Site U1607

Paul C. Knutz; Anne E. Jennings; Laurel B. Childress; Raquel M. Bryant; Samantha K. Cargill; Helen K. Coxall; Tracy D. Frank; Georgia R. Grant; Rachael E. Gray; Sandrine Le Houedec; Libby Ives; Vikash Kumar; Jannik Martens; Fawz Naim; Mei Nelissen; Volkan Özen; Sandra Passchier; Lara F. Pérez; Jian Ren; Brian W. Romans; Osamu Seki; Lisa  Tauxe; Emily J. Tibbett; Yuka Yokoyama; Yancheng Zhang; Heike Zimmermann

doi:10.14379/iodp.proc.400.107.2025

Osamu Seki, Lisa Tauxe, Emily J. Tibbett, Yuka Yokoyama, Yancheng Zhang, Heike Zimmermann

Publikation: Bidrag til bog/rapport/konferenceproceedings › Bogkapitel › Forskning › peer review

Resumé

Site U1607 (proposed Site MB-07B), the easternmost site in the Expedition 400 site transect, was cored at 74°29.5499′N, 60°34.9900′W at 739 meters below sea level (mbsl) on the middle shelf (Figure F1). Extensive seismic and limited borehole data indicate that this site captures Megaunits C, D1, and D2, interpreted as a middle–late Miocene sediment drift that overlies a succession of mainly hemipelagic strata, possibly of early Miocene to Oligocene age (Knutz et al., 2022b) (Figures F2, F3). Accordingly, Site U1607 may capture the time period from 6 to 30 Ma.

Originalsprog	Engelsk
Titel	NW Greenland Glaciated Margin
Redaktører	P.C. Knutz, A.E. Jennings, L.B. Childress
Forlag	International Ocean Discovery Program
Antal sider	56
ISBN (Elektronisk)	978-1-954252-93-6
DOI	https://doi.org/10.14379/iodp.proc.400.107.2025
Status	Udgivet - 24 mar. 2025

Publikationsserier

Navn	Proceedings of the International Ocean Discovery Program
Vol/bind	400

Programområde

Programområde 5: Natur og klima

Adgang til dokumentet

10.14379/iodp.proc.400.107.2025Licens: CC BY

Citationsformater

Knutz, P. C., Jennings, A. E., Childress, L. B., Bryant, R. M., Cargill, S. K., Coxall, H. K., Frank, T. D., Grant, G. R., Gray, R. E., Le Houedec, S., Ives, L., Kumar, V., Martens, J., Naim, F., Nelissen, M., Özen, V., Passchier, S., Pérez, L. F., Ren, J., ... Zimmermann, H. (2025). Site U1607. I P. C. Knutz, A. E. Jennings, & L. B. Childress (red.), NW Greenland Glaciated Margin International Ocean Discovery Program. https://doi.org/10.14379/iodp.proc.400.107.2025

@inbook{d99e3dc0bf2046ac847b77c07f816213,

title = "Site U1607",

abstract = "Site U1607 (proposed Site MB-07B), the easternmost site in the Expedition 400 site transect, was cored at 74°29.5499′N, 60°34.9900′W at 739 meters below sea level (mbsl) on the middle shelf (Figure F1). Extensive seismic and limited borehole data indicate that this site captures Megaunits C, D1, and D2, interpreted as a middle–late Miocene sediment drift that overlies a succession of mainly hemipelagic strata, possibly of early Miocene to Oligocene age (Knutz et al., 2022b) (Figures F2, F3). Accordingly, Site U1607 may capture the time period from 6 to 30 Ma.",

keywords = "Baffin Bay, contourites, Expedition 400, glacial–interglacial cycles, ice sheet instability, International Ocean Discovery Program, IODP, JOIDES Resolution, NW Greenland Glaciated Margin, Site U1607",

author = "Knutz, \{Paul C.\} and Jennings, \{Anne E.\} and Childress, \{Laurel B.\} and Bryant, \{Raquel M.\} and Cargill, \{Samantha K.\} and Coxall, \{Helen K.\} and Frank, \{Tracy D.\} and Grant, \{Georgia R.\} and Gray, \{Rachael E.\} and \{Le Houedec\}, Sandrine and Libby Ives and Vikash Kumar and Jannik Martens and Fawz Naim and Mei Nelissen and Volkan {\"O}zen and Sandra Passchier and P{\'e}rez, \{Lara F.\} and Jian Ren and Romans, \{Brian W.\} and Osamu Seki and Lisa Tauxe and Tibbett, \{Emily J.\} and Yuka Yokoyama and Yancheng Zhang and Heike Zimmermann",

