Canterbury Basin sea level: global and local controls on continental margin stratigraphy

Craig S. Fulthorpe, Koichi Hoyanagi, Martin P. Crundwell, Jaume Dinarès-Turell, Xuan Ding, Simon C. George, Daniel A. Hepp, John Jaeger, Shungo Kawagata, David B. Kemp, Young-Gyun Kim, Michelle A. Kominz, Peter Blum, Helen Lever, Julius Sebastian Lipp, Kathleen M. Marsaglia, Cecilia M. McHugh, Naomi Murakoshi, Ohi Takeshi, Laura Pea & 13 others Mathieu Richaud, Suto Itsuki, Susumu Tanabe, Gilles Guèrin, Kirsteen J. Tinto, Goichiro Uramoto, Toshihiro Yoshimura, Angela L. Slagle, Stacie A. Blair, Gregory H. Browne, Robert M. Carter, Maria-Cristina Ciobanu, George E. Claypool

Research output: Book/ReportBookResearch

Abstract

Integrated Ocean Drilling Program (IODP) Expedition 317 was devoted to understanding the relative importance of global sea level (eustasy) versus local tectonic and sedimentary processes in controlling continental margin sedimentary cycles. The expedition recovered sediments from the Eocene to recent period, with a particular focus on the sequence stratigraphy of the late Miocene to recent, when global sea level change was dominated by glacioeustasy. Drilling in the Canterbury Basin, on the eastern margin of the South Island of New Zealand, takes advantage of high rates of Neogene sediment supply, which preserves a high-frequency (0.1–0.5 m.y.) record of depositional cyclicity. The Canterbury Basin provides an opportunity to study the complex interactions between processes responsible for the preserved stratigraphic record of sequences because of the proximity of an uplifting mountain chain, the Southern Alps, and strong ocean currents. Currents have locally built large, elongate sediment drifts within the prograding Neogene section. Expedition 317 did not drill into one of these elongate drifts, but currents are inferred to have strongly influenced deposition across the basin, including in locations lacking prominent mounded drifts. Upper Miocene to recent sedimentary sequences were cored in a transect of three sites on the continental shelf (landward to basinward, Sites U1353, U1354, and U1351) and one on the continental slope (Site U1352). The transect provides a stratigraphic record of depositional cycles across the shallow-water environment most directly affected by relative sea level change. Lithologic boundaries, provisionally correlative with seismic sequence boundaries, have been identified in cores from each site and provide insights into the origins of seismically resolvable sequences. This record will be used to estimate the timing and amplitude of global sea level change and to document the sedimentary processes that operate during sequence formation. Sites U1353 and U1354 provide significant, double-cored, high-recovery sections through the Holocene and late Quaternary for high-resolution study of recent glacial cycles in a continental shelf setting. Continental slope Site U1352 represents a complete section from modern slope terrigenous sediment to hard Eocene limestone, with all the associated lithologic, biostratigraphic, physical, geochemical, and microbiological transitions. The site also provides a record of ocean circulation and fronts during the last ~35 m.y. The early Oligocene (~30 Ma) Marshall Paraconformity was the deepest drilling target of Expedition 317 and is hypothesized to represent intensified current erosion or nondeposition associated with the initiation of thermohaline circulation following the separation of Australian and Antarctica. Expedition 317 set a number of scientific ocean drilling records: (1) deepest hole drilled in a single expedition and second deepest hole in the history of scientific ocean drilling (Hole U1352C, 1927 m); (2) deepest hole and second deepest hole drilled by the R/V JOIDES Resolution on a continental shelf (Hole U1351B, 1030 m; Hole U1353B, 614 m); (3) shallowest water depth for a site drilled by the JOIDES Resolution for scientific purposes (Site U1353, 84.7 m water depth); and (4) deepest sample taken by scientific ocean drilling for microbiological studies (1925 m, Site U1352). Expedition 317 supplements previous drilling of sedimentary sequences for sequence stratigraphic and sea level objectives, particularly drilling on the New Jersey margin (Ocean Drilling Program [ODP] Legs 150, 150X, 174A, and 174AX and IODP Expedition 313) and in the Bahamas (ODP Leg 166), but includes an expanded Pliocene section. Completion of at least one transect across a geographically and tectonically distinct siliciclastic margin was the necessary next step in deciphering continental margin stratigraphy. Expedition 317 also complements ODP Leg 181, which focused on drift development in more distal parts of the Eastern New Zealand Oceanic Sedimentary System (ENZOSS).
LanguageEnglish
PublisherIntegrated Ocean Drilling Program Management International
Number of pages133
DOIs
Publication statusPublished - 2010

Fingerprint

continental margin
Ocean Drilling Program
stratigraphy
drilling
sea level
basin
sea level change
continental shelf
transect
geological record
sedimentary sequence
continental slope
sediment
Neogene
water depth
Eocene
ocean
shallow water
glacioeustacy
Miocene

Bibliographical note

Version archived for private and non-commercial use with the permission of the author/s and according to publisher conditions. For further rights please contact the publisher.

