Evolution of the Late Miocene Mediterranean–Atlantic gateways and their impact on regional and global environmental change
Marine gateways play a critical role in the exchange of water, heat, salt and nutrients between oceans and seas. As a result, changes in gateway geometry can significantly alter both the pattern of global ocean circulation and associated heat transport and climate, as well as having a profound impac...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Flecker, Rachel [verfasserIn] |
|---|
| Format: |
E-Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2015transfer abstract |
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| Umfang: |
28 |
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| Übergeordnetes Werk: |
Enthalten in: Hydrophobic and antimicrobial dentin: A peptide-based 2-tier protective system for dental resin composite restorations - Moussa, Dina G. ELSEVIER, 2019, Amsterdam [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:150 ; year:2015 ; pages:365-392 ; extent:28 |
| Links: |
|---|
| DOI / URN: |
10.1016/j.earscirev.2015.08.007 |
|---|
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ELV018881440 |
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| 520 | |a Marine gateways play a critical role in the exchange of water, heat, salt and nutrients between oceans and seas. As a result, changes in gateway geometry can significantly alter both the pattern of global ocean circulation and associated heat transport and climate, as well as having a profound impact on local environmental conditions. Mediterranean–Atlantic marine corridors that pre-date the modern Gibraltar Strait, closed during the Late Miocene and are now exposed on land in northern Morocco and southern Spain. The restriction and closure of these Miocene connections resulted in extreme salinity fluctuations in the Mediterranean, leading to the precipitation of thick evaporites. This event is known as the Messinian Salinity Crisis (MSC). The evolution and closure of the Mediterranean–Atlantic gateways are a critical control on the MSC, but at present the location, geometry and age of these gateways are still highly controversial, as is the impact of changing Mediterranean outflow on Northern Hemisphere circulation. Here, we present a comprehensive overview of the evolution of the Late Miocene gateways and the nature of Mediterranean–Atlantic exchange as deduced from published studies focussed both on the sediments preserved within the fossil corridors and inferences that can be derived from data in the adjacent basins. We also consider the possible impact of evolving exchange on both the Mediterranean and global climate and highlight the main enduring challenges for reconstructing past Mediterranean–Atlantic exchange. | ||
| 520 | |a Marine gateways play a critical role in the exchange of water, heat, salt and nutrients between oceans and seas. As a result, changes in gateway geometry can significantly alter both the pattern of global ocean circulation and associated heat transport and climate, as well as having a profound impact on local environmental conditions. Mediterranean–Atlantic marine corridors that pre-date the modern Gibraltar Strait, closed during the Late Miocene and are now exposed on land in northern Morocco and southern Spain. The restriction and closure of these Miocene connections resulted in extreme salinity fluctuations in the Mediterranean, leading to the precipitation of thick evaporites. This event is known as the Messinian Salinity Crisis (MSC). The evolution and closure of the Mediterranean–Atlantic gateways are a critical control on the MSC, but at present the location, geometry and age of these gateways are still highly controversial, as is the impact of changing Mediterranean outflow on Northern Hemisphere circulation. Here, we present a comprehensive overview of the evolution of the Late Miocene gateways and the nature of Mediterranean–Atlantic exchange as deduced from published studies focussed both on the sediments preserved within the fossil corridors and inferences that can be derived from data in the adjacent basins. We also consider the possible impact of evolving exchange on both the Mediterranean and global climate and highlight the main enduring challenges for reconstructing past Mediterranean–Atlantic exchange. | ||
| 700 | 1 | |a Krijgsman, Wout |4 oth | |
| 700 | 1 | |a Capella, Walter |4 oth | |
| 700 | 1 | |a de Castro Martíns, Cesar |4 oth | |
| 700 | 1 | |a Dmitrieva, Evelina |4 oth | |
| 700 | 1 | |a Mayser, Jan Peter |4 oth | |
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| 700 | 1 | |a Modestou, Sevasti |4 oth | |
