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Author: Grafiati

Published: 10 December 2022

Last updated: 29 January 2023

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1

Fulthorpe, C. S., K. Hoyanagi, and P. Blum. "IODP Expedition 317: Exploring the Record of Sea-Level Change Off New Zealand." Scientific Drilling 12 (September 1, 2011): 4–14. http://dx.doi.org/10.5194/sd-12-4-2011.

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2

Frieling, Joost, Emiel P. Huurdeman, Charlotte C. M. Rem, Timme H. Donders, Jörg Pross, Steven M. Bohaty, Guy R. Holdgate, Stephen J. Gallagher, Brian McGowran, and Peter K. Bijl. "Identification of the Paleocene–Eocene boundary in coastal strata in the Otway Basin, Victoria, Australia." Journal of Micropalaeontology 37, no. 1 (February 13, 2018): 317–39. http://dx.doi.org/10.5194/jm-37-317-2018.

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Abstract. Detailed, stratigraphically well-constrained environmental reconstructions are available for Paleocene and Eocene strata at a range of sites in the southwest Pacific Ocean (New Zealand and East Tasman Plateau; ETP) and Integrated Ocean Discovery Program (IODP) Site U1356 in the south of the Australo-Antarctic Gulf (AAG). These reconstructions have revealed a large discrepancy between temperature proxy data and climate models in this region, suggesting a crucial error in model, proxy data or both. To resolve the origin of this discrepancy, detailed reconstructions are needed from both sides of the Tasmanian Gateway. Paleocene–Eocene sedimentary archives from the west of the Tasmanian Gateway have unfortunately remained scarce (only IODP Site U1356), and no well-dated successions are available for the northern sector of the AAG. Here we present new stratigraphic data for upper Paleocene and lower Eocene strata from the Otway Basin, southeast Australia, on the (north)west side of the Tasmanian Gateway. We analyzed sediments recovered from exploration drilling (Latrobe-1 drill core) and outcrop sampling (Point Margaret) and performed high-resolution carbon isotope geochemistry of bulk organic matter and dinoflagellate cyst (dinocyst) and pollen biostratigraphy on sediments from the regional lithostratigraphic units, including the Pebble Point Formation, Pember Mudstone and Dilwyn Formation. Pollen and dinocyst assemblages are assigned to previously established Australian pollen and dinocyst zonations and tied to available zonations for the SW Pacific. Based on our dinocyst stratigraphy and previously published planktic foraminifer biostratigraphy, the Pebble Point Formation at Point Margaret is dated to the latest Paleocene. The globally synchronous negative carbon isotope excursion that marks the Paleocene–Eocene boundary is identified within the top part of the Pember Mudstone in the Latrobe-1 borehole and at Point Margaret. However, the high abundances of the dinocyst Apectodinium prior to this negative carbon isotope excursion prohibit a direct correlation of this regional bio-event with the quasi-global Apectodinium acme at the Paleocene–Eocene Thermal Maximum (PETM; 56 Ma). Therefore, the first occurrence of the pollen species Spinizonocolpites prominatus and the dinocyst species Florentinia reichartii are here designated as regional markers for the PETM. In the Latrobe-1 drill core, dinocyst biostratigraphy further indicates that the early Eocene (∼ 56–51 Ma) sediments are truncated by a ∼ 10 Myr long hiatus overlain by middle Eocene (∼ 40 Ma) strata. These sedimentary archives from southeast Australia may prove key in resolving the model–data discrepancy in this region, and the new stratigraphic data presented here allow for detailed comparisons between paleoclimate records on both sides of the Tasmanian Gateway.

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3

Ding, Xuan, YingYing Wu, and Wen Li. "0.9 Ma oxygen isotope stratigraphy for a shallow-water sedimentary transect across three IODP 317 sites in the Canterbury Bight of the southwest Pacific Ocean." Palaeogeography, Palaeoclimatology, Palaeoecology 465 (January 2017): 1–13. http://dx.doi.org/10.1016/j.palaeo.2016.10.008.

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4

TOKI, TOMOHIRO, YUTO UEHARA, KAZUNARI KINJO, AKIRA IJIRI, URUMU TSUNOGAI, HITOSHI TOMARU, and JUICHIRO ASHI. "Methane production and accumulation in the Nankai accretionary prism: Results from IODP Expeditions 315 and 316." GEOCHEMICAL JOURNAL 46, no. 2 (2012): 89–106. http://dx.doi.org/10.2343/geochemj.1.0155.

