de.pangaea.dataset733467 und dataset PANGAEA

info@pangaea.de

https://www.pangaea.de/ information pointOfContact 2026-02-06T11:46:37Z https://doi.pangaea.de/10.1594/PANGAEA.733467 2010-02-08T10:24:21 publication https://doi.org/10.1594/PANGAEA.733467 Sakamoto, Tatsuhiko

tats@bio.mie-u.ac.jp

author Janecek, Thomas R

curator@gly.fsu.edu

author Emeis, Kay-Christian

kay.emeis@uni-hamburg.de

https://orcid.org/0000-0003-0459-913X information author PANGAEA

info@pangaea.de

https://www.pangaea.de/ information publisher tableDigital Supplement to: Sakamoto, Tatsuhiko; Janecek, Thomas R; Emeis, Kay-Christian (1998): Continuous sedimentary sequences from the Eastern Mediterranean Sea: composite depth sections. In: Robertson, AHF; Emeis, K-C; Richter, C; Camerlenghi, A (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, 160: College Station, TX (Ocean Drilling Program), 160, 37-59, https://doi.org/10.2973/odp.proc.sr.160.053.1998 We have developed revised postcruise composite depth sections over the ~100-m-long, Pliocene-Holocene sediment sequences at four paleoceanographic sites (Site 964: Ionian Basin; Sites 966 and 967: Eratosthenes Seamount; Site 969: Mediterranean Ridge), which are located in different tectonic and oceanographic settings and water depths in the Eastern Mediterranean Sea. These revised composite sections were constructed using correlation intervals of a few centimeters instead of the 1- to 10-m intervals used in the shipboard composite construction procedure. These revised composite depth sections now take into account differential stretching and squeezing within a core and correct depth differences between holes caused by coring artifact and tectonic disturbances that resulted in attenuated and incomplete sections. The revised composite depth sections were constructed by combining digitized color images of split cores, visual core descriptions from shipboard operations, and color reflectance measurements with a 2-cm sampling resolution. The detailed revised depth sequences not only enable us to correlate sapropels between holes, but also other lithofacies, such as pale nannofossil oozes, reddish oozes, dark clays, and ash layers. Depending on the location of the drill site, over 80 individual sapropels are recognized in the revised composite depth sections. During Leg 160, use of the advanced piston coring system on the JOIDES Resolution typically resulted in an average gap between cores of 1-2 m, with a maximum of 8 m. Gaps within cores, resulting from faulting, slumping, or mass flows, also averaged 1-2 m in length. These revised composite depth sections can be used as starting points for the development of highresolution time scales and paleoceanographic time series in the Mediterranean. completed Sakamoto, Tatsuhiko

tats@bio.mie-u.ac.jp

principalInvestigator IODP Integrated Ocean Drilling Program / International Ocean Discovery Program theme 1995-01-01 creation PANGAEA

info@pangaea.de

https://www.pangaea.de/ information pointOfContact copyright copyright CC-BY-3.0: Creative Commons Attribution 3.0 Unported textTable und geoscientificInformation 32.7253 32.7253 34.0683 34.0683 1995-04-01T23:50:00 1995-04-02T11:40:00 0.02 120.12 DEPTH, sediment/rock physicalMeasurement m m Depth, composite revised physicalMeasurement Spectrophotometer Minolta CM-2002 rmcd rmcd Sample code/label thematicClassification Spectrophotometer Minolta CM-2002 Color, L*, lightness thematicClassification Spectrophotometer Minolta CM-2002 Color, a* thematicClassification Spectrophotometer Minolta CM-2002 Color, b* thematicClassification Spectrophotometer Minolta CM-2002 Color code HLS-system thematicClassification Spectrophotometer Minolta CM-2002; Munsell (hue) Color code HLS-system thematicClassification Spectrophotometer Minolta CM-2002; Munsell (value) Color code HLS-system thematicClassification Spectrophotometer Minolta CM-2002; Munsell (chroma) Color reflectance at 400 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 410 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 420 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 430 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 440 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 450 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 460 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 470 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 480 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 490 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 500 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 510 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 520 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 530 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 540 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 550 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 560 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 570 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 580 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 590 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 600 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 610 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 620 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 630 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 640 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 650 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 660 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 670 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 680 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 690 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % Color reflectance at 700 nm physicalMeasurement Spectrophotometer Minolta CM-2002 % % text/tab-separated-values unknown https://doi.pangaea.de/10.1594/PANGAEA.733467?format=textfile download dataset The data set was checked for completeness, correctness, and consistency of metainformation. Validity of used methods was checked and - if applicable - precision and range of data. EVENT LABEL: 160-967A * LATITUDE: 34.068300 * LONGITUDE: 32.725300 * DATE/TIME START: 1995-04-01T23:50:00 * DATE/TIME END: 1995-04-02T11:40:00 * ELEVATION: -2553.0 m * Penetration: 141.3 m * Recovery: 142.14 m * LOCATION: Eastern Basin * CAMPAIGN: Leg160 * BASIS: Joides Resolution * METHOD/DEVICE: Drilling/drill rig 16 cores; 141.3 m cored; 0 m drilled; 100.6 % recovery 1995-04-01T23:50:00 Related to 2007-01-01 publication https://doi.org/10.1016/j.margeo.2007.03.004 Heslop, David

david.heslop@anu.edu.au

https://orcid.org/0000-0001-8245-0555 information author von Dobeneck, Tilo

tvondobeneck@marum.de

https://orcid.org/0000-0002-0087-4053 information author Höcker, Mathias author documentDigital Marine Geology 241(1-4) 63-78