| 700 | 1 | |a Ochoa, Diana |4 oth | |
| 700 | 1 | |a Simon, Dirk |4 oth | |
| 700 | 1 | |a Tulbure, Maria |4 oth | |
| 700 | 1 | |a van den Berg, Bas |4 oth | |
| 700 | 1 | |a van der Schee, Marlies |4 oth | |
| 700 | 1 | |a de Lange, Gert |4 oth | |
| 700 | 1 | |a Ellam, Robert |4 oth | |
| 700 | 1 | |a Govers, Rob |4 oth | |
| 700 | 1 | |a Gutjahr, Marcus |4 oth | |
| 700 | 1 | |a Hilgen, Frits |4 oth | |
| 700 | 1 | |a Kouwenhoven, Tanja |4 oth | |
| 700 | 1 | |a Lofi, Johanna |4 oth | |
| 700 | 1 | |a Meijer, Paul |4 oth | |
| 700 | 1 | |a Sierro, Francisco J. |4 oth | |
| 700 | 1 | |a Bachiri, Naima |4 oth | |
| 700 | 1 | |a Barhoun, Nadia |4 oth | |
| 700 | 1 | |a Alami, Abdelwahid Chakor |4 oth | |
| 700 | 1 | |a Chacon, Beatriz |4 oth | |
| 700 | 1 | |a Flores, Jose A. |4 oth | |
| 700 | 1 | |a Gregory, John |4 oth | |
| 700 | 1 | |a Howard, James |4 oth | |
| 700 | 1 | |a Lunt, Dan |4 oth | |
| 700 | 1 | |a Ochoa, Maria |4 oth | |
| 700 | 1 | |a Pancost, Rich |4 oth | |
| 700 | 1 | |a Vincent, Stephen |4 oth | |
| 700 | 1 | |a Yousfi, Mohamed Zakaria |4 oth | |
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10.1016/j.earscirev.2015.08.007 doi GBVA2015021000003.pica (DE-627)ELV018881440 (ELSEVIER)S0012-8252(15)30031-3 DE-627 ger DE-627 rakwb eng 550 550 DE-600 530 VZ 35.18 bkl 44.09 bkl Flecker, Rachel verfasserin aut Evolution of the Late Miocene Mediterranean–Atlantic gateways and their impact on regional and global environmental change 2015transfer abstract 28 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Marine gateways play a critical role in the exchange of water, heat, salt and nutrients between oceans and seas. As a result, changes in gateway geometry can significantly alter both the pattern of global ocean circulation and associated heat transport and climate, as well as having a profound impact on local environmental conditions. Mediterranean–Atlantic marine corridors that pre-date the modern Gibraltar Strait, closed during the Late Miocene and are now exposed on land in northern Morocco and southern Spain. The restriction and closure of these Miocene connections resulted in extreme salinity fluctuations in the Mediterranean, leading to the precipitation of thick evaporites. This event is known as the Messinian Salinity Crisis (MSC). The evolution and closure of the Mediterranean–Atlantic gateways are a critical control on the MSC, but at present the location, geometry and age of these gateways are still highly controversial, as is the impact of changing Mediterranean outflow on Northern Hemisphere circulation. Here, we present a comprehensive overview of the evolution of the Late Miocene gateways and the nature of Mediterranean–Atlantic exchange as deduced from published studies focussed both on the sediments preserved within the fossil corridors and inferences that can be derived from data in the adjacent basins. We also consider the possible impact of evolving exchange on both the Mediterranean and global climate and highlight the main enduring challenges for reconstructing past Mediterranean–Atlantic exchange. Marine gateways play a critical role in the exchange of water, heat, salt and nutrients between oceans and seas. As a result, changes in gateway geometry can significantly alter both the pattern of global ocean circulation and associated heat transport and climate, as well as having a profound impact on local environmental conditions. Mediterranean–Atlantic marine corridors that pre-date the modern Gibraltar Strait, closed during the Late Miocene and are now exposed on land in northern Morocco and southern Spain. The restriction and closure of these Miocene connections resulted in extreme salinity fluctuations in the Mediterranean, leading to the precipitation of thick evaporites. This event is known as the Messinian Salinity Crisis (MSC). The evolution and closure of the Mediterranean–Atlantic gateways are a critical control on the MSC, but at present the location, geometry and age of these gateways are still highly controversial, as is the impact of changing Mediterranean outflow on Northern Hemisphere circulation. Here, we present a comprehensive overview of the evolution of the Late Miocene gateways and the nature of Mediterranean–Atlantic exchange as deduced from published studies focussed both on the sediments preserved within the fossil corridors and inferences that can be derived from data in the adjacent basins. We also consider the possible impact of evolving exchange on both the Mediterranean and global climate and highlight the main enduring challenges for reconstructing past Mediterranean–Atlantic