Keywords

  • Paleoceanography
  • sea-level
  • continental margin
  • Canterbury Basin

Cite this

Fulthorpe, C. S., Hoyanagi, K., Crundwell, M. P., Dinarès-Turell, J., Ding, X., George, S. C., ... Claypool, G. E. (2010). Canterbury Basin sea level: global and local controls on continental margin stratigraphy. Integrated Ocean Drilling Program Management International. https://doi.org/10.2204/iodp.pr.317.2010
Fulthorpe, Craig S. ; Hoyanagi, Koichi ; Crundwell, Martin P. ; Dinarès-Turell, Jaume ; Ding, Xuan ; George, Simon C. ; Hepp, Daniel A. ; Jaeger, John ; Kawagata, Shungo ; Kemp, David B. ; Kim, Young-Gyun ; Kominz, Michelle A. ; Blum, Peter ; Lever, Helen ; Lipp, Julius Sebastian ; Marsaglia, Kathleen M. ; McHugh, Cecilia M. ; Murakoshi, Naomi ; Takeshi, Ohi ; Pea, Laura ; Richaud, Mathieu ; Itsuki, Suto ; Tanabe, Susumu ; Guèrin, Gilles ; Tinto, Kirsteen J. ; Uramoto, Goichiro ; Yoshimura, Toshihiro ; Slagle, Angela L. ; Blair, Stacie A. ; Browne, Gregory H. ; Carter, Robert M. ; Ciobanu, Maria-Cristina ; Claypool, George E. / Canterbury Basin sea level : global and local controls on continental margin stratigraphy. Integrated Ocean Drilling Program Management International, 2010. 133 p.
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Fulthorpe, CS, Hoyanagi, K, Crundwell, MP, Dinarès-Turell, J, Ding, X, George, SC, Hepp, DA, Jaeger, J, Kawagata, S, Kemp, DB, Kim, Y-G, Kominz, MA, Blum, P, Lever, H, Lipp, JS, Marsaglia, KM, McHugh, CM, Murakoshi, N, Takeshi, O, Pea, L, Richaud, M, Itsuki, S, Tanabe, S, Guèrin, G, Tinto, KJ, Uramoto, G, Yoshimura, T, Slagle, AL, Blair, SA, Browne, GH, Carter, RM, Ciobanu, M-C & Claypool, GE 2010, Canterbury Basin sea level: global and local controls on continental margin stratigraphy. Integrated Ocean Drilling Program Management International. https://doi.org/10.2204/iodp.pr.317.2010

Canterbury Basin sea level : global and local controls on continental margin stratigraphy. / Fulthorpe, Craig S.; Hoyanagi, Koichi; Crundwell, Martin P.; Dinarès-Turell, Jaume; Ding, Xuan; George, Simon C.; Hepp, Daniel A.; Jaeger, John; Kawagata, Shungo; Kemp, David B.; Kim, Young-Gyun; Kominz, Michelle A.; Blum, Peter; Lever, Helen; Lipp, Julius Sebastian; Marsaglia, Kathleen M.; McHugh, Cecilia M.; Murakoshi, Naomi; Takeshi, Ohi; Pea, Laura; Richaud, Mathieu; Itsuki, Suto; Tanabe, Susumu; Guèrin, Gilles; Tinto, Kirsteen J.; Uramoto, Goichiro; Yoshimura, Toshihiro; Slagle, Angela L.; Blair, Stacie A.; Browne, Gregory H.; Carter, Robert M.; Ciobanu, Maria-Cristina; Claypool, George E.

Integrated Ocean Drilling Program Management International, 2010. 133 p.

Research output: Book/ReportBookResearch

TY - BOOK

T1 - Canterbury Basin sea level

T2 - global and local controls on continental margin stratigraphy

AU - Fulthorpe, Craig S.

AU - Hoyanagi, Koichi

AU - Crundwell, Martin P.

