Late quaternary variability of hydrography and weathering inputs on the SW Iberian shelf from clay minerals and the radiogenic isotopes of neodymium, strontium and lead

The radiogenic isotope systems of neodymium (Nd), strontium (Sr) and lead (Pb) have been used in numerous studies throughout the last decades to investigate water mass circulations of the past and present oceans, and to trace changing contributions of detrital material from different source areas. C...
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Gespeichert in:

Autor*in:	Stumpf, Roland [verfasserIn] Frank, Martin - 1966- [doktorvater]
Hochschulschrift:	Kiel, Univ., Diss., 2011

Format:	E-Book
Sprache:	Englisch

Erschienen:	2011

Schlagwörter:	Iberische Halbinsel / Holozän / Meeressediment / Isotopengeochemie
Formangabe:	Hochschulschrift

Umfang:	Online-Ressource (122 S., 5,98 MB)

Weitere Ausgabe:	Erscheint auch als Druck-Ausgabe Stumpf, Roland: Late Quaternary variability of hydrography and weathering inputs on the SW Iberian shelf from clay minerals and the radiogenic isotopes of neodymium, strontium and lead - 2011

Links:	Link aufrufen Volltext Volltext Volltext

DOI / URN:	urn:nbn:de:gbv:8-diss-65217

Katalog-ID:	66422346X

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Indexfelder

author_variant	r s rs
matchkey_str	stumpfrolandfrankmartin:2011----:aeutrayaibltohdorpynwahrniptotewbrasefrmlyieasnteaig
oclc_num	838016684
hierarchy_sort_str	2011
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publishDate	2011
allfields	11,O07 dnb 1012726614 DE-101 urn:nbn:de:gbv:8-diss-65217 urn (DE-627)66422346X (DE-599)DNB1012726614 (OCoLC)838016684 DE-627 ger DE-627 rakwb eng XA-DE 550 OCLC 550 DNB 14 ssgn 38.88 bkl Stumpf, Roland verfasserin (DE-588)1012637484 (DE-627)662254511 (DE-576)34572934X aut Late quaternary variability of hydrography and weathering inputs on the SW Iberian shelf from clay minerals and the radiogenic isotopes of neodymium, strontium and lead vorgelegt von Roland Stumpf 2011 Online-Ressource (122 S., 5,98 MB) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Kiel, Univ., Diss., 2011 The radiogenic isotope systems of neodymium (Nd), strontium (Sr) and lead (Pb) have been used in numerous studies throughout the last decades to investigate water mass circulations of the past and present oceans, and to trace changing contributions of detrital material from different source areas. Clay mineral assemblages and clay mineral ratios from the fine fraction of marine sediments have also been used to characterize endmember sources. This thesis focuses on a reconstruction of the late Quaternary hydrographic variability of the flow path of the Mediterranean Outflow Water (MOW) and the changing weathering contributions of the detrital clay-size fraction to the SW Iberian shelf. Mediterranean Outflow Water is characterized by higher temperatures and salinities than other ambient water masses. MOW spreads at water depths between 500 and 1500 m from the Strait of Gibraltar into the eastern North Atlantic and has been a source of salinity for the Atlantic Meridional Overturning Circulation in the North Atlantic. In order to evaluate the hydrographic changes of MOW since the Last Glacial Maximum (LGM) high-resolution Nd and Pb isotope records of past ambient seawater obtained from authigenic ferromanganese oxyhydroxide coatings of bulk marine sediments from three gravity cores in the Gulf of Cadiz (577 m water depth) and along the Portuguese margin (1 745 m and 1 974 m water depth) were produced. The surface and downcore Nd isotope data from all water depths exhibit only a very small variability close to the present day composition of MOW but do not reflect the present day Nd isotopic stratification of the water column as determined from a nearby open ocean hydrographic station ... 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(DE-627)661648451 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 Resolving-System Volltext http://d-nb.info/1012726614/34 Langzeitarchivierung Nationalbibliothek Volltext http://eldiss.uni-kiel.de/macau/receive/dissertation_diss_00006521 Verlag kostenfrei Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_24 ISIL_DE-8 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_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_381 ISIL_DE-Ki130 38.88 Regionale Hydrologie (DE-627)181569914 BO 045F 550 20 01 0084 1256011339 x 14-07-11 21 01 0046 1256022284 z 14-07-11 22 01 0018 1256033995 SUBolrd xu 14-07-11 23 01 0830 1256043168 olr-d x 14-07-11 24 01 0008 1268607932 ka z 13-09-11 30 01 0104 125604928X z 14-07-11 40 01 0007 1256058106 ksn 08-02-12 