Distribution, ecology, and oxygen and carbon isotope characteristics of modern planktonic foraminifers in the Makarov Basin of the Arctic Ocean
The Arctic region, with magnificent ice cover on the surface of the Arctic Ocean and adjacent seas, is not only extremely sensitive to but also has strong amplifica- tion effects on climate change. Observations during the past decades have documented substantial retreat and thinning of the Arctic se...
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| Published in | Chinese science bulletin Vol. 59; no. 7; pp. 674 - 687 |
|---|---|
| Main Authors | , , , |
| Format | Journal Article |
| Language | English |
| Published |
Dordrecht
Springer-Verlag
01.03.2014
Science China Press |
| Subjects | |
| Online Access | Get full text |
| ISSN | 1001-6538 1861-9541 |
| DOI | 10.1007/s11434-013-0082-8 |
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| Abstract | The Arctic region, with magnificent ice cover on the surface of the Arctic Ocean and adjacent seas, is not only extremely sensitive to but also has strong amplifica- tion effects on climate change. Observations during the past decades have documented substantial retreat and thinning of the Arctic sea-ice cover, a process that is accelerating. Its feedback and impact on the global climate has become an important subject of current climate change research. Calcite tests of planktonic foraminifers are major constituents in pelagic sediments, and they provide valu- able materials for the reconstruction of past oceanographic conditions. However, research is still sparse in the Arctic sea area because of limited availability of the materials for investigation. Here, we present a study of modem fora- minifers from the plankton tow samples taken in the Makarov Basin of the Arctic Ocean during the fourth Arctic expedition of China. We have analyzed ecological information stored in the modem planktonic foraminifers and in their stable isotope signals, and established a rela- tionship between the distribution of the main taxa and theenvironment. Our main observations are as follows： （1） in the Makarov Basin, the polar species Neogloboquadrina pachyderma （sinistral coiling） dominates the 〉150 μm planktonic foraminiferal assemblages. （2） The planktonic foraminifers live mainly in the upper halocline at a water depth of 50-100 m and less in the depth interval of 100-200 m. （3） Temperature change in the halocline can affect the absolute abundance of planktonic foraminifers and their distribution in the water column. The warmer halocline is more favorable to the development of plank- tonic foraminifers. （4） A lighter 6180 value （2.11‰） of N. pachyderma （sin.） is recorded in the depth interval of 100-200 m, which is likely related to the isotopically light brines separated out during sea ice freezing. The relatively heavy δ18O value （1.68 ‰-2.68‰, average 2.27‰） in the depth interval of 50-100 m may be influenced by the low salinity water with the relatively heavy δ18O value formed during the sea-ice melting in the surface layer. |
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| AbstractList | The Arctic region, with magnificent ice cover on the surface of the Arctic Ocean and adjacent seas, is not only extremely sensitive to but also has strong amplifica- tion effects on climate change. Observations during the past decades have documented substantial retreat and thinning of the Arctic sea-ice cover, a process that is accelerating. Its feedback and impact on the global climate has become an important subject of current climate change research. Calcite tests of planktonic foraminifers are major constituents in pelagic sediments, and they provide valu- able materials for the reconstruction of past oceanographic conditions. However, research is still sparse in the Arctic sea area because of limited availability of the materials for investigation. Here, we present a study of modem fora- minifers from the plankton tow samples taken in the Makarov Basin of the Arctic Ocean during the fourth Arctic expedition of China. We have analyzed ecological information stored in the modem planktonic foraminifers and in their stable isotope signals, and established a rela- tionship between the distribution of the main taxa and theenvironment. Our main observations are as follows： （1） in the Makarov Basin, the polar species Neogloboquadrina pachyderma （sinistral coiling） dominates the 〉150 μm planktonic foraminiferal