exchange. Krijgsman, Wout oth Capella, Walter oth de Castro Martíns, Cesar oth Dmitrieva, Evelina oth Mayser, Jan Peter oth Marzocchi, Alice oth Modestou, Sevasti oth Ochoa, Diana oth Simon, Dirk oth Tulbure, Maria oth van den Berg, Bas oth van der Schee, Marlies oth de Lange, Gert oth Ellam, Robert oth Govers, Rob oth Gutjahr, Marcus oth Hilgen, Frits oth Kouwenhoven, Tanja oth Lofi, Johanna oth Meijer, Paul oth Sierro, Francisco J. oth Bachiri, Naima oth Barhoun, Nadia oth Alami, Abdelwahid Chakor oth Chacon, Beatriz oth Flores, Jose A. oth Gregory, John oth Howard, James oth Lunt, Dan oth Ochoa, Maria oth Pancost, Rich oth Vincent, Stephen oth Yousfi, Mohamed Zakaria oth Enthalten in Elsevier Moussa, Dina G. ELSEVIER Hydrophobic and antimicrobial dentin: A peptide-based 2-tier protective system for dental resin composite restorations 2019 Amsterdam [u.a.] (DE-627)ELV001972944 volume:150 year:2015 pages:365-392 extent:28 https://doi.org/10.1016/j.earscirev.2015.08.007 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 35.18 Kolloidchemie Grenzflächenchemie VZ 44.09 Medizintechnik VZ AR 150 2015 365-392 28 045F 550 |
| spelling |
10.1016/j.earscirev.2015.08.007 doi GBVA2015021000003.pica (DE-627)ELV018881440 (ELSEVIER)S0012-8252(15)30031-3 DE-627 ger DE-627 rakwb eng 550 550 DE-600 530 VZ 35.18 bkl 44.09 bkl Flecker, Rachel verfasserin aut Evolution of the Late Miocene Mediterranean–Atlantic gateways and their impact on regional and global environmental change 2015transfer abstract 28 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Marine gateways play a critical role in the exchange of water, heat, salt and nutrients between oceans and seas. As a result, changes in gateway geometry can significantly alter both the pattern of global ocean circulation and associated heat transport and climate, as well as having a profound impact on local environmental conditions. Mediterranean–Atlantic marine corridors that pre-date the modern Gibraltar Strait, closed during the Late Miocene and are now exposed on land in northern Morocco and southern Spain. The restriction and closure of these Miocene connections resulted in extreme salinity fluctuations in the Mediterranean, leading to the precipitation of thick evaporites. This event is known as the Messinian Salinity Crisis (MSC). The evolution and closure of the Mediterranean–Atlantic gateways are a critical control on the MSC, but at present the location, geometry and age of these gateways are still highly controversial, as is the impact of changing Mediterranean outflow on Northern Hemisphere circulation. Here, we present a comprehensive overview of the evolution of the Late Miocene gateways and the nature of Mediterranean–Atlantic exchange as deduced from published studies focussed both on the sediments preserved within the fossil corridors and inferences that can be derived from data in the adjacent basins. We also consider the possible impact of evolving exchange on both the Mediterranean and global climate and highlight the main enduring challenges for reconstructing past Mediterranean–Atlantic exchange. Marine gateways play a critical role in the exchange of water, heat, salt and nutrients between oceans and seas. As a result, changes in gateway geometry can significantly alter both the pattern of global ocean circulation and associated heat transport and climate, as well as having a profound impact on local environmental conditions. Mediterranean–Atlantic marine corridors that pre-date the modern Gibraltar Strait, closed during the Late Miocene and are now exposed on land in northern Morocco and southern Spain. The restriction and closure of these Miocene connections resulted in extreme salinity fluctuations in the Mediterranean, leading to the precipitation of thick evaporites. This event is known as the Messinian Salinity Crisis (MSC). The evolution and closure of the Mediterranean–Atlantic gateways are a critical control on the MSC, but at present the location, geometry and age of these gateways are still highly controversial, as is the impact of changing Mediterranean outflow on Northern Hemisphere circulation. Here, we present a comprehensive overview of the evolution of the Late Miocene gateways and the nature of Mediterranean–Atlantic exchange as deduced from published studies focussed both on the sediments preserved within the fossil corridors and inferences that can be derived from data in the adjacent basins. We also consider the possible impact of evolving exchange on both the Mediterranean and global climate and highlight the main enduring challenges for reconstructing past Mediterranean–Atlantic