Environmental controls on the resilience of Scott Reefs since the Miocene (North West Shelf, Australia): Insights from 3D seismic data
North and South Scott Reefs are isolated carbonate platforms separated by an inter-reef channel on the NWS, Australia. They evolved from a barrier reef in the Miocene, and into isolated carbonate build-ups (ICB's) during the Pliocene, and finally to the isolated carbonate platforms that continu...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Williams, Carra [verfasserIn] Paumard, Victorien [verfasserIn] Webster, Jody M. [verfasserIn] Leonard, Jonathon [verfasserIn] Salles, Tristan [verfasserIn] O'Leary, Michael [verfasserIn] Lang, Simon [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2023 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Marine and petroleum geology - Amsterdam [u.a.] : Elsevier Science, 1984, 151 |
|---|---|
| Übergeordnetes Werk: |
volume:151 |
| DOI / URN: |
10.1016/j.marpetgeo.2023.106188 |
|---|
| Katalog-ID: |
ELV009563091 |
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| 245 | 1 | 0 | |a Environmental controls on the resilience of Scott Reefs since the Miocene (North West Shelf, Australia): Insights from 3D seismic data |
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| 520 | |a North and South Scott Reefs are isolated carbonate platforms separated by an inter-reef channel on the NWS, Australia. They evolved from a barrier reef in the Miocene, and into isolated carbonate build-ups (ICB's) during the Pliocene, and finally to the isolated carbonate platforms that continued to present day. However, the timings of coral reef turn on and off are not well constrained with respect to global climatic changes in this region. The North West Shelf (NWS) of Australia recorded marked climatic and oceanographic changes through the Cenozoic. For example: (1) the Mid Miocene Climatic Optimum (MMCO), leading to the onset of ICB's and carbonate platform development; (2) the Mid Pleistocene Transition (MPT) (ca. 0.8–0.6 Ma) and the associated change in regional climate from wet to dry; and (3) glacial-interglacial variability through the Pleistocene until present day. Availability of high resolution and extensive 3D seismic data provides a unique opportunity to investigate the evolution of these reefs using seismic stratigraphy and seismic geomorphology. Four main phases of carbonate factory evolution (Phase I-IV) were identified from the Miocene to present. A chrono-stratigraphic framework is constructed, detailing relative sea-level (RSL) changes and the impact of global (e.g., climate, eustasy) and regional (e.g., tectonics, oceanography) forcing parameters on their development. Seismic stratigraphy reveals that despite rapid accommodation rate changes, the oceanographic setting, antecedent topography and rapid vertical reef accretion played a key role in the persistence of Scott Reefs. It is likely that the Indonesian throughflow (ITF) current has been a critical component in controlling the local climate. The Leeuwin current, tides, swells and wind regimes similarly exert a major influence on the NWS climate, whilst the inter-reef channel likely bypassed terrigenous sediment influx away from the reefs, avoiding periods of inundation during wet climates. | ||
| 650 | 4 | |a Seismic stratigraphy | |
| 650 | 4 | |a Seismic geomorphology | |
| 650 | 4 | |a Carbonate platform | |
| 650 | 4 | |a Coral reefs | |
| 650 | 4 | |a Tectono-stratigraphy | |
| 650 | 4 | |a Paleo-environmental reconstruction | |
| 650 | 4 | |a Chrono-stratigraphic framework | |
| 700 | 1 | |a Paumard, Victorien |e verfasserin |4 aut | |
| 700 | 1 | |a Webster, Jody M. |e verfasserin |4 aut | |
| 700 | 1 | |a Leonard, Jonathon |e verfasserin |4 aut | |
| 700 | 1 | |a Salles, Tristan |e verfasserin |4 aut | |
| 700 | 1 | |a O'Leary, Michael |e verfasserin |4 aut | |
| 700 | 1 | |a Lang, Simon |e verfasserin |4 aut | |
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10.1016/j.marpetgeo.2023.106188 doi (DE-627)ELV009563091 (ELSEVIER)S0264-8172(23)00094-6 DE-627 ger DE-627 rda eng 550 VZ 38.48 bkl 38.51 bkl Williams, Carra verfasserin (orcid)0000-0002-1312-4438 aut Environmental controls on the resilience of Scott Reefs since the Miocene (North West Shelf, Australia): Insights from 3D seismic data 2023 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier North and South Scott Reefs are isolated carbonate platforms separated by an inter-reef channel on the NWS, Australia. They evolved from a barrier reef in the Miocene, and into isolated carbonate build-ups (ICB's) during the Pliocene, and finally to the isolated carbonate platforms that continued to present day. However, the timings of coral reef turn on and off are not well constrained with respect to global climatic changes in this region. The North West Shelf (NWS) of Australia recorded marked climatic and oceanographic changes through the Cenozoic. For example: (1) the Mid Miocene Climatic Optimum (MMCO), leading to the onset of ICB's and carbonate platform development; (2) the Mid Pleistocene Transition (MPT) (ca. 0.8–0.6 Ma) and the associated change in regional climate from wet to dry; and (3) glacial-interglacial variability through the Pleistocene until present day. Availability of high resolution and extensive 3D seismic data provides a unique opportunity to investigate the evolution of these reefs using seismic stratigraphy and seismic geomorphology. Four main phases of carbonate factory evolution (Phase I-IV) were identified from the Miocene to present. A chrono-stratigraphic framework is constructed, detailing relative sea-level (RSL) changes and the impact of global (e.g., climate, eustasy) and regional (e.g., tectonics, oceanography) forcing parameters on their development. Seismic stratigraphy reveals that despite rapid accommodation rate changes, the oceanographic setting, antecedent topography and rapid vertical reef accretion played a key role in the persistence of Scott Reefs. It is likely that the Indonesian throughflow (ITF) current has been a critical component in controlling the local climate. The Leeuwin current, tides, swells and wind regimes similarly exert a major influence on the NWS climate, whilst the inter-reef channel likely bypassed terrigenous sediment influx away from the reefs, avoiding periods of inundation during wet climates. Seismic stratigraphy Seismic geomorphology Carbonate platform Coral reefs Tectono-stratigraphy Paleo-environmental reconstruction Chrono-stratigraphic framework Paumard, Victorien verfasserin aut Webster, Jody M. verfasserin aut Leonard, Jonathon verfasserin aut Salles, Tristan verfasserin aut O'Leary, Michael verfasserin aut Lang, Simon verfasserin aut Enthalten in Marine and petroleum geology Amsterdam [u.a.] : Elsevier Science, 1984 151 Online-Ressource (DE-627)303393416 (DE-600)1494910-6 (DE-576)259484032 0264-8172 nnns volume:151 GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2088 GBV_ILN_2106 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.48 Marine Geologie VZ 38.51 Geologie fossiler Brennstoffe VZ AR 151 |
| spelling |
10.1016/j.marpetgeo.2023.106188 doi (DE-627)ELV009563091 (ELSEVIER)S0264-8172(23)00094-6 DE-627 ger DE-627 rda eng 550 VZ 38.48 bkl 38.51 bkl Williams, Carra verfasserin (orcid)0000-0002-1312-4438 aut Environmental controls on the resilience of Scott Reefs since the Miocene (North West Shelf, Australia): Insights from 3D seismic data 2023 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier North and South Scott Reefs are isolated carbonate platforms separated by an inter-reef channel on the NWS, Australia. They evolved from a barrier reef in the Miocene, and into isolated carbonate build-ups (ICB's) during the Pliocene, and finally to the isolated carbonate platforms that continued to present day. However, the timings of coral reef turn on and off are not well constrained with respect to global climatic changes in this region. The North West Shelf (NWS) of Australia recorded marked climatic and oceanographic changes through the Cenozoic. For example: (1) the Mid Miocene Climatic Optimum (MMCO), leading to the onset of ICB's and carbonate platform development; (2) the Mid Pleistocene Transition (MPT) (ca. 0.8–0.6 Ma) and the associated change in regional climate from wet to dry; and (3) glacial-interglacial variability through the Pleistocene until present day. Availability of high resolution and extensive 3D seismic data provides a unique opportunity to investigate the evolution of these reefs using seismic stratigraphy and seismic geomorphology. Four main phases of carbonate factory evolution (Phase I-IV) were identified from the Miocene to present. A chrono-stratigraphic framework is constructed, detailing relative sea-level (RSL) changes and the impact of global (e.g., climate, eustasy) and regional (e.g., tectonics, oceanography) forcing parameters on their development. Seismic stratigraphy reveals that despite rapid accommodation rate changes, the oceanographic setting, antecedent topography and rapid vertical reef accretion played a key role in the persistence of Scott Reefs. It is likely that the Indonesian throughflow (ITF) current has been a critical component in controlling the local climate. The Leeuwin current, tides, swells and wind regimes similarly exert a major influence on the NWS climate, whilst the inter-reef channel likely bypassed terrigenous sediment influx away from the reefs, avoiding periods of inundation during wet climates. Seismic stratigraphy Seismic geomorphology Carbonate platform Coral reefs Tectono-stratigraphy Paleo-environmental reconstruction Chrono-stratigraphic framework Paumard, Victorien verfasserin aut Webster, Jody M. verfasserin aut Leonard, Jonathon verfasserin aut Salles, Tristan verfasserin aut O'Leary, Michael verfasserin aut Lang, Simon verfasserin aut Enthalten in Marine and petroleum geology Amsterdam [u.a.] : Elsevier Science, 1984 151 Online-Ressource (DE-627)303393416 (DE-600)1494910-6 (DE-576)259484032 0264-8172 nnns volume:151 GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2088 GBV_ILN_2106 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.48 Marine Geologie VZ 38.51 Geologie fossiler Brennstoffe VZ AR 151 |