assemblages. （2） The planktonic foraminifers live mainly in the upper halocline at a water depth of 50-100 m and less in the depth interval of 100-200 m. （3） Temperature change in the halocline can affect the absolute abundance of planktonic foraminifers and their distribution in the water column. The warmer halocline is more favorable to the development of plank- tonic foraminifers. （4） A lighter 6180 value （2.11‰） of N. pachyderma （sin.） is recorded in the depth interval of 100-200 m, which is likely related to the isotopically light brines separated out during sea ice freezing. The relatively heavy δ18O value （1.68 ‰-2.68‰, average 2.27‰） in the depth interval of 50-100 m may be influenced by the low salinity water with the relatively heavy δ18O value formed during the sea-ice melting in the surface layer. The Arctic region, with magnificent ice cover on the surface of the Arctic Ocean and adjacent seas, is not only extremely sensitive to but also has strong amplification effects on climate change. Observations during the past decades have documented substantial retreat and thinning of the Arctic sea-ice cover, a process that is accelerating. Its feedback and impact on the global climate has become an important subject of current climate change research. Calcite tests of planktonic foraminifers are major constituents in pelagic sediments, and they provide valuable materials for the reconstruction of past oceanographic conditions. However, research is still sparse in the Arctic sea area because of limited availability of the materials for investigation. Here, we present a study of modern foraminifers from the plankton tow samples taken in the Makarov Basin of the Arctic Ocean during the fourth Arctic expedition of China. We have analyzed ecological information stored in the modern planktonic foraminifers and in their stable isotope signals, and established a relationship between the distribution of the main taxa and the environment. Our main observations are as follows: (1) in the Makarov Basin, the polar species Neogloboquadrina pachyderma (sinistral coiling) dominates the >150 μm planktonic foraminiferal assemblages. (2) The planktonic foraminifers live mainly in the upper halocline at a water depth of 50–100 m and less in the depth interval of 100–200 m. (3) Temperature change in the halocline can affect the absolute abundance of planktonic foraminifers and their distribution in the water column. The warmer halocline is more favorable to the development of planktonic foraminifers. (4) A lighter δ 18 O value (2.11 ‰) of N. pachyderma (sin.) is recorded in the depth interval of 100–200 m, which is likely related to the isotopically light brines separated out during sea ice freezing. The relatively heavy δ 18 O value (1.68 ‰–2.68 ‰, average 2.27 ‰) in the depth interval of 50–100 m may be influenced by the low salinity water with the relatively heavy δ 18 O value formed during the sea-ice melting in the surface layer. The Arctic region, with magnificent ice cover on the surface of the Arctic Ocean and adjacent seas, is not only extremely sensitive to but also has strong amplification effects on climate change. Observations during the past decades have documented substantial retreat and thinning of the Arctic sea-ice cover, a process that is accelerating. Its feedback and impact on the global climate has become an important subject of current climate change research. Calcite tests of planktonic foraminifers are major constituents in pelagic sediments, and they provide valuable materials for the reconstruction of past oceanographic conditions. However, research is still sparse in the Arctic sea area because of limited availability of the materials for investigation. Here, we present a study of modern foraminifers from the plankton tow samples taken in the Makarov Basin of the Arctic Ocean during the fourth Arctic expedition of China. We have analyzed ecological information stored in the modern planktonic foraminifers and in their stable isotope signals, and established a relationship between the distribution of the main taxa and the environment. Our main observations are as follows: (1) in the Makarov Basin, the polar species Neogloboquadrina pachyderma (sinistral coiling) dominates the >150 μm planktonic foraminiferal assemblages. (2) The planktonic foraminifers live mainly in the upper halocline at a water depth of 50–100 m and less in the depth interval of 100–200 m. (3) Temperature change