How did rivers in the wet tropics (NE Queensland, Australia) respond to climate changes over the past 30 000 years?
The nature and timing of fluvial response and coincident changes in climate as inferred from multiple, independent proxies are examined in the wet tropics of north-eastern Australia. Chronostratigraphic data provide evidence for regionally synchronous fluvial aggradation at 30-13ka, 8-5ka and again...
Ausführliche Beschreibung
Autor*in: |
Hughes, Kate [verfasserIn] |
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Format: |
Artikel |
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Sprache: |
Englisch |
Erschienen: |
2017 |
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Rechteinformationen: |
Nutzungsrecht: Copyright © 2017 John Wiley & Sons, Ltd. |
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Schlagwörter: |
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Übergeordnetes Werk: |
Enthalten in: Journal of quaternary science - Chichester, Sussex : Wiley, 1986, 32(2017), 6, Seite 744-759 |
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Übergeordnetes Werk: |
volume:32 ; year:2017 ; number:6 ; pages:744-759 |
Links: |
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DOI / URN: |
10.1002/jqs.2956 |
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Katalog-ID: |
OLC1996174959 |
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520 | |a The nature and timing of fluvial response and coincident changes in climate as inferred from multiple, independent proxies are examined in the wet tropics of north-eastern Australia. Chronostratigraphic data provide evidence for regionally synchronous fluvial aggradation at 30-13ka, 8-5ka and again from 1 ka. Terrace incision and removal occurred at 13-8ka and 5-1ka. A new synthesis of regional palaeoenvironmental proxy records spanning the last 30ka highlights key periods of environmental change. Comparison of the records of fluvial and environmental change reveals the relationship is complex with no clear relationship between river aggradation/incision and wetter/drier conditions. The nature and timing of fluvial response in the wet tropics also shows broad similarities with coastal valleys in south-eastern New South Wales, suggesting continental-scale controls on fluvial response to changing climate during the Late Quaternary in Australia. Copyright © 2017 John Wiley & Sons, Ltd. | ||
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10.1002/jqs.2956 doi PQ20170901 (DE-627)OLC1996174959 (DE-599)GBVOLC1996174959 (PRQ)p956-c6c2ca675399fcad643d7abbce975a48ee21d5fddd2e9f67b15ca9805edf78a83 (KEY)0142506420170000032000600744howdidriversinthewettropicsnequeenslandaustraliare DE-627 ger DE-627 rakwb eng 550 ZDB 38.16 bkl 38.15 bkl Hughes, Kate verfasserin aut How did rivers in the wet tropics (NE Queensland, Australia) respond to climate changes over the past 30 000 years? 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The nature and timing of fluvial response and coincident changes in climate as inferred from multiple, independent proxies are examined in the wet tropics of north-eastern Australia. Chronostratigraphic data provide evidence for regionally synchronous fluvial aggradation at 30-13ka, 8-5ka and again from 1 ka. Terrace incision and removal occurred at 13-8ka and 5-1ka. A new synthesis of regional palaeoenvironmental proxy records spanning the last 30ka highlights key periods of environmental change. Comparison of the records of fluvial and environmental change reveals the relationship is complex with no clear relationship between river aggradation/incision and wetter/drier conditions. The nature and timing of fluvial response in the wet tropics also shows broad similarities with coastal valleys in south-eastern New South Wales, suggesting continental-scale controls on fluvial response to changing climate during the Late Quaternary in Australia. Copyright © 2017 John Wiley & Sons, Ltd. Nutzungsrecht: Copyright © 2017 John Wiley & Sons, Ltd. aggradation humid tropics alluvial terraces late Quaternary palaeoclimate incision Rivers Quaternary Coastal environments Tropical regions Climate Climate change Aggradation Valleys Croke, Jacky oth Enthalten in Journal of quaternary science Chichester, Sussex : Wiley, 1986 32(2017), 6, Seite 744-759 (DE-627)129351938 (DE-600)155650-2 (DE-576)090798384 0267-8179 nnns volume:32 year:2017 number:6 pages:744-759 http://dx.doi.org/10.1002/jqs.2956 Volltext http://onlinelibrary.wiley.com/doi/10.1002/jqs.2956/abstract https://search.proquest.com/docview/1930666664 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_183 38.16 AVZ 38.15 AVZ AR 32 2017 6 744-759 |
spelling |
