"Exp"	"Site"	"Hole"	"Core"	"Type"	"Section"	"A/W"	"Sample ID"	"Offset top (cm)"	"Offset bottom (cm)"	"Top depth CSF-A (m)"	"Middle depth CSF-A (m)"	"Bottom depth CSF-A (m)"	"Top depth CSF-B (m)"	"Middle depth CSF-B (m)"	"Bottom depth CSF-B (m)"	"Domain no."	"Piece no."	"Core summary"	"Core comment"	
"397"	"U1385"	"H"	"2"	"X"	""	""	"397-U1385H-2X"	"0.0"	"722.0"	"114.600"	"118.210"	"121.820"	"114.6"	"118.21"	"121.82"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY and NANNOFOSSIL OOZE. Contacts between lithologies are bioturbated, irregular, and gradational. Foraminifera, color banding, and pyrite nodules are disseminated throughout. Bioturbation is moderate and trace fossils such Thalassinoides, Planolites, and Zoophycos are present. Severe fall-in is present in the first 21 cm of the section 1. Slightly biscuiting is observed in the remainder of the core. "	""	
"397"	"U1385"	"H"	"3"	"X"	""	""	"397-U1385H-3X"	"0.0"	"963.0"	"122.600"	"127.415"	"132.230"	"122.6"	"127.415"	"132.23"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY and NANNOFOSSIL OOZE. Contacts between lithologies are bioturbated, irregular, and gradational. Foraminifera and pyrite nodules are disseminated throughout. Bioturbation is moderate and trace fossils such Thalassinoides, Planolites, and Zoophycos are present. Severe fall-in is present in the first 6 cm of the section 1. Slightly biscuiting is observed in the remainder of the core. A void is present in the section 7 at 51-52 cm."	""	
"397"	"U1385"	"H"	"4"	"X"	""	""	"397-U1385H-4X"	"0.0"	"958.0"	"132.300"	"137.090"	"141.880"	"132.3"	"137.09"	"141.88"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY and NANNOFOSSIL OOZE. Contacts between lithologies are bioturbated, irregular, and gradational. Foraminifera, color banding, and pyrite nodules are disseminated throughout. Sandy patches and shell fragments are observed in section 2 at 134-140 cm. Bioturbation is moderate and trace fossils such Thalassinoides, Planolites, and Zoophycos are present. Severe fall-in is present in the first 7 cm of the section 1. Slightly biscuiting is observed in the remainder of the core. "	""	
"397"	"U1385"	"H"	"5"	"X"	""	""	"397-U1385H-5X"	"0.0"	"983.0"	"142.000"	"146.915"	"151.830"	"142"	"146.85"	"151.7"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY and NANNOFOSSIL OOZE. Contacts between lithologies are bioturbated, irregular, and gradational. Foraminifera and pyrite nodules are disseminated throughout. Bioturbation is moderate and trace fossils such Chondrites, Thalassinoides, Planolites, and Zoophycos are present. Moderate biscuiting is present throughout the core. Cracks are observed in the section 1 at 45-52 and 137-145 cm, the last one caused by core extension."	""	
"397"	"U1385"	"H"	"6"	"X"	""	""	"397-U1385H-6X"	"0.0"	"263.0"	"151.700"	"153.015"	"154.330"	"151.7"	"152.7"	"153.7"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY and NANNOFOSSIL OOZE. Contacts between lithologies are bioturbated, irregular, and gradational. Foraminifera and pyrite nodules are disseminated throughout. Bioturbation is moderate and trace fossils such Chondrites, Thalassinoides, and Planolites are present. Severe fall-in and strong fragmentation are present in the first 21 cm and at 101-103 cm, respectively in the section 1. Moderate to strong biscuiting and brecciated are present throughout the core. "	""	
"397"	"U1385"	"H"	"7"	"X"	""	""	"397-U1385H-7X"	"0.0"	"986.0"	"153.700"	"158.630"	"163.560"	"153.7"	"158.55"	"163.4"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY and NANNOFOSSIL OOZE. Contacts between lithologies are bioturbated, irregular, and gradational. Foraminifera, color banding, and pyrite nodules are disseminated throughout. Bioturbation is moderate and trace fossils such Zoophycos Thalassinoides, and Planolites are present. Slight biscuiting is present throughout the core. A void is present in the section 7 at 50-52 cm."	""	
"397"	"U1385"	"H"	"8"	"X"	""	""	"397-U1385H-8X"	"0.0"	"989.0"	"163.400"	"168.345"	"173.290"	"163.4"	"168.25"	"173.1"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY and NANNOFOSSIL OOZE. Contacts between lithologies are bioturbated, irregular, and gradational. Foraminifera, color banding, and pyrite nodules are disseminated throughout. Shell fragments are present in the section 1 at 82-83 cm. Bioturbation is moderate and trace fossils such Zoophycos Thalassinoides, and Planolites are present. Moderate biscuiting is present throughout the core. Strong fragmentation is present in the section 2 at 84-88 cm."	""	
