Millennial-Scale Changes of Intermediate Water Ventilation, Productivity and Nutrient Supply in the Okhotsk Sea and Subarctic North Pacific During the Last 18,000 Years
Paleoceanography, North Pacific, intermediate water, stable isotopes, biogenic productivity, Holocene, glacial termination, Okhotsk Sea. - A reconstruction of North Pacific mid-depth water ventilation and biogenic productivity variations over the last 18,000 years is presented, based on sediment cor...
Ausführliche Beschreibung
Autor*in: |
Lembke-Jene, Lester [verfasserIn] |
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Hochschulschrift: |
Bremen, Univ., Diss., 2013 |
Format: |
E-Book |
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Sprache: |
Englisch |
Erschienen: |
2013 |
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Formangabe: |
Hochschulschrift |
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Umfang: |
Online-Ressource |
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Weitere Ausgabe: |
Druckausg. Lembke-Jene, Lester: Millennial-Scale Changes of Intermediate Water Ventilation, Productivity and Nutrient Supply in the Okhotsk Sea and Subarctic North Pacific During the Last 18,000 Years - 2013 |
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Links: |
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DOI / URN: |
urn:nbn:de:gbv:46-00104656-16 |
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Katalog-ID: |
839010311 |
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I reconstructed transient decreases in IW oxygenation during deglacial warm phases, likely tied to rapid, significantly enhanced organic matter remineralization within the IW, in line with evidence for maxima in primary productivity. Investigations of upper ocean stratification and sea surface temperatures revealed a link between upper mixed layer stratification maxima and ventilation minima during interstadial deglacial phases in large swaths of the Northwest Pacific. Analysis of Holocene cores showed the modern pattern of IW ventilation to be a relatively recent feature of only the last 2,000 years. During the warmer than present early-mid-Holocene, active ventilation was significantly decreased. Estimated O2 concentrations of Okhotsk Sea IW reached only 50-60 % of modern values, and the region turned from an early Holocene O2-sink into the modern O2-source around 6,000 years ago. 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I reconstructed transient decreases in IW oxygenation during deglacial warm phases, likely tied to rapid, significantly enhanced organic matter remineralization within the IW, in line with evidence for maxima in primary productivity. Investigations of upper ocean stratification and sea surface temperatures revealed a link between upper mixed layer stratification maxima and ventilation minima during interstadial deglacial phases in large swaths of the Northwest Pacific. Analysis of Holocene cores showed the modern pattern of IW ventilation to be a relatively recent feature of only the last 2,000 years. During the warmer than present early-mid-Holocene, active ventilation was significantly decreased. Estimated O2 concentrations of Okhotsk Sea IW reached only 50-60 % of modern values, and the region turned from an early Holocene O2-sink into the modern O2-source around 6,000 years ago. Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Bremen uvp Druckausg. 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I reconstructed transient decreases in IW oxygenation during deglacial warm phases, likely tied to rapid, significantly enhanced organic matter remineralization within the IW, in line with evidence for maxima in primary productivity. Investigations of upper ocean stratification and sea surface temperatures revealed a link between upper mixed layer stratification maxima and ventilation minima during interstadial deglacial phases in large swaths of the Northwest Pacific. Analysis of Holocene cores showed the modern pattern of IW ventilation to be a relatively recent feature of only the last 2,000 years. During the warmer than present early-mid-Holocene, active ventilation was significantly decreased. Estimated O2 concentrations of Okhotsk Sea IW reached only 50-60 % of modern values, and the region turned from an early Holocene O2-sink into the modern O2-source around 6,000 years ago. Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Bremen uvp Druckausg. Lembke-Jene, Lester Millennial-Scale Changes of Intermediate Water Ventilation, Productivity and Nutrient Supply in the Okhotsk Sea and Subarctic North Pacific During the Last 18,000 Years 2013 Seiten (DE-627)839010222 http://nbn-resolving.de/urn:nbn:de:gbv:46-00104656-16 Resolving-System kostenfrei Volltext http://nbn-resolving.de/urn:nbn:de:gbv:46-00104656-16 2015-12-07 Resolving-System Volltext http://d-nb.info/1078720231/34 2015-12-07 Langzeitarchivierung Nationalbibliothek Volltext http://elib.suub.uni-bremen.de/edocs/00104656-1.pdf 2015-12-07 Verlag kostenfrei Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_65 ISIL_DE-3 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2403 ISIL_DE-LFER BO 20 01 0084 1587615835 x 08-12-15 21 01 0046 1579467679 ebook_2015_dissbremen Kostenloser Zugriff zza 10-11-15 22 01 0018 1587637243 SUBolrd xu 08-12-15 23 01 0830 158764732X olr-d x 08-12-15 30 01 0104 1587653907 z 08-12-15 40 01 0007 1587660490 xsn 08-12-15 60 01 0705 1587671476 OLRD z 08-12-15 63 01 3401 1595903305 ORD x 21-01-16 65 01 0003 416761765X GBV-ODiss Open Access z 16-07-22 70 01 0089 1587689421 zdo 08-12-15 105 01 0841 1596716738 z 21-01-16 110 01 3110 1587681862 x 08-12-15 132 01 0959 1591572355 OLR-DISS x 19-12-15 151 01 0546 3594317854 OLR-ODISS z 13-02-20 161 01 0960 1597724661 ORD x 28-01-16 293 01 3293 1598268406 ORD xf 28-01-16 370 01 4370 158768750X x 08-12-15 2403 01 DE-LFER 3495383999 00 --%%-- --%%-- n --%%-- l01 21-07-19 20 01 0084 http://nbn-resolving.de/urn:nbn:de:gbv:46-00104656-16 21 01 0046 http://nbn-resolving.de/urn:nbn:de:gbv:46-00104656-16 LF 22 01 0018 http://nbn-resolving.de/urn:nbn:de:gbv:46-00104656-16 23 01 0830 http://nbn-resolving.de/urn:nbn:de:gbv:46-00104656-16 30 01 0104 http://nbn-resolving.de/urn:nbn:de:gbv:46-00104656-16 40 01 0007 http://nbn-resolving.de/urn:nbn:de:gbv:46-00104656-16 60 01 0705 http://nbn-resolving.de/urn:nbn:de:gbv:46-00104656-16 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:gbv:46-00104656-16 LF 65 01 0003 http://nbn-resolving.de/urn:nbn:de:gbv:46-00104656-16 70 01 0089 http://nbn-resolving.de/urn:nbn:de:gbv:46-00104656-16 105 01 0841 http://nbn-resolving.de/urn:nbn:de:gbv:46-00104656-16 110 01 3110 http://nbn-resolving.de/urn:nbn:de:gbv:46-00104656-16 132 01 0959 http://nbn-resolving.de/urn:nbn:de:gbv:46-00104656-16 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:gbv:46-00104656-16 161 01 0960 http://nbn-resolving.de/urn:nbn:de:gbv:46-00104656-16 293 01 3293 http://nbn-resolving.de/urn:nbn:de:gbv:46-00104656-16 370 01 4370 http://nbn-resolving.de/urn:nbn:de:gbv:46-00104656-16 2403 01 DE-LFER http://nbn-resolving.de/urn:nbn:de:gbv:46-00104656-16 21 00 DE-46 99 07 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 21 01 0046 ebook_2015_dissbremen 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 65 01 0003 GBV-ODiss 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2015-12-08:15:39:35 |
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I reconstructed transient decreases in IW oxygenation during deglacial warm phases, likely tied to rapid, significantly enhanced organic matter remineralization within the IW, in line with evidence for maxima in primary productivity. Investigations of upper ocean stratification and sea surface temperatures revealed a link between upper mixed layer stratification maxima and ventilation minima during interstadial deglacial phases in large swaths of the Northwest Pacific. Analysis of Holocene cores showed the modern pattern of IW ventilation to be a relatively recent feature of only the last 2,000 years. During the warmer than present early-mid-Holocene, active ventilation was significantly decreased. Estimated O2 concentrations of Okhotsk Sea IW reached only 50-60 % of modern values, and the region turned from an early Holocene O2-sink into the modern O2-source around 6,000 years ago. Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Bremen uvp Druckausg. 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author |
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550 DNB Millennial-Scale Changes of Intermediate Water Ventilation, Productivity and Nutrient Supply in the Okhotsk Sea and Subarctic North Pacific During the Last 18,000 Years von Lester Lembke-Jene |
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millennial-scale changes of intermediate water ventilation, productivity and nutrient supply in the okhotsk sea and subarctic north pacific during the last 18,000 years |