exchange. Krijgsman, Wout oth Capella, Walter oth de Castro Martíns, Cesar oth Dmitrieva, Evelina oth Mayser, Jan Peter oth Marzocchi, Alice oth Modestou, Sevasti oth Ochoa, Diana oth Simon, Dirk oth Tulbure, Maria oth van den Berg, Bas oth van der Schee, Marlies oth de Lange, Gert oth Ellam, Robert oth Govers, Rob oth Gutjahr, Marcus oth Hilgen, Frits oth Kouwenhoven, Tanja oth Lofi, Johanna oth Meijer, Paul oth Sierro, Francisco J. oth Bachiri, Naima oth Barhoun, Nadia oth Alami, Abdelwahid Chakor oth Chacon, Beatriz oth Flores, Jose A. oth Gregory, John oth Howard, James oth Lunt, Dan oth Ochoa, Maria oth Pancost, Rich oth Vincent, Stephen oth Yousfi, Mohamed Zakaria oth Enthalten in Elsevier Moussa, Dina G. ELSEVIER Hydrophobic and antimicrobial dentin: A peptide-based 2-tier protective system for dental resin composite restorations 2019 Amsterdam [u.a.] (DE-627)ELV001972944 volume:150 year:2015 pages:365-392 extent:28 https://doi.org/10.1016/j.earscirev.2015.08.007 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 35.18 Kolloidchemie Grenzflächenchemie VZ 44.09 Medizintechnik VZ AR 150 2015 365-392 28 045F 550 |
| allfields_unstemmed |
10.1016/j.earscirev.2015.08.007 doi GBVA2015021000003.pica (DE-627)ELV018881440 (ELSEVIER)S0012-8252(15)30031-3 DE-627 ger DE-627 rakwb eng 550 550 DE-600 530 VZ 35.18 bkl 44.09 bkl Flecker, Rachel verfasserin aut Evolution of the Late Miocene Mediterranean–Atlantic gateways and their impact on regional and global environmental change 2015transfer abstract 28 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Marine gateways play a critical role in the exchange of water, heat, salt and nutrients between oceans and seas. As a result, changes in gateway geometry can significantly alter both the pattern of global ocean circulation and associated heat transport and climate, as well as having a profound impact on local environmental conditions. Mediterranean–Atlantic marine corridors that pre-date the modern Gibraltar Strait, closed during the Late Miocene and are now exposed on land in northern Morocco and southern Spain. The restriction and closure of these Miocene connections resulted in extreme salinity fluctuations in the Mediterranean, leading to the precipitation of thick evaporites. This event is known as the Messinian Salinity Crisis (MSC). The evolution and closure of the Mediterranean–Atlantic gateways are a critical control on the MSC, but at present the location, geometry and age of these gateways are still highly controversial, as is the impact of changing Mediterranean outflow on Northern Hemisphere circulation. Here, we present a comprehensive overview of the evolution of the Late Miocene gateways and the nature of Mediterranean–Atlantic exchange as deduced from published studies focussed both on the sediments preserved within the fossil corridors and inferences that can be derived from data in the adjacent basins. We also consider the possible impact of evolving exchange on both the Mediterranean and global climate and highlight the main enduring challenges for reconstructing past Mediterranean–Atlantic exchange. Marine gateways play a critical role in the exchange of water, heat, salt and nutrients between oceans and seas. As a result, changes in gateway geometry can significantly alter both the pattern of global ocean circulation and associated heat transport and climate, as well as having a profound impact on local environmental conditions. Mediterranean–Atlantic marine corridors that pre-date the modern Gibraltar Strait, closed during the Late Miocene and are now exposed on land in northern Morocco and southern Spain. The restriction and closure of these Miocene connections resulted in extreme salinity fluctuations in the Mediterranean, leading to the precipitation of thick evaporites. This event is known as the Messinian Salinity Crisis (MSC). The evolution and closure of the Mediterranean–Atlantic gateways are a critical control on the MSC, but at present the location, geometry and age of these gateways are still highly controversial, as is the impact of changing Mediterranean outflow on Northern Hemisphere circulation. Here, we present a comprehensive overview of the evolution of the Late Miocene gateways and the nature of Mediterranean–Atlantic exchange as deduced from published studies focussed both on the sediments preserved within the fossil corridors and inferences that can be derived from data in the adjacent basins. We also consider the possible impact of evolving exchange on both the Mediterranean and global climate and highlight the main enduring challenges for reconstructing past