| allfields_unstemmed |
10.1016/j.marpetgeo.2023.106188 doi (DE-627)ELV009563091 (ELSEVIER)S0264-8172(23)00094-6 DE-627 ger DE-627 rda eng 550 VZ 38.48 bkl 38.51 bkl Williams, Carra verfasserin (orcid)0000-0002-1312-4438 aut Environmental controls on the resilience of Scott Reefs since the Miocene (North West Shelf, Australia): Insights from 3D seismic data 2023 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier North and South Scott Reefs are isolated carbonate platforms separated by an inter-reef channel on the NWS, Australia. They evolved from a barrier reef in the Miocene, and into isolated carbonate build-ups (ICB's) during the Pliocene, and finally to the isolated carbonate platforms that continued to present day. However, the timings of coral reef turn on and off are not well constrained with respect to global climatic changes in this region. The North West Shelf (NWS) of Australia recorded marked climatic and oceanographic changes through the Cenozoic. For example: (1) the Mid Miocene Climatic Optimum (MMCO), leading to the onset of ICB's and carbonate platform development; (2) the Mid Pleistocene Transition (MPT) (ca. 0.8–0.6 Ma) and the associated change in regional climate from wet to dry; and (3) glacial-interglacial variability through the Pleistocene until present day. Availability of high resolution and extensive 3D seismic data provides a unique opportunity to investigate the evolution of these reefs using seismic stratigraphy and seismic geomorphology. Four main phases of carbonate factory evolution (Phase I-IV) were identified from the Miocene to present. A chrono-stratigraphic framework is constructed, detailing relative sea-level (RSL) changes and the impact of global (e.g., climate, eustasy) and regional (e.g., tectonics, oceanography) forcing parameters on their development. Seismic stratigraphy reveals that despite rapid accommodation rate changes, the oceanographic setting, antecedent topography and rapid vertical reef accretion played a key role in the persistence of Scott Reefs. It is likely that the Indonesian throughflow (ITF) current has been a critical component in controlling the local climate. The Leeuwin current, tides, swells and wind regimes similarly exert a major influence on the NWS climate, whilst the inter-reef channel likely bypassed terrigenous sediment influx away from the reefs, avoiding periods of inundation during wet climates. Seismic stratigraphy Seismic geomorphology Carbonate platform Coral reefs Tectono-stratigraphy Paleo-environmental reconstruction Chrono-stratigraphic framework Paumard, Victorien verfasserin aut Webster, Jody M. verfasserin aut Leonard, Jonathon verfasserin aut Salles, Tristan verfasserin aut O'Leary, Michael verfasserin aut Lang, Simon verfasserin aut Enthalten in Marine and petroleum geology Amsterdam [u.a.] : Elsevier Science, 1984 151 Online-Ressource (DE-627)303393416 (DE-600)1494910-6 (DE-576)259484032 0264-8172 nnns volume:151 GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2088 GBV_ILN_2106 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.48 Marine Geologie VZ 38.51 Geologie fossiler Brennstoffe VZ AR 151 |
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10.1016/j.marpetgeo.2023.106188 doi (DE-627)ELV009563091 (ELSEVIER)S0264-8172(23)00094-6 DE-627 ger DE-627 rda eng 550 VZ 38.48 bkl 38.51 bkl Williams, Carra verfasserin (orcid)0000-0002-1312-4438 aut Environmental controls on the resilience of Scott Reefs since the Miocene (North West Shelf, Australia): Insights from 3D seismic data 2023 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier North and South Scott Reefs are isolated carbonate platforms separated by an inter-reef channel on the NWS, Australia. They evolved from a barrier reef in the Miocene, and into isolated carbonate build-ups (ICB's) during the Pliocene, and finally to the isolated carbonate platforms that continued to present day. However, the timings of coral reef turn on and off are not well constrained with respect to global climatic changes in this region. The North West Shelf (NWS) of Australia recorded marked climatic and oceanographic changes through the Cenozoic. For example: (1) the Mid Miocene Climatic Optimum (MMCO), leading to the onset of ICB's and carbonate