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5

Nassiri, N., N. Nassiri, S. Sadeghi Yarandi, B. Mohammadi, and L. Rahmani. "Combined Phacoemulsification and Ahmed Valve Glaucoma Drainage Implant: A Retrospective Case Series." European Journal of Ophthalmology 18, no. 2 (March 2008): 191–98. http://dx.doi.org/10.1177/112067210801800205.

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Purpose To report on the efficacy and safety of combined phacoemulsification and an Ahmed valve glaucoma drainage implant with respect to visual acuity improvement, intraocular pressure (IOP) control, and requirement for antiglaucoma medication. Methods A retrospective chart review was conducted of 41 eyes (31 patients) with coexisting visually significant cataracts and uncontrolled glaucoma who had combined phacoemulsification and Ahmed valve implantation. The outcome measures were: visual acuity, IOP, antiglaucoma medication requirements, and intra- and post-operative complications. Success was categorized as absolute (IOPp<21 mmHg without the need for antiglaucoma medication) and relative (IOPp<21 mmHg with one or more antiglaucoma medications). Failure was considered to be an IOPp<6 mmHg or IOP>21 mmHg on maximally tolerated medications or any devastating complication. Results The mean patient age was 67.3±5.9 years old. The mean visual acuity improved from 0.73±0.5 to 0.16±0.16 (p=0.000). The mean IOP decreased from 28.2±3.1 to 16.8±2.1 (p=0.000, 40.4%), while the number of antiglaucoma medication decreased from 2.6±0.66 to 1.2±1.4 (p=0.000). The absolute and relative success rates were 56.1% and 31.7%, respectively; 5 eyes (12.2%) were considered failures. There were no intraoperative complications; postoperative complications occurred in 8 eyes (19.5%). A hypertensive phase was detected in 12 (29.3%) eyes. Conclusions Combined phacoemulsification and Ahmed valve glaucoma drainage implantation is a safe and effective alternative to phacotrabeculectomy in patients with coexisting cataract and refractory glaucoma.

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6

Harris, Robert N., Friederike Schmidt-Schierhorn, and Glenn Spinelli. "Heat flow along the NanTroSEIZE transect: Results from IODP Expeditions 315 and 316 offshore the Kii Peninsula, Japan." Geochemistry, Geophysics, Geosystems 12, no. 8 (August 2011): n/a. http://dx.doi.org/10.1029/2011gc003593.

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7

Withler, R. E., T. D. Beacham, R. F. Watkins, and T. A. Stevens. "Identification of Farm-reared and Native Chinook Salmon (Oncorhynchus tshawytscha) on the West Coast of Vancouver Island, British Columbia, Using the Nuclear DNA probe B2-2." Canadian Journal of Fisheries and Aquatic Sciences 51, S1 (December 19, 1994): 267–76. http://dx.doi.org/10.1139/f94-313.

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The chinook salmon DNA probe B2-2 was used to distinguish farm-reared (from two commercial farms) and native chinook salmon (Oncorhynchus tshawytscha) that were sampled from five populations on the west coast of Vancouver island. The Big Qualicum River population (east coast of Vancouver Island), which is believed to be the main progenitor of domesticated broodstocks used for aquaculture in British Columbia, was also sampled. The presence or absence and integrated optical densities (IODs) of three DNA fragments at 8.3 kilo base pairs (kbp) (band 1), 6.5 kbp (band 2), and 5.6 kbp (band 3) in the hybridization patterns of B2-2 on BamHI-restricted DNA were recorded for 269 chinook salmon. The frequency of occurrence of bands 2 and 3, and all seven measurements made of the relative and absolute values of the IODs of the three bands, varied significantly among populations. The IOD of band 3 provided the best discrimination among populations. The Big Qualicum and two fish farm populations were differentiated from all five west coast native populations. Discriminant analysis and a neural network were used independently to classify correctly to type an average of 97% of the native and 83% of the farm west coast DNA patterns used as test samples.

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8

Matsuzaki, Kenji M., Hiroshi Nishi, Hiroki Hayashi, Noritoshi Suzuki, Babu R. Gyawali, Minoru Ikehara, Takuyuki Tanaka, and Reishi Takashima. "Radiolarian biostratigraphic scheme and stable oxygen isotope stratigraphy in southern Japan (IODP Expedition 315 Site C0001)." Newsletters on Stratigraphy 47, no. 1 (April 1, 2014): 107–30. http://dx.doi.org/10.1127/0078-0421/2014/0044.