Mediterranean–Atlantic exchange. Krijgsman, Wout oth Capella, Walter oth de Castro Martíns, Cesar oth Dmitrieva, Evelina oth Mayser, Jan Peter oth Marzocchi, Alice oth Modestou, Sevasti oth Ochoa, Diana oth Simon, Dirk oth Tulbure, Maria oth van den Berg, Bas oth van der Schee, Marlies oth de Lange, Gert oth Ellam, Robert oth Govers, Rob oth Gutjahr, Marcus oth Hilgen, Frits oth Kouwenhoven, Tanja oth Lofi, Johanna oth Meijer, Paul oth Sierro, Francisco J. oth Bachiri, Naima oth Barhoun, Nadia oth Alami, Abdelwahid Chakor oth Chacon, Beatriz oth Flores, Jose A. oth Gregory, John oth Howard, James oth Lunt, Dan oth Ochoa, Maria oth Pancost, Rich oth Vincent, Stephen oth Yousfi, Mohamed Zakaria oth Enthalten in Elsevier Moussa, Dina G. ELSEVIER Hydrophobic and antimicrobial dentin: A peptide-based 2-tier protective system for dental resin composite restorations 2019 Amsterdam [u.a.] (DE-627)ELV001972944 volume:150 year:2015 pages:365-392 extent:28 https://doi.org/10.1016/j.earscirev.2015.08.007 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 35.18 Kolloidchemie Grenzflächenchemie VZ 44.09 Medizintechnik VZ AR 150 2015 365-392 28 045F 550 |
| allfieldsGer |
10.1016/j.earscirev.2015.08.007 doi GBVA2015021000003.pica (DE-627)ELV018881440 (ELSEVIER)S0012-8252(15)30031-3 DE-627 ger DE-627 rakwb eng 550 550 DE-600 530 VZ 35.18 bkl 44.09 bkl Flecker, Rachel verfasserin aut Evolution of the Late Miocene Mediterranean–Atlantic gateways and their impact on regional and global environmental change 2015transfer abstract 28 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Marine gateways play a critical role in the exchange of water, heat, salt and nutrients between oceans and seas. As a result, changes in gateway geometry can significantly alter both the pattern of global ocean circulation and associated heat transport and climate, as well as having a profound impact on local environmental conditions. Mediterranean–Atlantic marine corridors that pre-date the modern Gibraltar Strait, closed during the Late Miocene and are now exposed on land in northern Morocco and southern Spain. The restriction and closure of these Miocene connections resulted in extreme salinity fluctuations in the Mediterranean, leading to the precipitation of thick evaporites. This event is known as the Messinian Salinity Crisis (MSC). The evolution and closure of the Mediterranean–Atlantic gateways are a critical control on the MSC, but at present the location, geometry and age of these gateways are still highly controversial, as is the impact of changing Mediterranean outflow on Northern Hemisphere circulation. Here, we present a comprehensive overview of the evolution of the Late Miocene gateways and the nature of Mediterranean–Atlantic exchange as deduced from published studies focussed both on the sediments preserved within the fossil corridors and inferences that can be derived from data in the adjacent basins. We also consider the possible impact of evolving exchange on both the Mediterranean and global climate and highlight the main enduring challenges for reconstructing past Mediterranean–Atlantic exchange. Marine gateways play a critical role in the exchange of water, heat, salt and nutrients between oceans and seas. As a result, changes in gateway geometry can significantly alter both the pattern of global ocean circulation and associated heat transport and climate, as well as having a profound impact on local environmental conditions. Mediterranean–Atlantic marine corridors that pre-date the modern Gibraltar Strait, closed during the Late Miocene and are now exposed on land in northern Morocco and southern Spain. The restriction and closure of these Miocene connections resulted in extreme salinity fluctuations in the Mediterranean, leading to the precipitation of thick evaporites. This event is known as the Messinian Salinity Crisis (MSC). The evolution and closure of the Mediterranean–Atlantic gateways are a critical control on the MSC, but at present the location, geometry and age of these gateways are still highly controversial, as is the impact of changing Mediterranean outflow on Northern Hemisphere circulation. Here, we present a comprehensive overview of the evolution of the Late Miocene gateways and the nature of Mediterranean–Atlantic exchange as deduced from published studies focussed both on the sediments preserved within the fossil corridors and inferences that can be derived from data in the adjacent basins. We also consider the possible impact of evolving exchange on both the Mediterranean and global climate and highlight the main enduring challenges for reconstructing past