in the halocline can affect the absolute abundance of planktonic foraminifers and their distribution in the water column. The warmer halocline is more favorable to the development of planktonic foraminifers. (4) A lighter δ¹⁸O value (2.11 ‰) of N. pachyderma (sin.) is recorded in the depth interval of 100–200 m, which is likely related to the isotopically light brines separated out during sea ice freezing. The relatively heavy δ¹⁸O value (1.68 ‰–2.68 ‰, average 2.27 ‰) in the depth interval of 50–100 m may be influenced by the low salinity water with the relatively heavy δ¹⁸O value formed during the sea-ice melting in the surface layer. The Arctic region, with magnificent ice cover on the surface of the Arctic Ocean and adjacent seas, is not only extremely sensitive to but also has strong amplification effects on climate change. Observations during the past decades have documented substantial retreat and thinning of the Arctic sea-ice cover, a process that is accelerating. Its feedback and impact on the global climate has become an important subject of current climate change research. Calcite tests of planktonic foraminifers are major constituents in pelagic sediments, and they provide valuable materials for the reconstruction of past oceanographic conditions. However, research is still sparse in the Arctic sea area because of limited availability of the materials for investigation. Here, we present a study of modern foraminifers from the plankton tow samples taken in the Makarov Basin of the Arctic Ocean during the fourth Arctic expedition of China. We have analyzed ecological information stored in the modern planktonic foraminifers and in their stable isotope signals, and established a relationship between the distribution of the main taxa and the environment. Our main observations are as follows: (1) in the Makarov Basin, the polar species Neogloboquadrina pachyderma (sinistral coiling) dominates the >150 μm planktonic foraminiferal assemblages. (2) The planktonic foraminifers live mainly in the upper halocline at a water depth of 50–100 m and less in the depth interval of 100–200 m. (3) Temperature change in the halocline can affect the absolute abundance of planktonic foraminifers and their distribution in the water column. The warmer halocline is more favorable to the development of planktonic foraminifers. (4) A lighter δ ¹⁸O value (2.11 ‰) of N. pachyderma (sin.) is recorded in the depth interval of 100–200 m, which is likely related to the isotopically light brines separated out during sea ice freezing. The relatively heavy δ ¹⁸O value (1.68 ‰–2.68 ‰, average 2.27 ‰) in the depth interval of 50–100 m may be influenced by the low salinity water with the relatively heavy δ ¹⁸O value formed during the sea-ice melting in the surface layer. The Arctic region, with magnificent ice cover on the surface of the Arctic Ocean and adjacent seas, is not only extremely sensitive to but also has strong amplification effects on climate change. Observations during the past decades have documented substantial retreat and thinning of the Arctic sea-ice cover, a process that is accelerating. Its feedback and impact on the global climate has become an important subject of current climate change research. Calcite tests of planktonic foraminifers are major constituents in pelagic sediments, and they provide valuable materials for the reconstruction of past oceanographic conditions. However, research is still sparse in the Arctic sea area because of limited availability of the materials for investigation. Here, we present a study of modern foraminifers from the plankton tow samples taken in the Makarov Basin of the Arctic Ocean during the fourth Arctic expedition of China. We have analyzed ecological information stored in the modern planktonic foraminifers and in their stable isotope signals, and established a relationship between the distribution of the main taxa and the environment. Our main observations are as follows: (1) in the Makarov Basin, the polar species Neogloboquadrina pachyderma (sinistral coiling) dominates the >150 mu m planktonic foraminiferal assemblages. (2) The planktonic foraminifers live mainly in the upper halocline at a water depth of 50-100 m and less in the depth interval of 100-200 m. (3) Temperature change in the halocline can affect the absolute abundance of planktonic foraminifers and their distribution in the water column. The warmer halocline is more favorable to the development of planktonic foraminifers. (4) A lighter delta 18O value (2.11 ppt) of N. pachyderma (sin.) is recorded in the depth interval of 100-200 m, which is likely related to the isotopically light brines separated out during sea ice freezing. The relatively heavy delta 18O value (1.68 ppt-2.68 ppt, average 2.27 ppt) in the depth interval of 50-100 m may be influenced by the low salinity water with the relatively heavy delta 18O value formed during the sea-ice melting in the surface layer. |