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Millennial-Scale Changes of Intermediate Water Ventilation, Productivity and Nutrient Supply in the Okhotsk Sea and Subarctic North Pacific During the Last 18,000 Years |
abstract |
Paleoceanography, North Pacific, intermediate water, stable isotopes, biogenic productivity, Holocene, glacial termination, Okhotsk Sea. - A reconstruction of North Pacific mid-depth water ventilation and biogenic productivity variations over the last 18,000 years is presented, based on sediment cores from the source region (Okhotsk Sea) of modern intermediate water (IW) ventilation. I reconstructed transient decreases in IW oxygenation during deglacial warm phases, likely tied to rapid, significantly enhanced organic matter remineralization within the IW, in line with evidence for maxima in primary productivity. Investigations of upper ocean stratification and sea surface temperatures revealed a link between upper mixed layer stratification maxima and ventilation minima during interstadial deglacial phases in large swaths of the Northwest Pacific. Analysis of Holocene cores showed the modern pattern of IW ventilation to be a relatively recent feature of only the last 2,000 years. During the warmer than present early-mid-Holocene, active ventilation was significantly decreased. Estimated O2 concentrations of Okhotsk Sea IW reached only 50-60 % of modern values, and the region turned from an early Holocene O2-sink into the modern O2-source around 6,000 years ago. |
abstractGer |
Paleoceanography, North Pacific, intermediate water, stable isotopes, biogenic productivity, Holocene, glacial termination, Okhotsk Sea. - A reconstruction of North Pacific mid-depth water ventilation and biogenic productivity variations over the last 18,000 years is presented, based on sediment cores from the source region (Okhotsk Sea) of modern intermediate water (IW) ventilation. I reconstructed transient decreases in IW oxygenation during deglacial warm phases, likely tied to rapid, significantly enhanced organic matter remineralization within the IW, in line with evidence for maxima in primary productivity. Investigations of upper ocean stratification and sea surface temperatures revealed a link between upper mixed layer stratification maxima and ventilation minima during interstadial deglacial phases in large swaths of the Northwest Pacific. Analysis of Holocene cores showed the modern pattern of IW ventilation to be a relatively recent feature of only the last 2,000 years. During the warmer than present early-mid-Holocene, active ventilation was significantly decreased. Estimated O2 concentrations of Okhotsk Sea IW reached only 50-60 % of modern values, and the region turned from an early Holocene O2-sink into the modern O2-source around 6,000 years ago. |
abstract_unstemmed |
Paleoceanography, North Pacific, intermediate water, stable isotopes, biogenic productivity, Holocene, glacial termination, Okhotsk Sea. - A reconstruction of North Pacific mid-depth water ventilation and biogenic productivity variations over the last 18,000 years is presented, based on sediment cores from the source region (Okhotsk Sea) of modern intermediate water (IW) ventilation. I reconstructed transient decreases in IW oxygenation during deglacial warm phases, likely tied to rapid, significantly enhanced organic matter remineralization within the IW, in line with evidence for maxima in primary productivity. Investigations of upper ocean stratification and sea surface temperatures revealed a link between upper mixed layer stratification maxima and ventilation minima during interstadial deglacial phases in large swaths of the Northwest Pacific. Analysis of Holocene cores showed the modern pattern of IW ventilation to be a relatively recent feature of only the last 2,000 years. During the warmer than present early-mid-Holocene, active ventilation was significantly decreased. Estimated O2 concentrations of Okhotsk Sea IW reached only 50-60 % of modern values, and the region turned from an early Holocene O2-sink into the modern O2-source around 6,000 years ago. |
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title_short |
Millennial-Scale Changes of Intermediate Water Ventilation, Productivity and Nutrient Supply in the Okhotsk Sea and Subarctic North Pacific During the Last 18,000 Years |
url |
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