10.1002/jqs.2956 doi PQ20170901 (DE-627)OLC1996174959 (DE-599)GBVOLC1996174959 (PRQ)p956-c6c2ca675399fcad643d7abbce975a48ee21d5fddd2e9f67b15ca9805edf78a83 (KEY)0142506420170000032000600744howdidriversinthewettropicsnequeenslandaustraliare DE-627 ger DE-627 rakwb eng 550 ZDB 38.16 bkl 38.15 bkl Hughes, Kate verfasserin aut How did rivers in the wet tropics (NE Queensland, Australia) respond to climate changes over the past 30 000 years? 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The nature and timing of fluvial response and coincident changes in climate as inferred from multiple, independent proxies are examined in the wet tropics of north-eastern Australia. Chronostratigraphic data provide evidence for regionally synchronous fluvial aggradation at 30-13ka, 8-5ka and again from 1 ka. Terrace incision and removal occurred at 13-8ka and 5-1ka. A new synthesis of regional palaeoenvironmental proxy records spanning the last 30ka highlights key periods of environmental change. Comparison of the records of fluvial and environmental change reveals the relationship is complex with no clear relationship between river aggradation/incision and wetter/drier conditions. The nature and timing of fluvial response in the wet tropics also shows broad similarities with coastal valleys in south-eastern New South Wales, suggesting continental-scale controls on fluvial response to changing climate during the Late Quaternary in Australia. Copyright © 2017 John Wiley & Sons, Ltd. Nutzungsrecht: Copyright © 2017 John Wiley & Sons, Ltd. aggradation humid tropics alluvial terraces late Quaternary palaeoclimate incision Rivers Quaternary Coastal environments Tropical regions Climate Climate change Aggradation Valleys Croke, Jacky oth Enthalten in Journal of quaternary science Chichester, Sussex : Wiley, 1986 32(2017), 6, Seite 744-759 (DE-627)129351938 (DE-600)155650-2 (DE-576)090798384 0267-8179 nnns volume:32 year:2017 number:6 pages:744-759 http://dx.doi.org/10.1002/jqs.2956 Volltext http://onlinelibrary.wiley.com/doi/10.1002/jqs.2956/abstract https://search.proquest.com/docview/1930666664 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_183 38.16 AVZ 38.15 AVZ AR 32 2017 6 744-759 |
allfields_unstemmed |
10.1002/jqs.2956 doi PQ20170901 (DE-627)OLC1996174959 (DE-599)GBVOLC1996174959 (PRQ)p956-c6c2ca675399fcad643d7abbce975a48ee21d5fddd2e9f67b15ca9805edf78a83 (KEY)0142506420170000032000600744howdidriversinthewettropicsnequeenslandaustraliare DE-627 ger DE-627 rakwb eng 550 ZDB 38.16 bkl 38.15 bkl Hughes, Kate verfasserin aut How did rivers in the wet tropics (NE Queensland, Australia) respond to climate changes over the past 30 000 years? 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The nature and timing of fluvial response and coincident changes in climate as inferred from multiple, independent proxies are examined in the wet tropics of north-eastern Australia. Chronostratigraphic data provide evidence for regionally synchronous fluvial aggradation at 30-13ka, 8-5ka and again from 1 ka. Terrace incision and removal occurred at 13-8ka and 5-1ka. A new synthesis of regional palaeoenvironmental proxy records spanning the last 30ka highlights key periods of environmental change. Comparison of the records of fluvial and environmental change reveals the relationship is complex with no clear relationship between river aggradation/incision and wetter/drier conditions. The nature and timing of fluvial response in the wet tropics also shows broad similarities with coastal valleys in south-eastern New South Wales, suggesting continental-scale controls on fluvial response to changing climate during the Late Quaternary in Australia. Copyright © 2017 John Wiley & Sons, Ltd. Nutzungsrecht: Copyright © 2017 John Wiley & Sons, Ltd. aggradation humid tropics alluvial terraces late Quaternary palaeoclimate incision Rivers Quaternary Coastal environments Tropical regions Climate Climate change Aggradation Valleys Croke, Jacky oth Enthalten in Journal of quaternary science Chichester, Sussex : Wiley, 1986 32(2017), 6, Seite 744-759 (DE-627)129351938 (DE-600)155650-2 (DE-576)090798384 0267-8179 nnns volume:32 year:2017 number:6 pages:744-759 http://dx.doi.org/10.1002/jqs.2956 Volltext http://onlinelibrary.wiley.com/doi/10.1002/jqs.2956/abstract https://search.proquest.com/docview/1930666664 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_183 38.16 AVZ 38.15 AVZ AR 32 2017 6 744-759 |
