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 in | Ecology and evolution Vol. 8; no. 4; pp. 2097 - 2107 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
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John Wiley & Sons, Inc
01.02.2018
John Wiley and Sons Inc Wiley |
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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. |
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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 – name: 1 Key Laboratory of Coastal Zone Environmental Processes and Ecological Remediation Yantai Institute of Coastal Zone Research Chinese Academy of Sciences Yantai Shandong China – 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 – name: 6 Laboratory of Marine Ecology and Environmental Science Qingdao National Laboratory for Marine Science and Technology Qingdao China – name: 2 Shandong Provincial Key Laboratory of Coastal Zone Environmental Processes Yantai Shandong China |
Author_xml | – sequence: 1 givenname: Zineng orcidid: 0000-0001-8824-6969 surname: Yuan fullname: Yuan, Zineng organization: Shandong Provincial Key Laboratory of Coastal Zone Environmental Processes – sequence: 2 givenname: Dongyan surname: Liu fullname: Liu, Dongyan email: dyliu@sklec.ecnu.edu.cn organization: East China Normal University – sequence: 3 givenname: John K. surname: Keesing fullname: Keesing, John K. organization: Indian Ocean Marine Research Centre – sequence: 4 givenname: Meixun surname: Zhao fullname: Zhao, Meixun organization: Qingdao National Laboratory for Marine Science and Technology – sequence: 5 givenname: Shixin surname: Guo fullname: Guo, Shixin organization: Qingdao National Laboratory for Marine Science and Technology – sequence: 6 givenname: Yajun surname: Peng fullname: Peng, Yajun organization: Guizhou University of Finance and Economics – sequence: 7 givenname: Hailong surname: Zhang fullname: Zhang, Hailong organization: Qingdao National Laboratory for Marine Science and Technology |
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CitedBy_id | crossref_primary_10_1007_s10113_022_01949_5 crossref_primary_10_3389_fmars_2022_904461 crossref_primary_10_3389_fmicb_2018_03356 crossref_primary_10_1016_j_ecolind_2021_107676 crossref_primary_10_1029_2019PA003712 crossref_primary_10_1029_2020PA004140 |
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Keywords | ocean warming diatom Cygnet Bay dinoflagellate biomarkers TEX86H |
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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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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 |
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