60 01 0705 1256069256 OLRD z 14-07-11 63 01 3401 1595736034 ORD x 21-01-16 70 01 0089 1256085820 zdo 14-07-11 105 01 0841 1596549149 z 21-01-16 110 01 3110 1256078328 x 14-07-11 132 01 0959 1498064876 OLR-DISS x 12-08-14 151 01 0546 3594150917 OLR-ODISS z 13-02-20 161 01 0960 1597515698 ORD x 28-01-16 293 01 3293 1597973742 ORD xf 28-01-16 370 01 4370 1256080454 x 14-07-11 381 01 4381 1498183921 E-Diss x 13-08-14 20 01 0084 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 21 01 0046 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 22 01 0018 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 23 01 0830 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 24 01 0008 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 30 01 0104 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 60 01 0705 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 LF 70 01 0089 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 105 01 0841 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 110 01 3110 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 132 01 0959 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 161 01 0960 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 293 01 3293 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 370 01 4370 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 381 01 4381 http://eldiss.uni-kiel.de/macau/receive/dissertation_diss_00006521 34 381 00 DE-Ki130 00 Online Publikation / Publication 381 00 DE-Ki130 00 IFM-GEOMAR 2011 381 00 DE-Ki130 00 Open Access 381 00 DE-Ki130 00 Dissertation 381 00 DE-Ki130 00 FB1 / P-OZ 24 01 0008 50 (DE-627)057910383 geo 587.5 Geologie Spanien 24 01 0008 60 (DE-627)058573585 reg 29.7 Spanien 24 01 0008 70 (DE-627)057910367 geo 587 Geologie Iberische Halbinsel 40 00 DE-7 00 (DE-627)613608194 UDE 071 Mittelmeergebiet {Hydrologie} 40 00 DE-7 01 (DE-627)625046501 VAH 000 Verwitterung {Geologie} 40 00 DE-7 02 (DE-627)625047842 VBO 000 Isotopengeologie 40 00 DE-7 03 (DE-627)625050010 VEF 000 Südeuropa und Mittelmeergebiet {Geologie} 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 24 01 0008 ka 24 01 0008 pu 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 381 01 4381 E-Diss 23 01 0830 2011-07-14:13:45:32 40 01 0007 2011-12 9 g
spelling	11,O07 dnb 1012726614 DE-101 urn:nbn:de:gbv:8-diss-65217 urn (DE-627)66422346X (DE-599)DNB1012726614 (OCoLC)838016684 DE-627 ger DE-627 rakwb eng XA-DE 550 OCLC 550 DNB 14 ssgn 38.88 bkl Stumpf, Roland verfasserin (DE-588)1012637484 (DE-627)662254511 (DE-576)34572934X aut Late quaternary variability of hydrography and weathering inputs on the SW Iberian shelf from clay minerals and the radiogenic isotopes of neodymium, strontium and lead vorgelegt von Roland Stumpf 2011 Online-Ressource (122 S., 5,98 MB) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Kiel, Univ., Diss., 2011 The radiogenic isotope systems of neodymium (Nd), strontium (Sr) and lead (Pb) have been used in numerous studies throughout the last decades to investigate water mass circulations of the past and present oceans, and to trace changing contributions of detrital material from different source areas. Clay mineral assemblages and clay mineral ratios from the fine fraction of marine sediments have also been used to characterize endmember sources. This thesis focuses on a reconstruction of the late Quaternary hydrographic variability of the flow path of the Mediterranean Outflow Water (MOW) and the changing weathering contributions of the detrital clay-size fraction to the SW Iberian shelf. Mediterranean Outflow Water is characterized by higher temperatures and salinities than other ambient water masses. MOW spreads at water depths between 500 and 1500 m from the Strait of Gibraltar into the eastern North Atlantic and has been a source of salinity for the Atlantic Meridional Overturning Circulation in the North Atlantic. In order to evaluate the hydrographic changes of MOW since the Last Glacial Maximum (LGM) high-resolution Nd and Pb isotope records of past ambient seawater obtained from authigenic ferromanganese oxyhydroxide coatings of bulk marine sediments from three gravity cores in the Gulf of Cadiz (577 m water depth) and along the Portuguese margin (1 745 m and 1 974 m water depth) were produced. The surface and downcore Nd isotope data from all water depths exhibit only a very small variability close to the present day composition of MOW but do not reflect the present day Nd isotopic stratification of the water column as determined from a nearby open ocean hydrographic station ... Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content g (DE-588)4253070-2 (DE-627)104718013 (DE-576)210528109 Iberische Halbinsel Südwest gnd s (DE-588)4160492-1 (DE-627)104766328 (DE-576)209858184 Holozän gnd s (DE-588)4134766-3 (DE-627)10567009X (DE-576)209655070 Meeressediment gnd s (DE-588)4136262-7 (DE-627)105658820 (DE-576)209667699 Isotopengeochemie gnd (DE-627) Frank, Martin 1966- doktorvater (DE-588)14097444X (DE-627)623219646 (DE-576)321620992 oth Kiel uvp Erscheint auch als Druck-Ausgabe Stumpf, Roland Late Quaternary variability of hydrography and weathering inputs on the SW Iberian shelf from clay minerals and the radiogenic isotopes of neodymium, strontium and lead 2011 106 S. (DE-627)661648451 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 Resolving-System Volltext http://d-nb.info/1012726614/34 Langzeitarchivierung Nationalbibliothek Volltext http://eldiss.uni-kiel.de/macau/receive/dissertation_diss_00006521 Verlag kostenfrei Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_24 ISIL_DE-8 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_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_381 ISIL_DE-Ki130 38.88 Regionale Hydrologie (DE-627)181569914 BO 045F 550 20 01 0084 1256011339 x 14-07-11 21 01 0046 1256022284 z 14-07-11 22 01 0018 1256033995 SUBolrd xu 14-07-11 23 01 0830 1256043168 olr-d x 14-07-11 24 01 0008 1268607932 ka z 13-09-11 30 01 0104 125604928X z 14-07-11 40 01 0007 1256058106 ksn 08-02-12 60 01 0705 1256069256 OLRD z 14-07-11 63 01 3401 1595736034 ORD x 21-01-16 70 01 0089 1256085820 zdo 14-07-11 105 01 0841 1596549149 z 21-01-16 110 01 3110 1256078328 x 14-07-11 132 01 0959 1498064876 OLR-DISS x 12-08-14 151 01 0546 3594150917 OLR-ODISS z 13-02-20 161 01 0960 1597515698 ORD x 28-01-16 293 01 3293 1597973742 ORD xf 28-01-16 370 01 4370 1256080454 x 14-07-11 381 01 4381 1498183921 E-Diss x 13-08-14 20 01 0084 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 21 01 0046 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 22 01 0018 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 23 01 0830 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 24 01 0008 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 30 01 0104 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 60 01 0705 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 LF 70 01 0089 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 105 01 0841 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 110 01 3110 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 132 01 0959 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 161 01 0960 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 293 01 3293 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 370 01 4370 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 381 01 4381 http://eldiss.uni-kiel.de/macau/receive/dissertation_diss_00006521 34 381 00 DE-Ki130 00 Online Publikation / Publication 381 00 DE-Ki130 00 IFM-GEOMAR 2011 381 00 DE-Ki130 00 Open Access 381 00 DE-Ki130 00 Dissertation 381 00 DE-Ki130 00 FB1 / P-OZ 24 01 0008 50 (DE-627)057910383 geo 587.5 Geologie Spanien 24 01 0008 60 (DE-627)058573585 reg 29.7 Spanien 24 01 0008 70 (DE-627)057910367 geo 587 Geologie Iberische Halbinsel 40 00 DE-7 00 (DE-627)613608194 UDE 071 Mittelmeergebiet {Hydrologie} 40 00 DE-7 01 (DE-627)625046501 VAH 000 Verwitterung {Geologie} 40 00 DE-7 02 (DE-627)625047842 VBO 000 Isotopengeologie 40 00 DE-7 03 (DE-627)625050010 VEF 000 Südeuropa und Mittelmeergebiet {Geologie} 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 24 01 0008 ka 24 01 0008 pu 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 381 01 4381 E-Diss 23 01 0830 2011-07-14:13:45:32 40 01 0007 2011-12 9 g
allfields_unstemmed	11,O07 dnb 1012726614 DE-101 urn:nbn:de:gbv:8-diss-65217 urn (DE-627)66422346X (DE-599)DNB1012726614 (OCoLC)838016684 DE-627 ger DE-627 rakwb eng XA-DE 550 OCLC 550 DNB 14 ssgn 38.88 bkl Stumpf, Roland verfasserin (DE-588)1012637484 (DE-627)662254511 (DE-576)34572934X aut Late quaternary variability of hydrography and weathering inputs on the SW Iberian shelf from clay minerals and the radiogenic isotopes of neodymium, strontium and lead vorgelegt von Roland Stumpf 2011 Online-Ressource (122 S., 5,98 MB) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Kiel, Univ., Diss., 2011 The radiogenic isotope systems of neodymium (Nd), strontium (Sr) and lead (Pb) have been used in numerous studies throughout the last decades to investigate water mass circulations of the past and present oceans, and to trace changing contributions of detrital material from different source areas. Clay mineral assemblages and clay mineral ratios from the fine fraction of marine sediments have also