Radioisotopic age constraints for Glacial Terminations IX and VII from aggradational sections of the Tiber River delta in Rome, Italy
Radioisotopic age constraints for Glacial Terminations IX and VII from aggradational sections of the Tiber River delta in Rome, Italy
Buried sedimentary aggradational sections deposited between 800 ka and 600 ka in the Tiber River coastal alluvial plain have been studied using borecores from around Rome. 40Ar/39Ar ages on sanidine and/or leucite from intercalated tephra layers and paleomagnetic investigation of clay sections provide geochronologic constraints on the timing of aggradation of two alluvial sections, demonstrating that they were deposited in response to glacio–eustatic sea level rise caused by Glacial Terminations IX and VII. 40Ar/39Ar age data indicate ages of 802 ± 8 ka (1? full errors) and 649 ± 3 ka (1? full errors) for Glacial Terminations IX and VII, respectively, providing a rare test, beyond the range of U-series dating for corals and speleothems ( 500 ka), of the astronomically calibrated timescale developed for oxygen isotope records from deep sea cores.
glacial termination, sea level, 40Ar/39Ar, paleomagnetism, Tiber River delta
61-80
Florindo, F.
8782f358-6dd8-4531-aaf1-4e1e859d52db
Karner, D.B.
ceda97de-f766-4a1a-9d67-0d37e3e92cd3
Marra, F.
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Renne, P.R.
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Roberts, A.P.
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Weaver, R.
f4c9143b-6c82-4683-960b-a9614edd5244
2007
Florindo, F.
8782f358-6dd8-4531-aaf1-4e1e859d52db
Karner, D.B.
ceda97de-f766-4a1a-9d67-0d37e3e92cd3
Marra, F.
0e85c5ec-4692-41af-92fb-13975cafd1d1
Renne, P.R.
ecc965d9-11a9-4150-9148-d3ef0c52b671
Roberts, A.P.
4497b436-ef02-428d-a46e-65a22094ba52
Weaver, R.
f4c9143b-6c82-4683-960b-a9614edd5244
Florindo, F., Karner, D.B., Marra, F., Renne, P.R., Roberts, A.P. and Weaver, R.
(2007)
Radioisotopic age constraints for Glacial Terminations IX and VII from aggradational sections of the Tiber River delta in Rome, Italy.
Earth and Planetary Science Letters, 256 (1-2), .
(doi:10.1016/j.epsl.2007.01.014).
Abstract
Buried sedimentary aggradational sections deposited between 800 ka and 600 ka in the Tiber River coastal alluvial plain have been studied using borecores from around Rome. 40Ar/39Ar ages on sanidine and/or leucite from intercalated tephra layers and paleomagnetic investigation of clay sections provide geochronologic constraints on the timing of aggradation of two alluvial sections, demonstrating that they were deposited in response to glacio–eustatic sea level rise caused by Glacial Terminations IX and VII. 40Ar/39Ar age data indicate ages of 802 ± 8 ka (1? full errors) and 649 ± 3 ka (1? full errors) for Glacial Terminations IX and VII, respectively, providing a rare test, beyond the range of U-series dating for corals and speleothems ( 500 ka), of the astronomically calibrated timescale developed for oxygen isotope records from deep sea cores.
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Published date: 2007
Keywords:
glacial termination, sea level, 40Ar/39Ar, paleomagnetism, Tiber River delta
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Local EPrints ID: 45394
URI: http://eprints.soton.ac.uk/id/eprint/45394
ISSN: 0012-821X
PURE UUID: 754e64d2-1b72-4fb9-a24b-b56cba4a6cb1
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Date deposited: 27 Mar 2007
Last modified: 15 Mar 2024 09:10
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Contributors
Author:
F. Florindo
Author:
D.B. Karner
Author:
F. Marra
Author:
P.R. Renne
Author:
A.P. Roberts
Author:
R. Weaver
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