year = "2025",

month = mar,

day = "24",

doi = "10.14379/iodp.proc.400.107.2025",

language = "English",

series = "Proceedings of the International Ocean Discovery Program",

publisher = "International Ocean Discovery Program",

editor = "P.C. Knutz and A.E. Jennings and L.B. Childress",

booktitle = "NW Greenland Glaciated Margin",

}

Knutz, PC, Jennings, AE, Childress, LB, Bryant, RM, Cargill, SK, Coxall, HK, Frank, TD, Grant, GR, Gray, RE, Le Houedec, S, Ives, L, Kumar, V, Martens, J, Naim, F, Nelissen, M, Özen, V, Passchier, S, Pérez, LF, Ren, J, Romans, BW, Seki, O, Tauxe, L, Tibbett, EJ, Yokoyama, Y, Zhang, Y & Zimmermann, H 2025, Site U1607. i PC Knutz, AE Jennings & LB Childress (red), NW Greenland Glaciated Margin. International Ocean Discovery Program, Proceedings of the International Ocean Discovery Program, bind 400. https://doi.org/10.14379/iodp.proc.400.107.2025

Site U1607. / Knutz, Paul C.; Jennings, Anne E.; Childress, Laurel B. et al.
NW Greenland Glaciated Margin. red. / P.C. Knutz; A.E. Jennings; L.B. Childress. International Ocean Discovery Program, 2025. (Proceedings of the International Ocean Discovery Program, Bind 400).

Publikation: Bidrag til bog/rapport/konferenceproceedings › Bogkapitel › Forskning › peer review

TY - CHAP

T1 - Site U1607

AU - Knutz, Paul C.

AU - Jennings, Anne E.

AU - Childress, Laurel B.

AU - Bryant, Raquel M.

AU - Cargill, Samantha K.

AU - Coxall, Helen K.

AU - Frank, Tracy D.

AU - Grant, Georgia R.

AU - Gray, Rachael E.

AU - Le Houedec, Sandrine

AU - Ives, Libby

AU - Kumar, Vikash

AU - Martens, Jannik

AU - Naim, Fawz

AU - Nelissen, Mei

AU - Özen, Volkan

AU - Passchier, Sandra

AU - Pérez, Lara F.

AU - Ren, Jian

AU - Romans, Brian W.

AU - Seki, Osamu

AU - Tauxe, Lisa

AU - Tibbett, Emily J.

AU - Yokoyama, Yuka

AU - Zhang, Yancheng

AU - Zimmermann, Heike

PY - 2025/3/24

Y1 - 2025/3/24

N2 - Site U1607 (proposed Site MB-07B), the easternmost site in the Expedition 400 site transect, was cored at 74°29.5499′N, 60°34.9900′W at 739 meters below sea level (mbsl) on the middle shelf (Figure F1). Extensive seismic and limited borehole data indicate that this site captures Megaunits C, D1, and D2, interpreted as a middle–late Miocene sediment drift that overlies a succession of mainly hemipelagic strata, possibly of early Miocene to Oligocene age (Knutz et al., 2022b) (Figures F2, F3). Accordingly, Site U1607 may capture the time period from 6 to 30 Ma.

AB - Site U1607 (proposed Site MB-07B), the easternmost site in the Expedition 400 site transect, was cored at 74°29.5499′N, 60°34.9900′W at 739 meters below sea level (mbsl) on the middle shelf (Figure F1). Extensive seismic and limited borehole data indicate that this site captures Megaunits C, D1, and D2, interpreted as a middle–late Miocene sediment drift that overlies a succession of mainly hemipelagic strata, possibly of early Miocene to Oligocene age (Knutz et al., 2022b) (Figures F2, F3). Accordingly, Site U1607 may capture the time period from 6 to 30 Ma.

KW - Baffin Bay

KW - contourites

KW - Expedition 400

KW - glacial–interglacial cycles

KW - ice sheet instability

KW - International Ocean Discovery Program

KW - IODP

KW - JOIDES Resolution

KW - NW Greenland Glaciated Margin

KW - Site U1607

UR - https://www.scopus.com/pages/publications/105003933761

U2 - 10.14379/iodp.proc.400.107.2025

DO - 10.14379/iodp.proc.400.107.2025

M3 - Chapter in book

T3 - Proceedings of the International Ocean Discovery Program

BT - NW Greenland Glaciated Margin

A2 - Knutz, P.C.

A2 - Jennings, A.E.

A2 - Childress, L.B.

PB - International Ocean Discovery Program

ER -