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9

Song, Buhan, and Boo-Keun Khim. "Biogenic Opal Production and Paleoclimate Change in the Wilkes Land Continental Rise (East Antarctica) during the Mid-to-late Miocene (IODP Exp 318 Site U1359)." Ocean and Polar Research 37, no. 1 (March 30, 2015): 23–35. http://dx.doi.org/10.4217/opr.2015.37.1.023.

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10

Riedel, M., T. Collett, and M. J. Malone. "Gas hydrate drilling transect across northern Cascadia margin - IODP Expedition 311." Geological Society, London, Special Publications 319, no. 1 (2009): 11–19. http://dx.doi.org/10.1144/sp319.2.

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11

McNeill, L., D. Saffer, T. Byrne, E. Araki, S. Toczko, N. Eguchi, and K. Takahashi. "IODP Expedition 319, NanTroSEIZE Stage 2: First IODP Riser Drilling Operations and Observatory Installation Towards Understanding Subduction Zone Seismogenesis." Scientific Drilling 10 (September 1, 2010): 4–13. http://dx.doi.org/10.5194/sd-10-4-2010.

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The Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE) is a major drilling project designed to investigate fault mechanics and the seismogenic behavior of subduction zone plate boundaries. Expedition 319 is the first riser drilling operation within scientific ocean drilling. Operations included riser drilling at Site C0009 in the forearc basin above the plate boundary fault, non-riser drilling at Site C0010 across the shallow part of the megasplay fault system – which may slip during plate boundary earthquakes – and initial drilling at Site C0011 (incoming oceanic plate) for Expedition 322. At Site C0009, new methods were tested, including analysis of drill mud cuttings and gas, and <i>in situ</i> measurements of stress, pore pressure, and permeability. These results, in conjunction with earlier drilling, will provide (a) the history of forearc basin development (including links to growth of the megasplay fault system and modern prism), (b) the first <i>in situ</i> hydrological measurements of the plate boundary hanging wall, and (c) integration of <i>in situ</i> stress measurements (orientation and magnitude) across the forearc and with depth. A vertical seismic profile (VSP) experiment provides improved constraints on the deeper structure of the subduction zone. At Site C0010, logging-while-drilling measurements indicate significant changes in fault zone and hanging wall properties over short (< 5 km) along-strike distances, suggesting different burial and/or uplift history. The first borehole observatory instruments were installed at Site C0010 to monitor pressure and temperature within the megasplay fault zone, and methods of deployment of more complex observatory instruments were tested for future operations. <br><br> doi:<a href="http://dx.doi.org/10.2204/iodp.sd.10.01.2010" target="_blank">10.2204/iodp.sd.10.01.2010</a>

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12

Matsuzaki, Kenji M., Noritoshi Suzuki, Hiroshi Nishi, Hiroki Hayashi, Babu R. Gyawali, Reishi Takashima, and Minoru Ikehara. "Early to Middle Pleistocene paleoceanographic history of southern Japan based on radiolarian data from IODP Exp. 314/315 Sites C0001 and C0002." Marine Micropaleontology 118 (June 2015): 17–33. http://dx.doi.org/10.1016/j.marmicro.2015.05.001.

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13

Tan, L. S., A. Raman, K. M. Ng, S. J. Chua, A. T. S. Wee, and S. L. Lim. "Ohmic Contact Formation on Silicon-doped Gallium Nitride Epilayers by Low Temperature Annealing." Materials Science Forum 338-342 (May 2000): 1619. http://dx.doi.org/10.4028/www.scientific.net/msf.338-342.1619.

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“removed due to double publication”. The original paper: Journal: Semiconductor Science and Technology Create an alertIssue Volume 15, Number 6 Citation: L S Tan et al 2000 Semicond. Sci. Technol. 15 585 doi: 10.1088/0268-1242/15/6/317 can be accesses at IOP: http://iopscience.iop.org/0268-1242/15/6/317

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14

Miyakawa, Ayumu, Saneatsu Saito, Yasuhiro Yamada, Hitoshi Tomaru, Masataka Kinoshita, and Takeshi Tsuji. "Gas hydrate saturation at S ite C 0002, IODP E xpeditions 314 and 315, in the K umano B asin, N ankai trough." Island Arc 23, no. 2 (April 7, 2014): 142–56. http://dx.doi.org/10.1111/iar.12064.

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15

Torres, M. E., A. M. Tréhu, N. Cespedes, M. Kastner, U. G. Wortmann, J. H. Kim, P. Long, et al. "Methane hydrate formation in turbidite sediments of northern Cascadia, IODP Expedition 311." Earth and Planetary Science Letters 271, no. 1-4 (July 2008): 170–80. http://dx.doi.org/10.1016/j.epsl.2008.03.061.

