
biomarkers
TEX86H
Language English
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SSID ssj0000602407
Score 2.145357
Snippet Ocean warming can modify the phytoplankton biomass on decadal scales. Significant increases in sea surface temperature (SST) and rainfall in the northwest of...
AbstractOcean warming can modify the phytoplankton biomass on decadal scales. Significant increases in sea surface temperature (SST) and rainfall in the...
Abstract Ocean warming can modify the phytoplankton biomass on decadal scales. Significant increases in sea surface temperature (SST) and rainfall in the...
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pubmedcentral
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SourceType Open Website
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StartPage 2097
SubjectTerms Alkanes
Aquaculture
Biomarkers
Biomass
Climate change
Coastal waters
Cygnet Bay
diatom
dinoflagellate
Dinoflagellates
Ecosystems
Glycerol
Grain size
Lipids
Microorganisms
Ocean temperature
Ocean warming
Original Research
Paleoecology
Phytoplankton
Plankton
Principal components analysis
Proxies
Rainfall
River discharge
River flow
Rivers
Sea surface temperature
Sedimentation & deposition
Sediments
Sterols
TEX 86 H
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Title Paleoecological evidence for decadal increase in phytoplankton biomass off northwestern Australia in response to climate change
URI https://onlinelibrary.wiley.com/doi/abs/10.1002%2Fece3.3836
https://www.ncbi.nlm.nih.gov/pubmed/29468028
https://www.proquest.com/docview/2007131600
https://www.proquest.com/docview/2513392223
https://www.proquest.com/docview/2007421156
https://pubmed.ncbi.nlm.nih.gov/PMC5817135
https://doaj.org/article/3fd08431fee948d486d586b778864143
Volume 8
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