platform development; (2) the Mid Pleistocene Transition (MPT) (ca. 0.8–0.6 Ma) and the associated change in regional climate from wet to dry; and (3) glacial-interglacial variability through the Pleistocene until present day. Availability of high resolution and extensive 3D seismic data provides a unique opportunity to investigate the evolution of these reefs using seismic stratigraphy and seismic geomorphology. Four main phases of carbonate factory evolution (Phase I-IV) were identified from the Miocene to present. A chrono-stratigraphic framework is constructed, detailing relative sea-level (RSL) changes and the impact of global (e.g., climate, eustasy) and regional (e.g., tectonics, oceanography) forcing parameters on their development. Seismic stratigraphy reveals that despite rapid accommodation rate changes, the oceanographic setting, antecedent topography and rapid vertical reef accretion played a key role in the persistence of Scott Reefs. It is likely that the Indonesian throughflow (ITF) current has been a critical component in controlling the local climate. The Leeuwin current, tides, swells and wind regimes similarly exert a major influence on the NWS climate, whilst the inter-reef channel likely bypassed terrigenous sediment influx away from the reefs, avoiding periods of inundation during wet climates. Seismic stratigraphy Seismic geomorphology Carbonate platform Coral reefs Tectono-stratigraphy Paleo-environmental reconstruction Chrono-stratigraphic framework Paumard, Victorien verfasserin aut Webster, Jody M. verfasserin aut Leonard, Jonathon verfasserin aut Salles, Tristan verfasserin aut O'Leary, Michael verfasserin aut Lang, Simon verfasserin aut Enthalten in Marine and petroleum geology Amsterdam [u.a.] : Elsevier Science, 1984 151 Online-Ressource (DE-627)303393416 (DE-600)1494910-6 (DE-576)259484032 0264-8172 nnns volume:151 GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2088 GBV_ILN_2106 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.48 Marine Geologie VZ 38.51 Geologie fossiler Brennstoffe VZ AR 151 |
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Enthalten in Marine and petroleum geology 151 volume:151 |
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Seismic stratigraphy Seismic geomorphology Carbonate platform Coral reefs Tectono-stratigraphy Paleo-environmental reconstruction Chrono-stratigraphic framework |
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Williams, Carra @@aut@@ Paumard, Victorien @@aut@@ Webster, Jody M. @@aut@@ Leonard, Jonathon @@aut@@ Salles, Tristan @@aut@@ O'Leary, Michael @@aut@@ Lang, Simon @@aut@@ |
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Williams, Carra ddc 550 bkl 38.48 bkl 38.51 misc Seismic stratigraphy misc Seismic geomorphology misc Carbonate platform misc Coral reefs misc Tectono-stratigraphy misc Paleo-environmental reconstruction misc Chrono-stratigraphic framework Environmental controls on the resilience of Scott Reefs since the Miocene (North West Shelf, Australia): Insights from 3D seismic data |
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550 VZ 38.48 bkl 38.51 bkl Environmental controls on the resilience of Scott Reefs since the Miocene (North West Shelf, Australia): Insights from 3D seismic data Seismic stratigraphy Seismic geomorphology Carbonate platform Coral reefs Tectono-stratigraphy Paleo-environmental reconstruction Chrono-stratigraphic framework |
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ddc 550 bkl 38.48 bkl 38.51 misc Seismic stratigraphy misc Seismic geomorphology misc Carbonate platform misc Coral reefs misc Tectono-stratigraphy misc Paleo-environmental reconstruction misc Chrono-stratigraphic framework |
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Environmental controls on the resilience of Scott Reefs since the Miocene (North West Shelf, Australia): Insights from 3D seismic data |
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Environmental controls on the resilience of Scott Reefs since the Miocene (North West Shelf, Australia): Insights from 3D seismic data |
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Williams, Carra Paumard, Victorien Webster, Jody M. Leonard, Jonathon Salles, Tristan O'Leary, Michael Lang, Simon |
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environmental controls on the resilience of scott reefs since the miocene (north west shelf, australia): insights from 3d seismic data |
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Environmental controls on the resilience of Scott Reefs since the Miocene (North West Shelf, Australia): Insights from 3D seismic data |
| abstract |