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16

Escutia, C., H. Brinkhuis, and A. Klaus. "IODP Expedition 318: From Greenhouse to Icehouse at the Wilkes Land Antarctic Margin." Scientific Drilling 12 (September 1, 2011): 15–23. http://dx.doi.org/10.5194/sd-12-15-2011.

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Integrated Ocean Drilling Program (IODP) Expedition 318, Wilkes Land Glacial History, drilled a transect of sites across the Wilkes Land margin of Antarctica to provide a long-term record of the sedimentary archives of Cenozoic Antarctic glaciation and its intimate relationships with global climatic and oceanographic change. The Wilkes Land drilling program was undertaken to constrain the age, nature, and paleoenvironment of the previously only seismically inferred glacial sequences. The expedition (January–March 2010) recovered ~2000 meters of high-quality middle Eocene–Holocene sediments from water depths between 400 m and 4000 m at four sites on the Wilkes Land rise (U1355, U1356, U1359, and U1361) and three sites on the Wilkes Land shelf (U1357, U1358, and U1360). <br><br> These records span ~53 million years of Antarctic history, and the various seismic units (WL-S4–WL-S9) have been successfully dated. The cores reveal the history of the Wilkes Land Antarctic margin from an ice-free “greenhouse” Antarctica, to the first cooling, to the onset and erosional consequences of the first glaciation and the subsequent dynamics of the waxing and waning ice sheets, all the way to thick, unprecedented "tree ring style" records with seasonal resolution of the last deglaciation that began ~10,000 y ago. The cores also reveal details of the tectonic history of the Australo-Antarctic Gulf from 53 Ma, portraying the onset of the second phase of rifting between Australia and Antarctica, to ever-subsiding margins and deepening, to the present continental and ever-widening ocean/continent configuration. <br><br> doi:<a href="http://dx.doi.org/10.2204/iodp.sd.12.02.2011" target="_blank">10.2204/iodp.sd.12.02.2011</a>

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17

Ferdelman, T. G., A. Kano, and T. Williams. "IODP Expedition 307 Drills Cold-Water Coral Mound Along the Irish Continental Margin." Scientific Drilling 2 (March 1, 2006): 11–16. http://dx.doi.org/10.5194/sd-2-11-2006.

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18

Titschack, J., M. Thierens, B. Dorschel, C. Schulbert, A. Freiwald, A. Kano, C. Takashima, N. Kawagoe, and X. Li. "Carbonate budget of a cold-water coral mound (Challenger Mound, IODP Exp. 307)." Marine Geology 259, no. 1-4 (April 2009): 36–46. http://dx.doi.org/10.1016/j.margeo.2008.12.007.

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19

Tudge, J., M. A. Lovell, S. J. Davies, P. K. Harvey, and S. Saito. "Petrophysically determined lithofacies at the Nankai Trough Accretionary Prism: NanTroSEIZE, IODP Expedition 314." Journal of the Geological Society 166, no. 5 (September 2009): 961–68. http://dx.doi.org/10.1144/0016-76492008-136.

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20

Cai, Mingjiang, Zhaokai Xu, Peter D. Clift, Boo-Keun Khim, Dhongil Lim, Zhaojie Yu, Denise K. Kulhanek, and Tiegang Li. "Long-term history of sediment inputs to the eastern Arabian Sea and its implications for the evolution of the Indian summer monsoon since 3.7 Ma." Geological Magazine 157, no. 6 (December 27, 2018): 908–19. http://dx.doi.org/10.1017/s0016756818000857.

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AbstractWe present a new set of clay mineral and grain-size data for the siliciclastic sediment fraction from International Ocean Discovery Program (IODP) Site U1456 located in the eastern Arabian Sea to reconstruct the variabilities in the continental erosion and weathering intensity in the western Himalaya, elucidate the sediment source-to-sink processes and discuss the potential controls underlying these changes since 3.7 Ma. The clay minerals mainly consist of smectite (0–90%, average 44%) and illite (3–90%, average 44%), with chlorite (1–26%, average 7%) and kaolinite (0–19%, average 5%) as minor components. The compositional variations in the clay minerals at IODP Site U1456 suggest four phases of sediment provenance: the Indus River (phase 1, 3.7–3.2 Ma), the Indus River and Deccan Traps (phase 2, 3.2–2.6 Ma), the Indus River (phase 3, 2.6–1.2 Ma) and the Indus River and Deccan Traps (phase 4, 1.2–0 Ma). These provenance changes since 3.7 Ma can be correlated with variations in the Indian summer monsoon intensity. The siliciclastic sediments in the eastern Arabian Sea were mainly derived from the Indus River when the Indian summer monsoon was generally weak. In contrast, when the Indian summer monsoon intensified, the siliciclastic sediment supply from the Deccan Traps increased. In particular, this study shows that the smectite/(illite+chlorite) ratio is a sensitive tool for reconstructing the history of the variation in the Indian summer monsoon intensity over the continents surrounding the Arabian Sea since 3.7 Ma.

