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A revised and improved age model for the middle Miocene part of IODP Site U1318 (Porcupine Basin, offshore southwestern Ireland)

(2018) GEOLOGICAL MAGAZINE. 155. p.1105-1116
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Abstract
Integrated Ocean Drilling Program Leg 307 Site U1318 is one of the few relatively complete middle Miocene drillcores from the North Atlantic (Porcupine Basin, offshore southwestern Ireland). Using benthic foraminiferal stable carbon and oxygen isotopes, the existing age model for Site U1318 was improved. The stable isotope record displays globally recognized isotope events, used to revise the existing magnetostratigraphy-based age model. Two intervals contained misidentified magnetochrons which were corrected. The sampled interval now has a refined age of 12.75-16.60 Ma with a temporal resolution of c. 29 ka.
Keywords
North Atlantic, isotope stratigraphy, magnetostratigraphy, dinoflagellate cysts, Neogene, GLOBAL SEA-LEVEL, ISOTOPE STRATIGRAPHY, DINOFLAGELLATE CYST, OCEAN CIRCULATION, CARBON ISOTOPES, OXYGEN, SEQUENCES, HISTORY, RECORDS, EVENTS

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Citation

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Chicago
Quaijtaal, Willemijn, Steven Tesseur, Timme H Donders, Philippe Claeys, and Stephen Louwye. 2018. “A Revised and Improved Age Model for the Middle Miocene Part of IODP Site U1318 (Porcupine Basin, Offshore Southwestern Ireland).” Geological Magazine 155: 1105–1116.
APA
Quaijtaal, W., Tesseur, S., Donders, T. H., Claeys, P., & Louwye, S. (2018). A revised and improved age model for the middle Miocene part of IODP Site U1318 (Porcupine Basin, offshore southwestern Ireland). GEOLOGICAL MAGAZINE, 155, 1105–1116.
Vancouver
1.
Quaijtaal W, Tesseur S, Donders TH, Claeys P, Louwye S. A revised and improved age model for the middle Miocene part of IODP Site U1318 (Porcupine Basin, offshore southwestern Ireland). GEOLOGICAL MAGAZINE. 2018;155:1105–16.
MLA
Quaijtaal, Willemijn, Steven Tesseur, Timme H Donders, et al. “A Revised and Improved Age Model for the Middle Miocene Part of IODP Site U1318 (Porcupine Basin, Offshore Southwestern Ireland).” GEOLOGICAL MAGAZINE 155 (2018): 1105–1116. Print.
@article{8507028,
  abstract     = {Integrated Ocean Drilling Program Leg 307 Site U1318 is one of the few relatively complete middle Miocene drillcores from the North Atlantic (Porcupine Basin, offshore southwestern Ireland). Using benthic foraminiferal stable carbon and oxygen isotopes, the existing age model for Site U1318 was improved. The stable isotope record displays globally recognized isotope events, used to revise the existing magnetostratigraphy-based age model. Two intervals contained misidentified magnetochrons which were corrected. The sampled interval now has a refined age of 12.75-16.60 Ma with a temporal resolution of c. 29 ka.},
  author       = {Quaijtaal, Willemijn and Tesseur, Steven and Donders, Timme H and Claeys, Philippe and Louwye, Stephen},
  issn         = {0016-7568},
  journal      = {GEOLOGICAL MAGAZINE},
  language     = {eng},
  pages        = {1105--1116},
  title        = {A revised and improved age model for the middle Miocene part of IODP Site U1318 (Porcupine Basin, offshore southwestern Ireland)},
  url          = {http://dx.doi.org/10.1017/s0016756816001278},
  volume       = {155},
  year         = {2018},
}

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