North and South Scott Reefs are isolated carbonate platforms separated by an inter-reef channel on the NWS, Australia. They evolved from a barrier reef in the Miocene, and into isolated carbonate build-ups (ICB's) during the Pliocene, and finally to the isolated carbonate platforms that continued to present day. However, the timings of coral reef turn on and off are not well constrained with respect to global climatic changes in this region. The North West Shelf (NWS) of Australia recorded marked climatic and oceanographic changes through the Cenozoic. For example: (1) the Mid Miocene Climatic Optimum (MMCO), leading to the onset of ICB's and carbonate platform development; (2) the Mid Pleistocene Transition (MPT) (ca. 0.8–0.6 Ma) and the associated change in regional climate from wet to dry; and (3) glacial-interglacial variability through the Pleistocene until present day. Availability of high resolution and extensive 3D seismic data provides a unique opportunity to investigate the evolution of these reefs using seismic stratigraphy and seismic geomorphology. Four main phases of carbonate factory evolution (Phase I-IV) were identified from the Miocene to present. A chrono-stratigraphic framework is constructed, detailing relative sea-level (RSL) changes and the impact of global (e.g., climate, eustasy) and regional (e.g., tectonics, oceanography) forcing parameters on their development. Seismic stratigraphy reveals that despite rapid accommodation rate changes, the oceanographic setting, antecedent topography and rapid vertical reef accretion played a key role in the persistence of Scott Reefs. It is likely that the Indonesian throughflow (ITF) current has been a critical component in controlling the local climate. The Leeuwin current, tides, swells and wind regimes similarly exert a major influence on the NWS climate, whilst the inter-reef channel likely bypassed terrigenous sediment influx away from the reefs, avoiding periods of inundation during wet climates. |
| abstractGer |
North and South Scott Reefs are isolated carbonate platforms separated by an inter-reef channel on the NWS, Australia. They evolved from a barrier reef in the Miocene, and into isolated carbonate build-ups (ICB's) during the Pliocene, and finally to the isolated carbonate platforms that continued to present day. However, the timings of coral reef turn on and off are not well constrained with respect to global climatic changes in this region. The North West Shelf (NWS) of Australia recorded marked climatic and oceanographic changes through the Cenozoic. For example: (1) the Mid Miocene Climatic Optimum (MMCO), leading to the onset of ICB's and carbonate platform development; (2) the Mid Pleistocene Transition (MPT) (ca. 0.8–0.6 Ma) and the associated change in regional climate from wet to dry; and (3) glacial-interglacial variability through the Pleistocene until present day. Availability of high resolution and extensive 3D seismic data provides a unique opportunity to investigate the evolution of these reefs using seismic stratigraphy and seismic geomorphology. Four main phases of carbonate factory evolution (Phase I-IV) were identified from the Miocene to present. A chrono-stratigraphic framework is constructed, detailing relative sea-level (RSL) changes and the impact of global (e.g., climate, eustasy) and regional (e.g., tectonics, oceanography) forcing parameters on their development. Seismic stratigraphy reveals that despite rapid accommodation rate changes, the oceanographic setting, antecedent topography and rapid vertical reef accretion played a key role in the persistence of Scott Reefs. It is likely that the Indonesian throughflow (ITF) current has been a critical component in controlling the local climate. The Leeuwin current, tides, swells and wind regimes similarly exert a major influence on the NWS climate, whilst the inter-reef channel likely bypassed terrigenous sediment influx away from the reefs, avoiding periods of inundation during wet climates. |
| abstract_unstemmed |
North and South Scott Reefs are isolated carbonate platforms separated by an inter-reef channel on the NWS, Australia. They evolved from a barrier reef in the Miocene, and into isolated carbonate build-ups (ICB's) during the Pliocene, and finally to the isolated carbonate platforms that continued to present day. However, the timings of coral reef turn on and off are not well constrained with respect to global climatic changes in this region. The North West Shelf (NWS) of Australia recorded marked climatic and oceanographic changes through the Cenozoic. For example: (1) the Mid Miocene Climatic Optimum (MMCO), leading to the onset of ICB's and carbonate platform development; (2) the Mid Pleistocene Transition (MPT) (ca. 0.8–0.6 Ma) and the associated change in regional climate from wet to dry; and (3) glacial-interglacial variability through the Pleistocene until present day. Availability of high resolution and extensive 3D seismic data provides a unique opportunity to investigate