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21

Westphal, H., K. Heindel, M. Brandano, and J. Peckmann. "Genesis of microbialites as contemporaneous framework components of deglacial coral reefs, Tahiti (IODP 310)." Facies 56, no. 3 (December 11, 2009): 337–52. http://dx.doi.org/10.1007/s10347-009-0207-3.

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22

Rochon, F. D., and P. C. Kong. "Iodo-bridged complexes of platinum(II) and synthesis of cis mixed-amine platinum(II) compounds." Canadian Journal of Chemistry 64, no. 9 (September 1, 1986): 1894–96. http://dx.doi.org/10.1139/v86-312.

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Iodo-bridged platinum(II) dimers, [Pt(L)I2]2 with ligands (L) containing nitrogen as the donor atom, have been synthesized from the reactions of cis-[Pt(L)2I2] with perchloric acid. The dimers can be cleaved in aqueous media by a second nitrogen ligand to produce isometrically pure cis-[Pt(L)(L′)I2].These compounds can finally be converted to the chloro or carboxylato compounds by precipitating the iodo ligands with a silver salt and adding KCl or a carboxylate salt. Several compounds of the types cis-[Pt(L)(L′)Cl2] and cis-[Pt(L)(L′)(dicarboxylate)] were thus prepared. A few dimers of the type [(L)(L′)Pt(tetra-carboxylate)Pt(L)(L′)] were also synthesized.

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23

Durand, Nicolas, Pierre Deschamps, Edouard Bard, Bruno Hamelin, Gilbert Camoin, Alexander L. Thomas, Gideon M. Henderson, Yusuke Yokoyama, and Hiroyuki Matsuzaki. "Comparison of 14C and U-Th Ages in Corals from IODP #310 Cores Offshore Tahiti." Radiocarbon 55, no. 4 (2013): 1947–74. http://dx.doi.org/10.2458/azu_js_rc.v55i2.16134.

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Shallow-water tropical corals can be used to calibrate the radiocarbon timescale. In this paper, we present a new data set based on the comparison between 14C ages and U-Th ages measured in fossil corals collected offshore the island of Tahiti during the Integrated Oceanic Drilling Program (IODP) Expedition 310. After applying strict mineralogical and geochemical screening criteria, the Tahiti record provides new data for 2 distinct time windows: 7 data for the interval between 29 and 37 cal kyr BP and 58 for the last deglaciation period, notably a higher resolution for the 14–16 cal kyr BP time interval. There are 3 main outcomes of this study. First, it extends the previous Tahiti record beyond 13.9 cal kyr BP, the oldest U-Th age obtained on cores drilled onshore in the modern Tahiti barrier reef. Second, it strengthens the data set of the 14–15 cal kyr BP period, allowing for better documentation of the 14C age plateau in this time range. This age plateau corresponds to a drop of the atmospheric 14C synchronous with an abrupt period of sea-level rise (Melt Water Pulse 1 A, MWP-1 A). The Tahiti 14C record documents complex changes in the global carbon cycle due to variations in the exchange rates between its different reservoirs. Third, during the Heinrich event 1, the Tahiti record disagrees with the Cariaco record, but is in broad agreement with other marine and continental data.

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24

HEINDEL, K., D. BIRGEL, J. PECKMANN, H. KUHNERT, and H. WESTPHAL. "FORMATION OF DEGLACIAL MICROBIALITES IN CORAL REEFS OFF TAHITI (IODP 310) INVOLVING SULFATE-REDUCING BACTERIA." PALAIOS 25, no. 10 (October 1, 2010): 618–35. http://dx.doi.org/10.2110/palo.2010.p10-032r.