Mediterranean–Atlantic exchange. Krijgsman, Wout oth Capella, Walter oth de Castro Martíns, Cesar oth Dmitrieva, Evelina oth Mayser, Jan Peter oth Marzocchi, Alice oth Modestou, Sevasti oth Ochoa, Diana oth Simon, Dirk oth Tulbure, Maria oth van den Berg, Bas oth van der Schee, Marlies oth de Lange, Gert oth Ellam, Robert oth Govers, Rob oth Gutjahr, Marcus oth Hilgen, Frits oth Kouwenhoven, Tanja oth Lofi, Johanna oth Meijer, Paul oth Sierro, Francisco J. oth Bachiri, Naima oth Barhoun, Nadia oth Alami, Abdelwahid Chakor oth Chacon, Beatriz oth Flores, Jose A. oth Gregory, John oth Howard, James oth Lunt, Dan oth Ochoa, Maria oth Pancost, Rich oth Vincent, Stephen oth Yousfi, Mohamed Zakaria oth Enthalten in Elsevier Moussa, Dina G. ELSEVIER Hydrophobic and antimicrobial dentin: A peptide-based 2-tier protective system for dental resin composite restorations 2019 Amsterdam [u.a.] (DE-627)ELV001972944 volume:150 year:2015 pages:365-392 extent:28 https://doi.org/10.1016/j.earscirev.2015.08.007 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 35.18 Kolloidchemie Grenzflächenchemie VZ 44.09 Medizintechnik VZ AR 150 2015 365-392 28 045F 550 |
| allfieldsSound |
10.1016/j.earscirev.2015.08.007 doi GBVA2015021000003.pica (DE-627)ELV018881440 (ELSEVIER)S0012-8252(15)30031-3 DE-627 ger DE-627 rakwb eng 550 550 DE-600 530 VZ 35.18 bkl 44.09 bkl Flecker, Rachel verfasserin aut Evolution of the Late Miocene Mediterranean–Atlantic gateways and their impact on regional and global environmental change 2015transfer abstract 28 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Marine gateways play a critical role in the exchange of water, heat, salt and nutrients between oceans and seas. As a result, changes in gateway geometry can significantly alter both the pattern of global ocean circulation and associated heat transport and climate, as well as having a profound impact on local environmental conditions. Mediterranean–Atlantic marine corridors that pre-date the modern Gibraltar Strait, closed during the Late Miocene and are now exposed on land in northern Morocco and southern Spain. The restriction and closure of these Miocene connections resulted in extreme salinity fluctuations in the Mediterranean, leading to the precipitation of thick evaporites. This event is known as the Messinian Salinity Crisis (MSC). The evolution and closure of the Mediterranean–Atlantic gateways are a critical control on the MSC, but at present the location, geometry and age of these gateways are still highly controversial, as is the impact of changing Mediterranean outflow on Northern Hemisphere circulation. Here, we present a comprehensive overview of the evolution of the Late Miocene gateways and the nature of Mediterranean–Atlantic exchange as deduced from published studies focussed both on the sediments preserved within the fossil corridors and inferences that can be derived from data in the adjacent basins. We also consider the possible impact of evolving exchange on both the Mediterranean and global climate and highlight the main enduring challenges for reconstructing past Mediterranean–Atlantic exchange. Marine gateways play a critical role in the exchange of water, heat, salt and nutrients between oceans and seas. As a result, changes in gateway geometry can significantly alter both the pattern of global ocean circulation and associated heat transport and climate, as well as having a profound impact on local environmental conditions. Mediterranean–Atlantic marine corridors that pre-date the modern Gibraltar Strait, closed during the Late Miocene and are now exposed on land in northern Morocco and southern Spain. The restriction and closure of these Miocene connections resulted in extreme salinity fluctuations in the Mediterranean, leading to the precipitation of thick evaporites. This event is known as the Messinian Salinity Crisis (MSC). The evolution and closure of the Mediterranean–Atlantic gateways are a critical control on the MSC, but at present the location, geometry and age of these gateways are still highly controversial, as is the impact of changing Mediterranean outflow on Northern Hemisphere circulation. Here, we present a comprehensive overview of the evolution of the Late Miocene gateways and the nature of Mediterranean–Atlantic exchange as deduced from published studies focussed both on the sediments preserved within the fossil corridors and inferences that can be derived from data in the adjacent basins. We also consider the possible impact of evolving exchange on both the Mediterranean and global climate and highlight the main enduring challenges for reconstructing past