been used to characterize endmember sources. This thesis focuses on a reconstruction of the late Quaternary hydrographic variability of the flow path of the Mediterranean Outflow Water (MOW) and the changing weathering contributions of the detrital clay-size fraction to the SW Iberian shelf. Mediterranean Outflow Water is characterized by higher temperatures and salinities than other ambient water masses. MOW spreads at water depths between 500 and 1500 m from the Strait of Gibraltar into the eastern North Atlantic and has been a source of salinity for the Atlantic Meridional Overturning Circulation in the North Atlantic. In order to evaluate the hydrographic changes of MOW since the Last Glacial Maximum (LGM) high-resolution Nd and Pb isotope records of past ambient seawater obtained from authigenic ferromanganese oxyhydroxide coatings of bulk marine sediments from three gravity cores in the Gulf of Cadiz (577 m water depth) and along the Portuguese margin (1 745 m and 1 974 m water depth) were produced. The surface and downcore Nd isotope data from all water depths exhibit only a very small variability close to the present day composition of MOW but do not reflect the present day Nd isotopic stratification of the water column as determined from a nearby open ocean hydrographic station ... Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content g (DE-588)4253070-2 (DE-627)104718013 (DE-576)210528109 Iberische Halbinsel Südwest gnd s (DE-588)4160492-1 (DE-627)104766328 (DE-576)209858184 Holozän gnd s (DE-588)4134766-3 (DE-627)10567009X (DE-576)209655070 Meeressediment gnd s (DE-588)4136262-7 (DE-627)105658820 (DE-576)209667699 Isotopengeochemie gnd (DE-627) Frank, Martin 1966- doktorvater (DE-588)14097444X (DE-627)623219646 (DE-576)321620992 oth Kiel uvp Erscheint auch als Druck-Ausgabe Stumpf, Roland Late Quaternary variability of hydrography and weathering inputs on the SW Iberian shelf from clay minerals and the radiogenic isotopes of neodymium, strontium and lead 2011 106 S. (DE-627)661648451 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 Resolving-System Volltext http://d-nb.info/1012726614/34 Langzeitarchivierung Nationalbibliothek Volltext http://eldiss.uni-kiel.de/macau/receive/dissertation_diss_00006521 Verlag kostenfrei Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_24 ISIL_DE-8 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_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_381 ISIL_DE-Ki130 38.88 Regionale Hydrologie (DE-627)181569914 BO 045F 550 20 01 0084 1256011339 x 14-07-11 21 01 0046 1256022284 z 14-07-11 22 01 0018 1256033995 SUBolrd xu 14-07-11 23 01 0830 1256043168 olr-d x 14-07-11 24 01 0008 1268607932 ka z 13-09-11 30 01 0104 125604928X z 14-07-11 40 01 0007 1256058106 ksn 08-02-12 60 01 0705 1256069256 OLRD z 14-07-11 63 01 3401 1595736034 ORD x 21-01-16 70 01 0089 1256085820 zdo 14-07-11 105 01 0841 1596549149 z 21-01-16 110 01 3110 1256078328 x 14-07-11 132 01 0959 1498064876 OLR-DISS x 12-08-14 151 01 0546 3594150917 OLR-ODISS z 13-02-20 161 01 0960 1597515698 ORD x 28-01-16 293 01 3293 1597973742 ORD xf 28-01-16 370 01 4370 1256080454 x 14-07-11 381 01 4381 1498183921 E-Diss x 13-08-14 20 01 0084 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 21 01 0046 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 22 01 0018 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 23 01 0830 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 24 01 0008 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 30 01 0104 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 60 01 0705 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 LF 70 01 0089 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 105 01 0841 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 110 01 3110 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 132 01 0959 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 161 01 0960 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 293 01 3293 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 370 01 4370 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 381 01 4381 http://eldiss.uni-kiel.de/macau/receive/dissertation_diss_00006521 34 381 00 DE-Ki130 00 Online Publikation / Publication 381 00 DE-Ki130 00 IFM-GEOMAR 2011 381 00 DE-Ki130 00 Open Access 381 00 DE-Ki130 00 Dissertation 381 00 DE-Ki130 00 FB1 / P-OZ 24 01 0008 50 (DE-627)057910383 geo 587.5 Geologie Spanien 24 01 0008 60 (DE-627)058573585 reg 29.7 Spanien 24 01 0008 70 (DE-627)057910367 geo 587 Geologie Iberische Halbinsel 40 00 DE-7 00 (DE-627)613608194 UDE 071 Mittelmeergebiet {Hydrologie} 40 00 DE-7 01 (DE-627)625046501 VAH 000 Verwitterung {Geologie} 40 00 DE-7 02 (DE-627)625047842 VBO 000 Isotopengeologie 40 00 DE-7 03 (DE-627)625050010 VEF 000 Südeuropa und Mittelmeergebiet {Geologie} 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 24 01 0008 ka 24 01 0008 pu 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 381 01 4381 E-Diss 23 01 0830 2011-07-14:13:45:32 40 01 0007 2011-12 9 g