"397"	"U1385"	"H"	"9"	"X"	""	""	"397-U1385H-9X"	"0.0"	"972.0"	"173.100"	"177.960"	"182.820"	"173.1"	"177.95"	"182.8"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY and NANNOFOSSIL OOZE. Contacts between lithologies are bioturbated, irregular, and gradational. Foraminifera, color banding, and pyrite nodules are disseminated throughout. Bioturbation is moderate and trace fossils such Zoophycos, Thalassinoides, and Planolites are present. Slightly sediment fragmentation, in the first 6 cm, and moderate biscuiting are observed throughout the core. In the section 1 and 4-7, the biscuits look strongly deformed. Voids are observed at 16-20 cm and 47-52 cm in the section 7."	""	
"397"	"U1385"	"H"	"10"	"X"	""	""	"397-U1385H-10X"	"0.0"	"978.0"	"182.800"	"187.690"	"192.580"	"182.8"	"187.65"	"192.5"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY and NANNOFOSSIL OOZE. Foraminifera, color banding, and pyrite nodules are disseminated throughout. Bioturbation is moderate and trace fossils such Chondrites, Thalassinoides, and Planolites are present. Fall-in is present in the section 1 at 0-5 cm. Slight biscuiting is present throughout the core. "	""	
"397"	"U1385"	"H"	"11"	"X"	""	""	"397-U1385H-11X"	"0.0"	"980.0"	"192.500"	"197.400"	"202.300"	"192.5"	"197.35"	"202.2"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY and NANNOFOSSIL OOZE. Foraminifera, color banding, and pyrite nodules are disseminated throughout. Dark smudges with foraminifera in Section 7 at 33-51 cm and Core Catcher. Bioturbation is moderate and trace fossils such Thalassinoides, and Planolites are present. Moderate biscuiting is present throughout the core. Moderate fragmentation is observed at 46-50 cm and 101-108 cm in the section 1."	""	
"397"	"U1385"	"H"	"12"	"X"	""	""	"397-U1385H-12X"	"0.0"	"987.0"	"202.200"	"207.135"	"212.070"	"202.2"	"207.05"	"211.9"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY and NANNOFOSSIL OOZE. Foraminifera, color banding, and pyrite are disseminated throughout. Bioturbation is moderate and trace fossils such as Thalassinoides and Chondrites are present. Slight biscuiting is present throughout the core. "	""	
"397"	"U1385"	"H"	"13"	"X"	""	""	"397-U1385H-13X"	"0.0"	"987.0"	"211.900"	"216.835"	"221.770"	"211.9"	"216.75"	"221.6"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY and NANNOFOSSIL OOZE. Foraminifera, color banding, and pyrite are disseminated throughout. Bioturbation is moderate and trace fossils such as Thalassinoides, Zoophycos, and Chondrites are present. Slight to moderate biscuiting is present throughout the core. "	""	
"397"	"U1385"	"H"	"14"	"X"	""	""	"397-U1385H-14X"	"0.0"	"982.0"	"221.600"	"226.510"	"231.420"	"221.6"	"226.45"	"231.3"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY and NANNOFOSSIL OOZE. Foraminifera, color banding, and pyrite are disseminated throughout. Bioturbation is moderate and trace fossils such as Thalassinoides, Zoophycos, and Chondrites are present. Slight to moderate biscuiting is present throughout the core. "	""	
"397"	"U1385"	"H"	"15"	"X"	""	""	"397-U1385H-15X"	"0.0"	"987.0"	"231.300"	"236.235"	"241.170"	"231.3"	"236.15"	"241"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY and NANNOFOSSIL OOZE. Foraminifera, color banding, and pyrite are disseminated throughout. Bioturbation is moderate and trace fossils such as Thalassinoides, Zoophycos, and Chondrites are present. Slight to moderate biscuiting is present throughout the core. Fall-in is present in the first 3 cm of Section 1. "	""	
"397"	"U1385"	"H"	"16"	"X"	""	""	"397-U1385H-16X"	"0.0"	"966.0"	"241.000"	"245.830"	"250.660"	"241"	"245.83"	"250.66"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY. Foraminifera, color banding, and pyrite are disseminated throughout. Bioturbation is moderate and trace fossils such as Thalassinoides, Planolites, Zoophycos, and Chondrites are present. Slight to strong biscuiting is present throughout the core. Section 1 and 2, 0-10 cm are severely disturbed by biscuiting and other disturbance.  "	""	