AU - Dinarès-Turell, Jaume

AU - Ding, Xuan

AU - George, Simon C.

AU - Hepp, Daniel A.

AU - Jaeger, John

AU - Kawagata, Shungo

AU - Kemp, David B.

AU - Kim, Young-Gyun

AU - Kominz, Michelle A.

AU - Blum, Peter

AU - Lever, Helen

AU - Lipp, Julius Sebastian

AU - Marsaglia, Kathleen M.

AU - McHugh, Cecilia M.

AU - Murakoshi, Naomi

AU - Takeshi, Ohi

AU - Pea, Laura

AU - Richaud, Mathieu

AU - Itsuki, Suto

AU - Tanabe, Susumu

AU - Guèrin, Gilles

AU - Tinto, Kirsteen J.

AU - Uramoto, Goichiro

AU - Yoshimura, Toshihiro

AU - Slagle, Angela L.

AU - Blair, Stacie A.

AU - Browne, Gregory H.

AU - Carter, Robert M.

AU - Ciobanu, Maria-Cristina

AU - Claypool, George E.

N1 - Version archived for private and non-commercial use with the permission of the author/s and according to publisher conditions. For further rights please contact the publisher.

PY - 2010

Y1 - 2010

N2 - Integrated Ocean Drilling Program (IODP) Expedition 317 was devoted to understanding the relative importance of global sea level (eustasy) versus local tectonic and sedimentary processes in controlling continental margin sedimentary cycles. The expedition recovered sediments from the Eocene to recent period, with a particular focus on the sequence stratigraphy of the late Miocene to recent, when global sea level change was dominated by glacioeustasy. Drilling in the Canterbury Basin, on the eastern margin of the South Island of New Zealand, takes advantage of high rates of Neogene sediment supply, which preserves a high-frequency (0.1–0.5 m.y.) record of depositional cyclicity. The Canterbury Basin provides an opportunity to study the complex interactions between processes responsible for the preserved stratigraphic record of sequences because of the proximity of an uplifting mountain chain, the Southern Alps, and strong ocean currents. Currents have locally built large, elongate sediment drifts within the prograding Neogene section. Expedition 317 did not drill into one of these elongate drifts, but currents are inferred to have strongly influenced deposition across the basin, including in locations lacking prominent mounded drifts. Upper Miocene to recent sedimentary sequences were cored in a transect of three sites on the continental shelf (landward to basinward, Sites U1353, U1354, and U1351) and one on the continental slope (Site U1352). The transect provides a stratigraphic record of depositional cycles across the shallow-water environment most directly affected by relative sea level change. Lithologic boundaries, provisionally correlative with seismic sequence boundaries, have been identified in cores from each site and provide insights into the origins of seismically resolvable sequences. This record will be used to estimate the timing and amplitude of global sea level change and to document the sedimentary processes that operate during sequence formation. Sites U1353 and U1354 provide significant, double-cored, high-recovery sections through the Holocene and late Quaternary for high-resolution study of recent glacial cycles in a continental shelf setting. Continental slope Site U1352 represents a complete section from modern slope terrigenous sediment to hard Eocene limestone, with all the associated lithologic, biostratigraphic, physical, geochemical, and microbiological transitions. The site also provides a record of ocean circulation and fronts during the last ~35 m.y. The early Oligocene (~30 Ma) Marshall Paraconformity was the deepest drilling target of Expedition 317 and is hypothesized to represent intensified current erosion or nondeposition associated with the initiation of thermohaline circulation following the separation of Australian and Antarctica. Expedition 317 set a number of scientific ocean drilling records: (1) deepest hole drilled in a single expedition and second deepest hole in the history of scientific ocean drilling (Hole U1352C, 1927 m); (2) deepest hole and second deepest hole drilled by the R/V JOIDES Resolution on a continental shelf (Hole U1351B, 1030 m; Hole U1353B, 614 m); (3) shallowest water depth for a site drilled by the JOIDES Resolution for scientific purposes (Site U1353, 84.7 m water depth); and (4) deepest sample taken by scientific ocean drilling for microbiological studies (1925 m, Site U1352). Expedition 317 supplements previous drilling of sedimentary sequences for sequence stratigraphic and sea level objectives, particularly drilling on the New Jersey margin (Ocean Drilling Program [ODP] Legs 150, 150X, 174A, and 174AX and IODP Expedition 313) and in the Bahamas (ODP Leg 166), but includes an expanded Pliocene section. Completion of at least one transect across a geographically and tectonically distinct siliciclastic margin was the necessary next step in deciphering continental margin stratigraphy. Expedition 317 also complements ODP Leg 181, which focused on drift development in more distal parts of the Eastern New Zealand Oceanic Sedimentary System (ENZOSS).