allfieldsGer	11,O07 dnb 1012726614 DE-101 urn:nbn:de:gbv:8-diss-65217 urn (DE-627)66422346X (DE-599)DNB1012726614 (OCoLC)838016684 DE-627 ger DE-627 rakwb eng XA-DE 550 OCLC 550 DNB 14 ssgn 38.88 bkl Stumpf, Roland verfasserin (DE-588)1012637484 (DE-627)662254511 (DE-576)34572934X aut Late quaternary variability of hydrography and weathering inputs on the SW Iberian shelf from clay minerals and the radiogenic isotopes of neodymium, strontium and lead vorgelegt von Roland Stumpf 2011 Online-Ressource (122 S., 5,98 MB) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Kiel, Univ., Diss., 2011 The radiogenic isotope systems of neodymium (Nd), strontium (Sr) and lead (Pb) have been used in numerous studies throughout the last decades to investigate water mass circulations of the past and present oceans, and to trace changing contributions of detrital material from different source areas. Clay mineral assemblages and clay mineral ratios from the fine fraction of marine sediments have also been used to characterize endmember sources. This thesis focuses on a reconstruction of the late Quaternary hydrographic variability of the flow path of the Mediterranean Outflow Water (MOW) and the changing weathering contributions of the detrital clay-size fraction to the SW Iberian shelf. Mediterranean Outflow Water is characterized by higher temperatures and salinities than other ambient water masses. MOW spreads at water depths between 500 and 1500 m from the Strait of Gibraltar into the eastern North Atlantic and has been a source of salinity for the Atlantic Meridional Overturning Circulation in the North Atlantic. In order to evaluate the hydrographic changes of MOW since the Last Glacial Maximum (LGM) high-resolution Nd and Pb isotope records of past ambient seawater obtained from authigenic ferromanganese oxyhydroxide coatings of bulk marine sediments from three gravity cores in the Gulf of Cadiz (577 m water depth) and along the Portuguese margin (1 745 m and 1 974 m water depth) were produced. The surface and downcore Nd isotope data from all water depths exhibit only a very small variability close to the present day composition of MOW but do not reflect the present day Nd isotopic stratification of the water column as determined from a nearby open ocean hydrographic station ... Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content g (DE-588)4253070-2 (DE-627)104718013 (DE-576)210528109 Iberische Halbinsel Südwest gnd s (DE-588)4160492-1 (DE-627)104766328 (DE-576)209858184 Holozän gnd s (DE-588)4134766-3 (DE-627)10567009X (DE-576)209655070 Meeressediment gnd s (DE-588)4136262-7 (DE-627)105658820 (DE-576)209667699 Isotopengeochemie gnd (DE-627) Frank, Martin 1966- doktorvater (DE-588)14097444X (DE-627)623219646 (DE-576)321620992 oth Kiel uvp Erscheint auch als Druck-Ausgabe Stumpf, Roland Late Quaternary variability of hydrography and weathering inputs on the SW Iberian shelf from clay minerals and the radiogenic isotopes of neodymium, strontium and lead 2011 106 S. (DE-627)661648451 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 Resolving-System Volltext http://d-nb.info/1012726614/34 Langzeitarchivierung Nationalbibliothek Volltext http://eldiss.uni-kiel.de/macau/receive/dissertation_diss_00006521 Verlag kostenfrei Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_24 ISIL_DE-8 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_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_381 ISIL_DE-Ki130 38.88 Regionale Hydrologie (DE-627)181569914 BO 045F 550 20 01 0084 1256011339 x 14-07-11 21 01 0046 1256022284 z 14-07-11 22 01 0018 1256033995 SUBolrd xu 14-07-11 23 01 0830 1256043168 olr-d x 14-07-11 24 01 0008 1268607932 ka z 13-09-11 30 01 0104 125604928X z 14-07-11 40 01 0007 1256058106 ksn 08-02-12 60 01 0705 1256069256 OLRD z 14-07-11 63 01 3401 1595736034 ORD x 21-01-16 70 01 0089 1256085820 zdo 14-07-11 105 01 0841 1596549149 z 21-01-16 110 01 3110 1256078328 x 14-07-11 132 01 0959 1498064876 OLR-DISS x 12-08-14 151 01 0546 3594150917 OLR-ODISS z 13-02-20 161 01 0960 1597515698 ORD x 28-01-16 293 01 3293 1597973742 ORD xf 28-01-16 370 01 4370 1256080454 x 14-07-11 381 01 4381 1498183921 E-Diss x 13-08-14 20 01 0084 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 