"397"	"U1385"	"H"	"17"	"X"	""	""	"397-U1385H-17X"	"0.0"	"989.0"	"250.700"	"255.645"	"260.590"	"250.7"	"255.55"	"260.4"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY. Foraminifera, color banding, and pyrite are disseminated throughout. Bioturbation is moderate and trace fossils such as Thalassinoides, Planolites, Zoophycos, and Chondrites are present. Slight to moderate biscuiting is present throughout the core. Fall-in is present in the first 9 cm of Section 1.   "	""	
"397"	"U1385"	"H"	"18"	"X"	""	""	"397-U1385H-18X"	"0.0"	"985.0"	"260.400"	"265.325"	"270.250"	"260.4"	"265.25"	"270.1"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY and NANNOFOSSIL OOZE. Contacts between lithologies are bioturbated, irregular, and gradational. Foraminifera, color banding, and pyrite are disseminated throughout. Bioturbation is moderate and trace fossils such as Thalassinoides, Planolites, Zoophycos, and Chondrites are present. Moderate to strong biscuiting is present throughout the core. Fall-in is present in the first 6 cm of Section 1.   "	""	
"397"	"U1385"	"H"	"19"	"X"	""	""	"397-U1385H-19X"	"0.0"	"990.0"	"270.100"	"275.050"	"280.000"	"270.1"	"274.95"	"279.8"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY and NANNOFOSSIL OOZE. Contacts between lithologies are color boundaries, straight, and gradational. Foraminifera, color banding, and pyrite are disseminated throughout. Bioturbation is moderate and trace fossils such as Thalassinoides, Zoophycos, Planolites, and Chondrites are present. Moderate to strong biscuiting is present throughout the core."	""	
"397"	"U1385"	"H"	"20"	"X"	""	""	"397-U1385H-20X"	"0.0"	"991.0"	"279.800"	"284.755"	"289.710"	"279.8"	"284.65"	"289.5"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY. Foraminifera, color banding, and pyrite are disseminated throughout. Bioturbation is moderate and trace fossils such as Thalassinoides, Zoophycos, and Chondrites are present. Moderate to strong biscuiting is present throughout the core."	""	
"397"	"U1385"	"H"	"21"	"X"	""	""	"397-U1385H-21X"	"0.0"	"972.0"	"289.500"	"294.360"	"299.220"	"289.5"	"294.35"	"299.2"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY and NANNOFOSSIL OOZE. Foraminifera, color banding, and pyrite nodules are disseminated throughout. Bioturbation is moderate and trace fossils such as Thalassinoides, Zoophycos, and Chondrites are present. Moderate biscuiting is present throughout the core."	""	
"397"	"U1385"	"H"	"22"	"X"	""	""	"397-U1385H-22X"	"0.0"	"987.0"	"299.200"	"304.135"	"309.070"	"299.2"	"304.05"	"308.9"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY and NANNOFOSSIL OOZE. Foraminifera, color banding, and pyrite nodules are disseminated throughout. Bioturbation is moderate and trace fossils such as Thalassinoides, Planolites, Zoophycos, Ophiomorpha, and Chondrites are present. Moderate biscuiting is present throughout the core. A severe void is observed between 50-51 cm."	""	
"397"	"U1385"	"H"	"23"	"X"	""	""	"397-U1385H-23X"	"0.0"	"971.0"	"308.900"	"313.755"	"318.610"	"308.9"	"313.75"	"318.6"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY. Foraminifera, color banding, and pyrite nodules (more abundant in the section 2) are disseminated throughout. Bioturbation is moderate and trace fossils such as Thalassinoides, Planolites, Zoophycos, and Chondrites are present. Fall-in is observed in the first 8 cm of the first section. Moderate biscuiting is present throughout the core."	""	
"397"	"U1385"	"H"	"24"	"X"	""	""	"397-U1385H-24X"	"0.0"	"984.0"	"318.600"	"323.520"	"328.440"	"318.6"	"323.45"	"328.3"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY. Contacts between lithologies are bioturbated, irregular, and gradational. Foraminifera, color banding, and pyrite nodules are disseminated throughout. Bioturbation is moderate and trace fossils such as Thalassinoides, Planolites and Chondrites are present. Moderate biscuiting is present throughout the core. Moderate to strong fragmentation is observed in the section 3 (123-125 cm) and section 4 (108-121 cm) caused by core extension"	""	