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10.1002/jqs.2956 doi PQ20170901 (DE-627)OLC1996174959 (DE-599)GBVOLC1996174959 (PRQ)p956-c6c2ca675399fcad643d7abbce975a48ee21d5fddd2e9f67b15ca9805edf78a83 (KEY)0142506420170000032000600744howdidriversinthewettropicsnequeenslandaustraliare DE-627 ger DE-627 rakwb eng 550 ZDB 38.16 bkl 38.15 bkl Hughes, Kate verfasserin aut How did rivers in the wet tropics (NE Queensland, Australia) respond to climate changes over the past 30 000 years? 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The nature and timing of fluvial response and coincident changes in climate as inferred from multiple, independent proxies are examined in the wet tropics of north-eastern Australia. Chronostratigraphic data provide evidence for regionally synchronous fluvial aggradation at 30-13ka, 8-5ka and again from 1 ka. Terrace incision and removal occurred at 13-8ka and 5-1ka. A new synthesis of regional palaeoenvironmental proxy records spanning the last 30ka highlights key periods of environmental change. Comparison of the records of fluvial and environmental change reveals the relationship is complex with no clear relationship between river aggradation/incision and wetter/drier conditions. The nature and timing of fluvial response in the wet tropics also shows broad similarities with coastal valleys in south-eastern New South Wales, suggesting continental-scale controls on fluvial response to changing climate during the Late Quaternary in Australia. Copyright © 2017 John Wiley & Sons, Ltd. Nutzungsrecht: Copyright © 2017 John Wiley & Sons, Ltd. aggradation humid tropics alluvial terraces late Quaternary palaeoclimate incision Rivers Quaternary Coastal environments Tropical regions Climate Climate change Aggradation Valleys Croke, Jacky oth Enthalten in Journal of quaternary science Chichester, Sussex : Wiley, 1986 32(2017), 6, Seite 744-759 (DE-627)129351938 (DE-600)155650-2 (DE-576)090798384 0267-8179 nnns volume:32 year:2017 number:6 pages:744-759 http://dx.doi.org/10.1002/jqs.2956 Volltext http://onlinelibrary.wiley.com/doi/10.1002/jqs.2956/abstract https://search.proquest.com/docview/1930666664 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_183 38.16 AVZ 38.15 AVZ AR 32 2017 6 744-759 |
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10.1002/jqs.2956 doi PQ20170901 (DE-627)OLC1996174959 (DE-599)GBVOLC1996174959 (PRQ)p956-c6c2ca675399fcad643d7abbce975a48ee21d5fddd2e9f67b15ca9805edf78a83 (KEY)0142506420170000032000600744howdidriversinthewettropicsnequeenslandaustraliare DE-627 ger DE-627 rakwb eng 550 ZDB 38.16 bkl 38.15 bkl Hughes, Kate verfasserin aut How did rivers in the wet tropics (NE Queensland, Australia) respond to climate changes over the past 30 000 years? 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier The nature and timing of fluvial response and coincident changes in climate as inferred from multiple, independent proxies are examined in the wet tropics of north-eastern Australia. Chronostratigraphic data provide evidence for regionally synchronous fluvial aggradation at 30-13ka, 8-5ka and again from 1 ka. Terrace incision and removal occurred at 13-8ka and 5-1ka. A new synthesis of regional palaeoenvironmental proxy records spanning the last 30ka highlights key periods of environmental change. Comparison of the records of fluvial and environmental change reveals the relationship is complex with no clear relationship between river aggradation/incision and wetter/drier conditions. The nature and timing of fluvial response in the wet tropics also shows broad similarities with coastal valleys in south-eastern New South Wales, suggesting continental-scale controls on fluvial response to changing climate during the Late Quaternary in Australia. Copyright © 2017 John Wiley & Sons, Ltd. Nutzungsrecht: Copyright © 2017 John Wiley & Sons, Ltd. aggradation humid tropics alluvial terraces late Quaternary palaeoclimate incision Rivers Quaternary Coastal environments Tropical regions Climate Climate change Aggradation Valleys Croke, Jacky oth Enthalten in Journal of quaternary science Chichester, Sussex : Wiley, 1986 32(2017), 6, Seite 744-759 (DE-627)129351938 (DE-600)155650-2 (DE-576)090798384 0267-8179 nnns volume:32 year:2017 number:6 pages:744-759 http://dx.doi.org/10.1002/jqs.2956 Volltext http://onlinelibrary.wiley.com/doi/10.1002/jqs.2956/abstract https://search.proquest.com/docview/1930666664 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_183 38.16 AVZ 38.15 AVZ AR 32 2017 6 744-759 |
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550 ZDB 38.16 bkl 38.15 bkl How did rivers in the wet tropics (NE Queensland, Australia) respond to climate changes over the past 30 000 years? aggradation humid tropics alluvial terraces late Quaternary palaeoclimate incision Rivers Quaternary Coastal environments Tropical regions Climate Climate change Aggradation Valleys |
topic |
ddc 550 bkl 38.16 bkl 38.15 misc aggradation misc humid tropics misc alluvial terraces misc late Quaternary palaeoclimate misc incision misc Rivers misc Quaternary misc Coastal environments misc Tropical regions misc Climate misc Climate change misc Aggradation misc Valleys |
topic_unstemmed |