21 01 0046 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 22 01 0018 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 23 01 0830 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 24 01 0008 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 30 01 0104 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 60 01 0705 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 LF 70 01 0089 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 105 01 0841 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 110 01 3110 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 132 01 0959 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 161 01 0960 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 293 01 3293 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 370 01 4370 http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 381 01 4381 http://eldiss.uni-kiel.de/macau/receive/dissertation_diss_00006521 34 381 00 DE-Ki130 00 Online Publikation / Publication 381 00 DE-Ki130 00 IFM-GEOMAR 2011 381 00 DE-Ki130 00 Open Access 381 00 DE-Ki130 00 Dissertation 381 00 DE-Ki130 00 FB1 / P-OZ 24 01 0008 50 (DE-627)057910383 geo 587.5 Geologie Spanien 24 01 0008 60 (DE-627)058573585 reg 29.7 Spanien 24 01 0008 70 (DE-627)057910367 geo 587 Geologie Iberische Halbinsel 40 00 DE-7 00 (DE-627)613608194 UDE 071 Mittelmeergebiet {Hydrologie} 40 00 DE-7 01 (DE-627)625046501 VAH 000 Verwitterung {Geologie} 40 00 DE-7 02 (DE-627)625047842 VBO 000 Isotopengeologie 40 00 DE-7 03 (DE-627)625050010 VEF 000 Südeuropa und Mittelmeergebiet {Geologie} 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 22 01 0018 SUBolrd 23 01 0830 olr-d 24 01 0008 ka 24 01 0008 pu 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 381 01 4381 E-Diss 23 01 0830 2011-07-14:13:45:32 40 01 0007 2011-12 9 g
allfieldsSound	11,O07 dnb 1012726614 DE-101 urn:nbn:de:gbv:8-diss-65217 urn (DE-627)66422346X (DE-599)DNB1012726614 (OCoLC)838016684 DE-627 ger DE-627 rakwb eng XA-DE 550 OCLC 550 DNB 14 ssgn 38.88 bkl Stumpf, Roland verfasserin (DE-588)1012637484 (DE-627)662254511 (DE-576)34572934X aut Late quaternary variability of hydrography and weathering inputs on the SW Iberian shelf from clay minerals and the radiogenic isotopes of neodymium, strontium and lead vorgelegt von Roland Stumpf 2011 Online-Ressource (122 S., 5,98 MB) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Kiel, Univ., Diss., 2011 The radiogenic isotope systems of neodymium (Nd), strontium (Sr) and lead (Pb) have been used in numerous studies throughout the last decades to investigate water mass circulations of the past and present oceans, and to trace changing contributions of detrital material from different source areas. Clay mineral assemblages and clay mineral ratios from the fine fraction of marine sediments have also been used to characterize endmember sources. This thesis focuses on a reconstruction of the late Quaternary hydrographic variability of the flow path of the Mediterranean Outflow Water (MOW) and the changing weathering contributions of the detrital clay-size fraction to the SW Iberian shelf. Mediterranean Outflow Water is characterized by higher temperatures and salinities than other ambient water masses. MOW spreads at water depths between 500 and 1500 m from the Strait of Gibraltar into the eastern North Atlantic and has been a source of salinity for the Atlantic Meridional Overturning Circulation in the North Atlantic. In order to evaluate the hydrographic changes of MOW since the Last Glacial Maximum (LGM) high-resolution Nd and Pb isotope records of past ambient seawater obtained from authigenic ferromanganese oxyhydroxide coatings of bulk marine sediments from three gravity cores in the Gulf of Cadiz (577 m water depth) and along the Portuguese margin (1 745 m and 1 974 m water depth) were produced. The surface and downcore Nd isotope data from all water depths exhibit only a very small variability close to the present day composition of MOW but do not reflect the present day Nd isotopic stratification of the water column as determined from a nearby open ocean hydrographic station ... Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content g (DE-588)4253070-2 (DE-627)104718013 (DE-576)210528109 Iberische Halbinsel Südwest gnd s (DE-588)4160492-1 (DE-627)104766328 (DE-576)209858184 Holozän gnd s (DE-588)4134766-3 (DE-627)10567009X (DE-576)209655070 Meeressediment gnd s (DE-588)4136262-7 (DE-627)105658820 (DE-576)209667699 Isotopengeochemie gnd (DE-627) Frank, Martin 1966- doktorvater (DE-588)14097444X (DE-627)623219646 (DE-576)321620992 oth Kiel uvp Erscheint auch als Druck-Ausgabe Stumpf, Roland Late Quaternary variability of hydrography and weathering inputs on the SW Iberian shelf from clay minerals and the radiogenic isotopes of neodymium, strontium and lead 2011 106 S. 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language	English