Mediterranean–Atlantic exchange. Krijgsman, Wout oth Capella, Walter oth de Castro Martíns, Cesar oth Dmitrieva, Evelina oth Mayser, Jan Peter oth Marzocchi, Alice oth Modestou, Sevasti oth Ochoa, Diana oth Simon, Dirk oth Tulbure, Maria oth van den Berg, Bas oth van der Schee, Marlies oth de Lange, Gert oth Ellam, Robert oth Govers, Rob oth Gutjahr, Marcus oth Hilgen, Frits oth Kouwenhoven, Tanja oth Lofi, Johanna oth Meijer, Paul oth Sierro, Francisco J. oth Bachiri, Naima oth Barhoun, Nadia oth Alami, Abdelwahid Chakor oth Chacon, Beatriz oth Flores, Jose A. oth Gregory, John oth Howard, James oth Lunt, Dan oth Ochoa, Maria oth Pancost, Rich oth Vincent, Stephen oth Yousfi, Mohamed Zakaria oth Enthalten in Elsevier Moussa, Dina G. ELSEVIER Hydrophobic and antimicrobial dentin: A peptide-based 2-tier protective system for dental resin composite restorations 2019 Amsterdam [u.a.] (DE-627)ELV001972944 volume:150 year:2015 pages:365-392 extent:28 https://doi.org/10.1016/j.earscirev.2015.08.007 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 35.18 Kolloidchemie Grenzflächenchemie VZ 44.09 Medizintechnik VZ AR 150 2015 365-392 28 045F 550 |
| language |
English |
| source |
Enthalten in Hydrophobic and antimicrobial dentin: A peptide-based 2-tier protective system for dental resin composite restorations Amsterdam [u.a.] volume:150 year:2015 pages:365-392 extent:28 |
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Evolution of the Late Miocene Mediterranean–Atlantic gateways and their impact on regional and global environmental change |
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Marine gateways play a critical role in the exchange of water, heat, salt and nutrients between oceans and seas. As a result, changes in gateway geometry can significantly alter both the pattern of global ocean circulation and associated heat transport and climate, as well as having a profound impact on local environmental conditions. Mediterranean–Atlantic marine corridors that pre-date the modern Gibraltar Strait, closed during the Late Miocene and are now exposed on land in northern Morocco and southern Spain. The restriction and closure of these Miocene connections resulted in extreme salinity fluctuations in the Mediterranean, leading to the precipitation of thick evaporites. This event is known as the Messinian Salinity Crisis (MSC). The evolution and closure of the Mediterranean–Atlantic gateways are a critical control on the MSC, but at present the location, geometry and age of these gateways are still highly controversial, as is the impact of changing Mediterranean outflow on Northern Hemisphere circulation. Here, we present a comprehensive overview of the evolution of the Late Miocene gateways and the nature of Mediterranean–Atlantic exchange as deduced from published studies focussed both on the sediments preserved within the fossil corridors and inferences that can be derived from data in the adjacent basins. We also consider the possible impact of evolving exchange on both the Mediterranean and global climate and highlight the main enduring challenges for reconstructing past Mediterranean–Atlantic exchange. |
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Marine gateways play a critical role in the exchange of water, heat, salt and nutrients between oceans and seas. As a result, changes in gateway geometry can significantly alter both the pattern of global ocean circulation and associated heat transport and climate, as well as having a profound impact on local environmental conditions. Mediterranean–Atlantic marine corridors that pre-date the modern Gibraltar Strait, closed during the Late Miocene and are now exposed on land in northern Morocco and southern Spain. The restriction and closure of these Miocene connections resulted in extreme salinity fluctuations in the Mediterranean, leading to the precipitation of thick evaporites. This event is known as the Messinian Salinity Crisis (MSC). The evolution and closure of the Mediterranean–Atlantic gateways are a critical control on the MSC, but at present the location, geometry and age of these gateways are still highly controversial, as is the impact of changing Mediterranean outflow on Northern Hemisphere circulation. Here, we present a comprehensive overview of the evolution of the Late Miocene gateways and the nature of Mediterranean–Atlantic exchange as deduced from published studies focussed both on the sediments preserved within the fossil corridors and inferences that can be derived from data in the adjacent basins. We also consider the possible impact of evolving exchange on both the Mediterranean and global climate and highlight the main enduring challenges for reconstructing past Mediterranean–Atlantic exchange. |