| Author | Tao, Zhencheng Zhang, Haifeng Ding, Xuan Wang, Rujian |
| AuthorAffiliation | School of Marine Sciences, China University of Geosciences,Beijing 100083, China State Key Laboratory of Marine Geology, Tongji University,Shanghai 200092, China The Second Institute of Oceanography, SOA, Hangzhou 310012,China Institute of Oceanology, Chinese Academy of Sciences,Qingdao 266071, China |
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| CitedBy_id | crossref_primary_10_1029_2020JC016144 crossref_primary_10_1016_j_margeo_2014_03_024 |
| Cites_doi | 10.1016/S0012-821X(96)00211-7 10.1016/0079-6611(89)90013-X 10.2113/0300157 10.1144/0262-821X11-030 10.1016/j.quascirev.2010.02.010 10.1029/2009GL037274 10.1016/S0924-7963(00)00009-9 10.1029/96PA02753 10.1016/S0967-0645(97)00055-6 10.1016/S0277-3791(97)00067-X 10.1016/0012-821X(70)90109-3 10.1016/j.quascirev.2010.02.008 10.1360/972011-913 10.1029/96PA02617 10.1111/j.1751-8369.2001.tb00049.x 10.1016/0198-0149(81)90115-1 10.1175/JCLI3967.1 10.1029/1999JC000024 10.1029/JC090iC03p04833 10.1016/S0198-0149(06)80018-X 10.1016/j.gloplacha.2011.03.004 10.1016/j.epsl.2008.01.012 10.1088/1755-1315/14/1/012005 10.1016/0198-0149(89)90048-4 10.1016/0025-3227(94)90183-X 10.1016/S0377-8398(96)00014-X 10.1029/2007JC004253 10.1029/2006GL028024 |
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| Notes | Arctic Ocean · Makarov Basin ·Plankton tow · Planktonic foraminifers · Oxygen andcarbon isotopes The Arctic region, with magnificent ice cover on the surface of the Arctic Ocean and adjacent seas, is not only extremely sensitive to but also has strong amplifica- tion effects on climate change. Observations during the past decades have documented substantial retreat and thinning of the Arctic sea-ice cover, a process that is accelerating. Its feedback and impact on the global climate has become an important subject of current climate change research. Calcite tests of planktonic foraminifers are major constituents in pelagic sediments, and they provide valu- able materials for the reconstruction of past oceanographic conditions. However, research is still sparse in the Arctic sea area because of limited availability of the materials for investigation. Here, we present a study of modem fora- minifers from the plankton tow samples taken in the Makarov Basin of the Arctic Ocean during the fourth Arctic expedition of China. We have analyzed ecological information stored in the modem planktonic foraminifers and in their stable isotope signals, and established a rela- tionship between the distribution of the main taxa and theenvironment. Our main observations are as follows： （1） in the Makarov Basin, the polar species Neogloboquadrina pachyderma （sinistral coiling） dominates the 〉150 μm planktonic foraminiferal assemblages. （2） The planktonic foraminifers live mainly in the upper halocline at a water depth of 50-100 m and less in the depth interval of 100-200 m. （3） Temperature change in the halocline can affect the absolute abundance of planktonic foraminifers and their distribution in the water column. The warmer halocline is more favorable to the development of plank- tonic foraminifers. （4） A lighter 6180 value （2.11‰） of N. pachyderma （sin.） is recorded in the depth interval of 100-200 m, which is likely related to the isotopically light brines separated out during sea ice freezing. The relatively heavy δ18O value （1.68 ‰-2.68‰, average 2.27‰） in the depth interval of 50-100 m may be influenced by the low salinity water with the relatively heavy δ18O value formed during the sea-ice melting in the surface layer. 11-1785/N http://dx.doi.org/10.1007/s11434-013-0082-8 ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
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| Title | Distribution, ecology, and oxygen and carbon isotope characteristics of modern planktonic foraminifers in the Makarov Basin of the Arctic Ocean |
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