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topic_facet	Iberische Halbinsel Holozän Meeressediment Isotopengeochemie
hochschulschrift_txt_mv	Kiel, Univ., Diss., 2011
sw_local_iln_str_mv	381:Online Publikation / Publication DE-Ki130:Online Publikation / Publication 381:IFM-GEOMAR 2011 DE-Ki130:IFM-GEOMAR 2011 381:Open Access DE-Ki130:Open Access 381:Dissertation DE-Ki130:Dissertation 381:FB1 / P-OZ DE-Ki130:FB1 / P-OZ
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authorswithroles_txt_mv	Stumpf, Roland @@aut@@ Frank, Martin @@oth@@
publishDateDaySort_date	2011-01-01T00:00:00Z
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Clay mineral assemblages and clay mineral ratios from the fine fraction of marine sediments have also been used to characterize endmember sources. This thesis focuses on a reconstruction of the late Quaternary hydrographic variability of the flow path of the Mediterranean Outflow Water (MOW) and the changing weathering contributions of the detrital clay-size fraction to the SW Iberian shelf. Mediterranean Outflow Water is characterized by higher temperatures and salinities than other ambient water masses. MOW spreads at water depths between 500 and 1500 m from the Strait of Gibraltar into the eastern North Atlantic and has been a source of salinity for the Atlantic Meridional Overturning Circulation in the North Atlantic. In order to evaluate the hydrographic changes of MOW since the Last Glacial Maximum (LGM) high-resolution Nd and Pb isotope records of past ambient seawater obtained from authigenic ferromanganese oxyhydroxide coatings of bulk marine sediments from three gravity cores in the Gulf of Cadiz (577 m water depth) and along the Portuguese margin (1 745 m and 1 974 m water depth) were produced. 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title	Late quaternary variability of hydrography and weathering inputs on the SW Iberian shelf from clay minerals and the radiogenic isotopes of neodymium, strontium and lead
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title_full	Late quaternary variability of hydrography and weathering inputs on the SW Iberian shelf from clay minerals and the radiogenic isotopes of neodymium, strontium and lead vorgelegt von Roland Stumpf
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title_sort	late quaternary variability of hydrography and weathering inputs on the sw iberian shelf from clay minerals and the radiogenic isotopes of neodymium, strontium and lead
title_auth	Late quaternary variability of hydrography and weathering inputs on the SW Iberian shelf from clay minerals and the radiogenic isotopes of neodymium, strontium and lead
abstract	The radiogenic isotope systems of neodymium (Nd), strontium (Sr) and lead (Pb) have been used in numerous studies throughout the last decades to investigate water mass circulations of the past and present oceans, and to trace changing contributions of detrital material from different source areas. Clay mineral assemblages and clay mineral ratios from the fine fraction of marine sediments have also been used to characterize endmember sources. This thesis focuses on a reconstruction of the late Quaternary hydrographic variability of the flow path of the Mediterranean Outflow Water (MOW) and the changing weathering contributions of the detrital clay-size fraction to the SW Iberian shelf. Mediterranean Outflow Water is characterized by higher temperatures and salinities than other ambient water masses. MOW spreads at water depths between 500 and 1500 m from the Strait of Gibraltar into the eastern North Atlantic and has been a source of salinity for the Atlantic Meridional Overturning Circulation in the North Atlantic. In order to evaluate the hydrographic changes of MOW since the Last Glacial Maximum (LGM) high-resolution Nd and Pb isotope records of past ambient seawater obtained from authigenic ferromanganese oxyhydroxide coatings of bulk marine sediments from three gravity cores in the Gulf of Cadiz (577 m water depth) and along the Portuguese margin (1 745 m and 1 974 m water depth) were produced. The surface and downcore Nd isotope data from all water depths exhibit only a very small variability close to the present day composition of MOW but do not reflect the present day Nd isotopic stratification of the water column as determined from a nearby open ocean hydrographic station ...