AB - Integrated Ocean Drilling Program (IODP) Expedition 317 was devoted to understanding the relative importance of global sea level (eustasy) versus local tectonic and sedimentary processes in controlling continental margin sedimentary cycles. The expedition recovered sediments from the Eocene to recent period, with a particular focus on the sequence stratigraphy of the late Miocene to recent, when global sea level change was dominated by glacioeustasy. Drilling in the Canterbury Basin, on the eastern margin of the South Island of New Zealand, takes advantage of high rates of Neogene sediment supply, which preserves a high-frequency (0.1–0.5 m.y.) record of depositional cyclicity. The Canterbury Basin provides an opportunity to study the complex interactions between processes responsible for the preserved stratigraphic record of sequences because of the proximity of an uplifting mountain chain, the Southern Alps, and strong ocean currents. Currents have locally built large, elongate sediment drifts within the prograding Neogene section. Expedition 317 did not drill into one of these elongate drifts, but currents are inferred to have strongly influenced deposition across the basin, including in locations lacking prominent mounded drifts. Upper Miocene to recent sedimentary sequences were cored in a transect of three sites on the continental shelf (landward to basinward, Sites U1353, U1354, and U1351) and one on the continental slope (Site U1352). The transect provides a stratigraphic record of depositional cycles across the shallow-water environment most directly affected by relative sea level change. Lithologic boundaries, provisionally correlative with seismic sequence boundaries, have been identified in cores from each site and provide insights into the origins of seismically resolvable sequences. This record will be used to estimate the timing and amplitude of global sea level change and to document the sedimentary processes that operate during sequence formation. Sites U1353 and U1354 provide significant, double-cored, high-recovery sections through the Holocene and late Quaternary for high-resolution study of recent glacial cycles in a continental shelf setting. Continental slope Site U1352 represents a complete section from modern slope terrigenous sediment to hard Eocene limestone, with all the associated lithologic, biostratigraphic, physical, geochemical, and microbiological transitions. The site also provides a record of ocean circulation and fronts during the last ~35 m.y. The early Oligocene (~30 Ma) Marshall Paraconformity was the deepest drilling target of Expedition 317 and is hypothesized to represent intensified current erosion or nondeposition associated with the initiation of thermohaline circulation following the separation of Australian and Antarctica. Expedition 317 set a number of scientific ocean drilling records: (1) deepest hole drilled in a single expedition and second deepest hole in the history of scientific ocean drilling (Hole U1352C, 1927 m); (2) deepest hole and second deepest hole drilled by the R/V JOIDES Resolution on a continental shelf (Hole U1351B, 1030 m; Hole U1353B, 614 m); (3) shallowest water depth for a site drilled by the JOIDES Resolution for scientific purposes (Site U1353, 84.7 m water depth); and (4) deepest sample taken by scientific ocean drilling for microbiological studies (1925 m, Site U1352). Expedition 317 supplements previous drilling of sedimentary sequences for sequence stratigraphic and sea level objectives, particularly drilling on the New Jersey margin (Ocean Drilling Program [ODP] Legs 150, 150X, 174A, and 174AX and IODP Expedition 313) and in the Bahamas (ODP Leg 166), but includes an expanded Pliocene section. Completion of at least one transect across a geographically and tectonically distinct siliciclastic margin was the necessary next step in deciphering continental margin stratigraphy. Expedition 317 also complements ODP Leg 181, which focused on drift development in more distal parts of the Eastern New Zealand Oceanic Sedimentary System (ENZOSS).

KW - Paleoceanography

KW - sea-level

KW - continental margin

KW - Canterbury Basin

U2 - 10.2204/iodp.pr.317.2010

DO - 10.2204/iodp.pr.317.2010

M3 - Book

BT - Canterbury Basin sea level

PB - Integrated Ocean Drilling Program Management International

ER -

Fulthorpe CS, Hoyanagi K, Crundwell MP, Dinarès-Turell J, Ding X, George SC et al. Canterbury Basin sea level: global and local controls on continental margin stratigraphy. Integrated Ocean Drilling Program Management International, 2010. 133 p. https://doi.org/10.2204/iodp.pr.317.2010