"397"	"U1385"	"H"	"25"	"X"	""	""	"397-U1385H-25X"	"0.0"	"222.0"	"328.300"	"329.410"	"330.520"	"328.3"	"329.41"	"330.52"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY. Contacts between lithologies are bioturbated, irregular, and gradational. Foraminifera, color banding, and pyrite nodules are disseminated throughout. Bioturbation is moderate and trace fossils such as Thalassinoides, Planolites and Chondrites are present. Severe fall-in is observed in the first 12 cm of the section 1. Moderate biscuiting is present throughout the core."	""	
"397"	"U1385"	"H"	"26"	"X"	""	""	"397-U1385H-26X"	"0.0"	"873.0"	"331.300"	"335.665"	"340.030"	"331.3"	"335.665"	"340.03"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY and NANNOFOSSIL OOZE. Contacts between lithologies are bioturbated, irregular, and gradational. Foraminifera, color banding, and pyrite nodules are disseminated throughout. Bioturbation is moderate and trace fossils such as Thalassinoides, Planolites, Zoophycos, and Chondrites are present. Severe fall-in is observed in the first 14 cm of the section 1. Moderate biscuiting is present throughout the core."	""	
"397"	"U1385"	"H"	"27"	"X"	""	""	"397-U1385H-27X"	"0.0"	"927.0"	"341.000"	"345.635"	"350.270"	"341"	"345.635"	"350.27"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY and NANNOFOSSIL OOZE. Contacts between lithologies are bioturbated, irregular, and gradational. Foraminifera, color banding, and pyrite nodules are disseminated throughout. Bioturbation is moderate and trace fossils such as Thalassinoides, Planolites, Zoophycos, and Chondrites are present. Severe fall-in is observed in the first 5 cm of the section 1. Moderate biscuiting is present throughout the core."	""	
"397"	"U1385"	"H"	"28"	"X"	""	""	"397-U1385H-28X"	"0.0"	"963.0"	"350.700"	"355.515"	"360.330"	"350.7"	"355.515"	"360.33"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY and NANNOFOSSIL OOZE. Contacts between lithologies are bioturbated, irregular, and gradational. Foraminifera, color banding, and pyrite nodules are disseminated throughout. Bioturbation is moderate and trace fossils such as Thalassinoides, Planolites, Zoophycos, Ophiomorpha and Chondrites are present. Severe fall-in is observed in the first 3 cm of the section 1. Moderate biscuiting is present throughout the core."	""	
"397"	"U1385"	"H"	"29"	"X"	""	""	"397-U1385H-29X"	"0.0"	"992.0"	"360.400"	"365.360"	"370.320"	"360.4"	"365.25"	"370.1"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY and NANNOFOSSIL OOZE. Contacts between lithologies are bioturbated, irregular, and gradational. Foraminifera, color banding, and pyrite nodules are disseminated throughout. Bioturbation is moderate and trace fossils such as Thalassinoides, Planolites, Zoophycos, and Chondrites are present. Severe fall-in is observed in the first 11 cm of the section 1. Moderate biscuiting is present throughout the core."	""	
"397"	"U1385"	"H"	"30"	"X"	""	""	"397-U1385H-30X"	"0.0"	"982.0"	"370.100"	"375.010"	"379.920"	"370.1"	"374.95"	"379.8"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY and NANNOFOSSIL OOZE. Contacts between lithologies are bioturbated, irregular, and gradational. Foraminifera, color banding, and pyrite nodules are disseminated throughout. Bioturbation is moderate and trace fossils such as Thalassinoides, Planolites, Zoophycos, and Chondrites are present. Moderate biscuiting is present throughout the core."	""	
"397"	"U1385"	"H"	"31"	"X"	""	""	"397-U1385H-31X"	"0.0"	"982.0"	"379.800"	"384.710"	"389.620"	"379.8"	"384.65"	"389.5"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY and NANNOFOSSIL OOZE. Contacts between lithologies are color boundaries, straight, and gradational. Foraminifera, color banding, and pyrite nodules are disseminated throughout. Bioturbation is moderate and trace fossils such as Thalassinoides, Planolites, Zoophycos, and Chondrites are present. Moderate biscuiting is present throughout the core."	""	
"397"	"U1385"	"H"	"32"	"X"	""	""	"397-U1385H-32X"	"0.0"	"984.0"	"389.500"	"394.420"	"399.340"	"389.5"	"394.35"	"399.2"	""	""	"This core is dominated by NANNOFOSSIL OOZE WITH CLAY and NANNOFOSSIL OOZE. Contacts between lithologies are color boundaries, straight, and gradational. Foraminifera, color banding, and pyrite are disseminated throughout. Bioturbation is moderate and trace fossils such as Thalassinoides, Planolites, Zoophycos, and Chondrites are present. Moderate biscuiting is present throughout the core."	""