the evolution of these reefs using seismic stratigraphy and seismic geomorphology. Four main phases of carbonate factory evolution (Phase I-IV) were identified from the Miocene to present. A chrono-stratigraphic framework is constructed, detailing relative sea-level (RSL) changes and the impact of global (e.g., climate, eustasy) and regional (e.g., tectonics, oceanography) forcing parameters on their development. Seismic stratigraphy reveals that despite rapid accommodation rate changes, the oceanographic setting, antecedent topography and rapid vertical reef accretion played a key role in the persistence of Scott Reefs. It is likely that the Indonesian throughflow (ITF) current has been a critical component in controlling the local climate. The Leeuwin current, tides, swells and wind regimes similarly exert a major influence on the NWS climate, whilst the inter-reef channel likely bypassed terrigenous sediment influx away from the reefs, avoiding periods of inundation during wet climates. |
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Environmental controls on the resilience of Scott Reefs since the Miocene (North West Shelf, Australia): Insights from 3D seismic data |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">ELV009563091</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230927085915.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">230511s2023 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.marpetgeo.2023.106188</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV009563091</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S0264-8172(23)00094-6</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rda</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.48</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.51</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Williams, Carra</subfield><subfield code="e">verfasserin</subfield><subfield code="0">(orcid)0000-0002-1312-4438</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Environmental controls on the resilience of Scott Reefs since the Miocene (North West Shelf, Australia): Insights from 3D seismic data</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2023</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">North and South Scott Reefs are isolated carbonate platforms separated by an inter-reef channel on the NWS, Australia. They evolved from a barrier reef in the Miocene, and into isolated carbonate build-ups (ICB's) during the Pliocene, and finally to the isolated carbonate platforms that continued to present day. However, the timings of coral reef turn on and off are not well constrained with respect to global climatic changes in this region. The North West Shelf (NWS) of Australia recorded marked climatic and oceanographic changes through the Cenozoic. For example: (1) the Mid Miocene Climatic Optimum (MMCO), leading to the onset of ICB's and carbonate platform development; (2) the Mid Pleistocene Transition (MPT) (ca. 0.8–0.6 Ma) and the associated change in regional climate from wet to dry; and (3) glacial-interglacial variability through the Pleistocene until present day. Availability of high resolution and extensive 3D seismic data provides a unique opportunity to investigate the evolution of these reefs using seismic stratigraphy and seismic geomorphology. Four main phases of carbonate factory evolution (Phase I-IV) were identified from the Miocene to present. A chrono-stratigraphic framework is constructed, detailing relative sea-level (RSL) changes and the impact of global (e.g., climate, eustasy) and regional (e.g., tectonics, oceanography) forcing parameters on their development. Seismic stratigraphy reveals that despite rapid accommodation rate changes, the oceanographic setting, antecedent topography and rapid vertical reef accretion played a key role in the persistence of Scott Reefs. It is likely that the Indonesian throughflow (ITF) current has been a critical component in controlling the local climate. The Leeuwin current, tides, swells and wind regimes similarly exert a major influence on the NWS climate, whilst the inter-reef channel likely bypassed terrigenous sediment influx away from the reefs, avoiding periods of inundation during wet climates.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Seismic stratigraphy</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Seismic geomorphology</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Carbonate platform</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Coral reefs</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Tectono-stratigraphy</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Paleo-environmental reconstruction</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Chrono-stratigraphic 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