ddc 550 bkl 38.16 bkl 38.15 misc aggradation misc humid tropics misc alluvial terraces misc late Quaternary palaeoclimate misc incision misc Rivers misc Quaternary misc Coastal environments misc Tropical regions misc Climate misc Climate change misc Aggradation misc Valleys |
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ddc 550 bkl 38.16 bkl 38.15 misc aggradation misc humid tropics misc alluvial terraces misc late Quaternary palaeoclimate misc incision misc Rivers misc Quaternary misc Coastal environments misc Tropical regions misc Climate misc Climate change misc Aggradation misc Valleys |
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How did rivers in the wet tropics (NE Queensland, Australia) respond to climate changes over the past 30 000 years? |
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How did rivers in the wet tropics (NE Queensland, Australia) respond to climate changes over the past 30 000 years? |
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Hughes, Kate |
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how did rivers in the wet tropics (ne queensland, australia) respond to climate changes over the past 30 000 years? |
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How did rivers in the wet tropics (NE Queensland, Australia) respond to climate changes over the past 30 000 years? |
abstract |
The nature and timing of fluvial response and coincident changes in climate as inferred from multiple, independent proxies are examined in the wet tropics of north-eastern Australia. Chronostratigraphic data provide evidence for regionally synchronous fluvial aggradation at 30-13ka, 8-5ka and again from 1 ka. Terrace incision and removal occurred at 13-8ka and 5-1ka. A new synthesis of regional palaeoenvironmental proxy records spanning the last 30ka highlights key periods of environmental change. Comparison of the records of fluvial and environmental change reveals the relationship is complex with no clear relationship between river aggradation/incision and wetter/drier conditions. The nature and timing of fluvial response in the wet tropics also shows broad similarities with coastal valleys in south-eastern New South Wales, suggesting continental-scale controls on fluvial response to changing climate during the Late Quaternary in Australia. Copyright © 2017 John Wiley & Sons, Ltd. |
abstractGer |
The nature and timing of fluvial response and coincident changes in climate as inferred from multiple, independent proxies are examined in the wet tropics of north-eastern Australia. Chronostratigraphic data provide evidence for regionally synchronous fluvial aggradation at 30-13ka, 8-5ka and again from 1 ka. Terrace incision and removal occurred at 13-8ka and 5-1ka. A new synthesis of regional palaeoenvironmental proxy records spanning the last 30ka highlights key periods of environmental change. Comparison of the records of fluvial and environmental change reveals the relationship is complex with no clear relationship between river aggradation/incision and wetter/drier conditions. The nature and timing of fluvial response in the wet tropics also shows broad similarities with coastal valleys in south-eastern New South Wales, suggesting continental-scale controls on fluvial response to changing climate during the Late Quaternary in Australia. Copyright © 2017 John Wiley & Sons, Ltd. |
abstract_unstemmed |
The nature and timing of fluvial response and coincident changes in climate as inferred from multiple, independent proxies are examined in the wet tropics of north-eastern Australia. Chronostratigraphic data provide evidence for regionally synchronous fluvial aggradation at 30-13ka, 8-5ka and again from 1 ka. Terrace incision and removal occurred at 13-8ka and 5-1ka. A new synthesis of regional palaeoenvironmental proxy records spanning the last 30ka highlights key periods of environmental change. Comparison of the records of fluvial and environmental change reveals the relationship is complex with no clear relationship between river aggradation/incision and wetter/drier conditions. The nature and timing of fluvial response in the wet tropics also shows broad similarities with coastal valleys in south-eastern New South Wales, suggesting continental-scale controls on fluvial response to changing climate during the Late Quaternary in Australia. Copyright © 2017 John Wiley & Sons, Ltd. |
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How did rivers in the wet tropics (NE Queensland, Australia) respond to climate changes over the past 30 000 years? |
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http://dx.doi.org/10.1002/jqs.2956 http://onlinelibrary.wiley.com/doi/10.1002/jqs.2956/abstract https://search.proquest.com/docview/1930666664 |
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