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Marine gateways play a critical role in the exchange of water, heat, salt and nutrients between oceans and seas. As a result, changes in gateway geometry can significantly alter both the pattern of global ocean circulation and associated heat transport and climate, as well as having a profound impact on local environmental conditions. Mediterranean–Atlantic marine corridors that pre-date the modern Gibraltar Strait, closed during the Late Miocene and are now exposed on land in northern Morocco and southern Spain. The restriction and closure of these Miocene connections resulted in extreme salinity fluctuations in the Mediterranean, leading to the precipitation of thick evaporites. This event is known as the Messinian Salinity Crisis (MSC). The evolution and closure of the Mediterranean–Atlantic gateways are a critical control on the MSC, but at present the location, geometry and age of these gateways are still highly controversial, as is the impact of changing Mediterranean outflow on Northern Hemisphere circulation. Here, we present a comprehensive overview of the evolution of the Late Miocene gateways and the nature of Mediterranean–Atlantic exchange as deduced from published studies focussed both on the sediments preserved within the fossil corridors and inferences that can be derived from data in the adjacent basins. We also consider the possible impact of evolving exchange on both the Mediterranean and global climate and highlight the main enduring challenges for reconstructing past Mediterranean–Atlantic exchange. |
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As a result, changes in gateway geometry can significantly alter both the pattern of global ocean circulation and associated heat transport and climate, as well as having a profound impact on local environmental conditions. Mediterranean–Atlantic marine corridors that pre-date the modern Gibraltar Strait, closed during the Late Miocene and are now exposed on land in northern Morocco and southern Spain. The restriction and closure of these Miocene connections resulted in extreme salinity fluctuations in the Mediterranean, leading to the precipitation of thick evaporites. This event is known as the Messinian Salinity Crisis (MSC). The evolution and closure of the Mediterranean–Atlantic gateways are a critical control on the MSC, but at present the location, geometry and age of these gateways are still highly controversial, as is the impact of changing Mediterranean outflow on Northern Hemisphere circulation. Here, we present a comprehensive overview of the evolution of the Late Miocene gateways and the nature of Mediterranean–Atlantic exchange as deduced from published studies focussed both on the sediments preserved within the fossil corridors and inferences that can be derived from data in the adjacent basins. We also consider the possible impact of evolving exchange on both the Mediterranean and global climate and highlight the main enduring challenges for reconstructing past Mediterranean–Atlantic exchange.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Marine gateways play a critical role in the exchange of water, heat, salt and nutrients between oceans and seas. As a result, changes in gateway geometry can significantly alter both the pattern of global ocean circulation and associated heat transport and climate, as well as having a profound impact on local environmental conditions. Mediterranean–Atlantic marine corridors that pre-date the modern Gibraltar Strait, closed during the Late Miocene and are now exposed on land in northern Morocco and southern Spain. The restriction and closure of these Miocene connections resulted in extreme salinity fluctuations in the Mediterranean, leading to the precipitation of thick evaporites. This event is known as the Messinian Salinity Crisis (MSC). The evolution and closure of the Mediterranean–Atlantic gateways are a critical control on the MSC, but at present the location, geometry and age of these gateways are still highly controversial, as is the impact of changing Mediterranean outflow on Northern Hemisphere circulation. Here, we present a comprehensive overview of the evolution of the Late Miocene gateways and the nature of Mediterranean–Atlantic exchange as deduced from published studies focussed both on the sediments preserved within the fossil corridors and inferences that can be derived from data in the adjacent basins. 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