abstractGer	The radiogenic isotope systems of neodymium (Nd), strontium (Sr) and lead (Pb) have been used in numerous studies throughout the last decades to investigate water mass circulations of the past and present oceans, and to trace changing contributions of detrital material from different source areas. Clay mineral assemblages and clay mineral ratios from the fine fraction of marine sediments have also been used to characterize endmember sources. This thesis focuses on a reconstruction of the late Quaternary hydrographic variability of the flow path of the Mediterranean Outflow Water (MOW) and the changing weathering contributions of the detrital clay-size fraction to the SW Iberian shelf. Mediterranean Outflow Water is characterized by higher temperatures and salinities than other ambient water masses. MOW spreads at water depths between 500 and 1500 m from the Strait of Gibraltar into the eastern North Atlantic and has been a source of salinity for the Atlantic Meridional Overturning Circulation in the North Atlantic. In order to evaluate the hydrographic changes of MOW since the Last Glacial Maximum (LGM) high-resolution Nd and Pb isotope records of past ambient seawater obtained from authigenic ferromanganese oxyhydroxide coatings of bulk marine sediments from three gravity cores in the Gulf of Cadiz (577 m water depth) and along the Portuguese margin (1 745 m and 1 974 m water depth) were produced. The surface and downcore Nd isotope data from all water depths exhibit only a very small variability close to the present day composition of MOW but do not reflect the present day Nd isotopic stratification of the water column as determined from a nearby open ocean hydrographic station ...
abstract_unstemmed	The radiogenic isotope systems of neodymium (Nd), strontium (Sr) and lead (Pb) have been used in numerous studies throughout the last decades to investigate water mass circulations of the past and present oceans, and to trace changing contributions of detrital material from different source areas. Clay mineral assemblages and clay mineral ratios from the fine fraction of marine sediments have also been used to characterize endmember sources. This thesis focuses on a reconstruction of the late Quaternary hydrographic variability of the flow path of the Mediterranean Outflow Water (MOW) and the changing weathering contributions of the detrital clay-size fraction to the SW Iberian shelf. Mediterranean Outflow Water is characterized by higher temperatures and salinities than other ambient water masses. MOW spreads at water depths between 500 and 1500 m from the Strait of Gibraltar into the eastern North Atlantic and has been a source of salinity for the Atlantic Meridional Overturning Circulation in the North Atlantic. In order to evaluate the hydrographic changes of MOW since the Last Glacial Maximum (LGM) high-resolution Nd and Pb isotope records of past ambient seawater obtained from authigenic ferromanganese oxyhydroxide coatings of bulk marine sediments from three gravity cores in the Gulf of Cadiz (577 m water depth) and along the Portuguese margin (1 745 m and 1 974 m water depth) were produced. The surface and downcore Nd isotope data from all water depths exhibit only a very small variability close to the present day composition of MOW but do not reflect the present day Nd isotopic stratification of the water column as determined from a nearby open ocean hydrographic station ...
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title_short	Late quaternary variability of hydrography and weathering inputs on the SW Iberian shelf from clay minerals and the radiogenic isotopes of neodymium, strontium and lead
url	http://nbn-resolving.de/urn:nbn:de:gbv:8-diss-65217 http://d-nb.info/1012726614/34 http://eldiss.uni-kiel.de/macau/receive/dissertation_diss_00006521
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GND_txtF_mv	Stumpf, Roland Hochschulschrift Iberische Halbinsel (Südwest) Spätquartär Alluvium Nacheiszeit Postglazial Holozän Meeressedimente Marines Sediment Meeresablagerung Meer / Sediment Marine Sedimente Meer / Aquatisches Sediment Meeressediment Isotopengeochemie Frank, M. Frank, Martin
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up_date	2024-07-13T18:04:51.851Z
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Late quaternary variability of hydrography and weathering inputs on the SW Iberian shelf from clay minerals and the radiogenic isotopes of neodymium, strontium and lead

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