"Leg 207, Site 1259 Thin Section Data" Sample Mineral Biogenic Rock Leg Site H Cor CT Sct Top (cm) Bot (cm) Depth (mbsf) Thin Section Number Lithology Calcite Clay Inorganic Calcite Feldspar Glauconite Fe-oxide Opaque minerals Pyrite Quartz Zeolite Zircon Fish Remains Bioclast Nannofossils Foraminifers Planktonic Foraminifer Benthic foraminifers Radiolarians Organic debris Shell fragments Microfossils Cement Micrite Sparite Lithic fragments Siliceous matrix Organic matter Lithology Comments 207 1259 A 26 R 3 121 124 241.11 76 D 12 35 1 50 1 1 100 Foraminifer packstone "Foraminifers are mainly filled with micrite, rarely with blocky calcite. Foraminifers are transported/winnowed. Small ones filling the space between big ones. Bioclasts are shell fragments. Micrite is matrix or cement." 207 1259 A 30 R 4 49 53.00 77 D 10 35 3 3 50 2 103 Foraminifer sand "Foraminifers filled with blocky calcite or probably broken out, empty-rare zeolite growth in chambers" 207 1259 A 38 R CC 0 5 359.24 31 D 35 1 2 12 8 42 100 Clayey carbonate wackestone with zeolite In broken piece out of nannofossil molds. Micrite includes nannofossils. 207 1259 A 49 R 1 55 57 458.95 78 D 9 1 * 50 40 100 Foraminifer wackestone to packstone "Foraminifers are filled with sparite, matrix (clayey) micrite. Bioclasts are bivalve shells." 207 1259 A 55 R 3 27 29 513.28 79 44 30 1 1 14 10 10 110 207 1259 A 59 R 4 110 113 544.93 81 D 20 * * * 5 50 15 10 10 110 Clayey limestone (with organic matter and clay) "The analyses show that total organic matter accounts for approximately 5% to 10%. 30% of micrite is clay and organic matter, 15% micritic (nannofossil) fecal pellets." 207 1259 A 59 R CC 19 22 546.61 80 D 10 3 * 1 8 75 3 3 103 Calcareous Wackestone Distinctly laminated. Micritic matrix consists of fecal pellets and is microsparitic. 207 1259 A 60 R 1 21 23 549.31 82 D 25 50 * 25 Quartz arenite "Quartz grains are predominantly angular to subangular. Some show undulous extinction. No quartz overgrowth is seen, except for rare concave/convex contacts. Matrix/cement is 25% clay and 25% micrite. Nannofossil fragments are present in ""cement""." 207 1259 B 24 R 4 38 40 548.48 105 M 5 15 * 30 50 100 Bioclastic limestone Angular quartz. Bioclasts are with neomorphic spar. 207 1259 B 24 R 4 49 52 548.59 99 D 5 10 15 65 5 100 Quartz arenite with opaque minerals Angular quartz. Calcite is large diagenetic calcite. Cement is carbonate. 207 1259 B 24 R 5 56 58 550.16 100 D 10 8 18 * 30 1 33 100 Bioclastic limestone with quartz "Bioclasts are mainly replaced by neomorphic spar, including echinoids, bivalve shells, gastropods. Sparite is microsparic cement." 207 1259 B 24 R 5 84 88 550.44 101 45 20 20 15 100 "Diagenetic limestone with clay, opaque minerals and quartz" "Opaque minerals include pebbles of pyrite. 20% of calcite is ""beef"" calcite, 25% is other diagenetic calcite." 207 1259 B 25 R 1 47 51 553.67 102 D 19 30 * 26 25 * 100 Partially pyritized quartz wacke to quartz arenite Opaque minerals include areas with pyrite replacing matrix. Calcite is diagenetic. 207 1259 B 25 R 1 113 117 554.33 103 D 46 10 25 1 * 15 3 100 Quartz wackestone (silt-sized) Very fine to extremely fine-grained quartz wacke. 207 1259 B 25 R 2 26 30 554.96 104 D 2 20 1 38 6 * 3 30 3 103 Very fine-grained quartz sandstone (wackestone) Bioclasts include echinoid fragments. Lithic fragments include quartzite and chert. Large crystals of diagenetic calcite incorporating quartz. 207 1259 C 11 R 3 11 13 492.04 106 D 20 6 10 4 3 2 55 100 Chalk with clay Distinctly glauconitic. 207 1259 C 11 R 4 19 21 493.62 107 M 2 20 * 27 4 3 5 4 3 30 2 100 Glauconitic claystone Diagenetic blocky calcite. Opaque minerals include several ~1mm pyrite nodules). Micrite is background matrix. Foraminifers are mainly fragments. 207 1259 C 15 R 2 42 45 515.72 108 10 10 2 25 10 2 5 36 100 Calcareous phosphorite with glauconite and foraminifer Microspar matrix. Cement is sparite. One big benthic foraminifer among planktonic foraminifers. Fish remains. 207 1259 C 17 R 5 86 90 534.72 109 D 16 3 2 2 50 25 2 100 Foraminifer wackestone with foraminifer packstone patches Micrite background. Bioclasts are long very thin shells.