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25

Iryu, Yasufumi, Yasunari Takahashi, Kazuhiko Fujita, Gilbert Camoin, Guy Cabioch, Hiroki Matsuda, Tokiyuki Sato, Kaoru Sugihara, Jody M. Webster, and Hildegard Westphal. "Sealevel history recorded in the Pleistocene carbonate sequence in IODP Hole 310-M0005D, off Tahiti." Island Arc 19, no. 4 (October 14, 2010): 690–706. http://dx.doi.org/10.1111/j.1440-1738.2010.00737.x.

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26

Alt, J. C., D. A. H. Teagle, S. Umino, S. Miyashita, N. R. Banerjee, and D. S. Wilson. "IODP Expeditions 309 and 312 Drill an Intact Section of Upper Oceanic Basement into Gabbros." Scientific Drilling 4 (March 1, 2007): 4–10. http://dx.doi.org/10.5194/sd-4-4-2007.

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The Integrated Ocean Drilling Program’s (IODP) Expeditions 309 and 312 successfully completed the first sampling of an intact section of upper oceanic crust, through lavas and the sheeted dikes into the uppermost gabbros. Hole 1256D, which was initiated on the Ocean Drilling Program’s (ODP) Leg 206, now penetrates to > 1500 mbsf and > 1250 m sub-basement. The first gabbroic rocks were encountered at 1407 mbsf. Below this, the hole penetrates ~100 m into a complex zone of fractionated gabbros intruded into contact metamorphosed dikes. <br><br> doi:<a href="http://dx.doi.org/10.2204/iodp.sd.4.01.2007" target="_blank">10.2204/iodp.sd.4.01.2007</a>

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27

Woo, Kyung-Sik. "IODP Exp 310 Tahiti Sea-level Change: Diagenetic history of the pre-LGM reefal limestone." Quaternary International 279-280 (November 2012): 540. http://dx.doi.org/10.1016/j.quaint.2012.08.1893.

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28

Ferdelman, T. G., A. Kano, T. Williams, B. A. Cragg, T. D. Frank, J. J. Gharib, P. Léonide, et al. "Scientific drilling of a cold-water carbonate mound: Shipboard biogeochemical results from IODP Expedition 307." Geochimica et Cosmochimica Acta 70, no. 18 (August 2006): A170. http://dx.doi.org/10.1016/j.gca.2006.06.341.

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29

Camoin, Gilbert, and Claire Seard. "Genesis of microbialites as contemporaneous framework components of deglacial coral reefs, Tahiti (IODP 310): COMMENT." Facies 58, no. 1 (January 20, 2011): 163–65. http://dx.doi.org/10.1007/s10347-011-0264-2.

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30

Abbey, Elizabeth, Jody M. Webster, Juan C. Braga, Kaoru Sugihara, Carden Wallace, Yasufumi Iryu, Donald Potts, Terry Done, Gilbert Camoin, and Claire Seard. "Variation in deglacial coralgal assemblages and their paleoenvironmental significance: IODP Expedition 310, “Tahiti Sea Level”." Global and Planetary Change 76, no. 1-2 (March 2011): 1–15. http://dx.doi.org/10.1016/j.gloplacha.2010.11.005.

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31

Vastardis, Iraklis, Sofia Fili, Georgios Perdikakis, Kalliopi Kontopoulou, Zisis Gatzioufas, and Markus Kohlhaas. "The Efficacy of Ab Externo Canaloplasty by Using a Nonabsorbable Suture and No Viscoelastics; IOP Results, Intraoperative and Early Complication Rates within 6-Month Follow-Up Period." Klinische Monatsblätter für Augenheilkunde 238, no. 04 (April 2021): 380–90. http://dx.doi.org/10.1055/a-1386-3170.

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Abstract Background To report the efficacy of ab externo canaloplasty by exclusively using only a nonabsorbable suture as a standalone operation or combined with phacoemulsification in terms of mean intraocular pressure (IOP), medication reduction, and intra- and postoperative complication rates as well as additional glaucoma surgery. Patients and Methods Forty-eight patients with primary open-angle glaucoma (POAG) and 50 eyes were divided into two groups according to the operation performed (Group A canaloplasty, n = 34 and Group B canaloplasty combined with phaco, n = 16), respectively. The success criteria were evaluated between three IOP ranges: a) IOP ≤ 16 mmHg, b) ≤ 18 mmHg, and c) ≤ 21 mmHg. Complete success was considered the percentage of eyes reaching these goals with no medication and qualified success with or without medication. Groups A and B were compared with the Kaplan-Meier test. Mean IOP and medication reduction as well as additional glaucoma surgery were also evaluated. The follow-up time was 6 months. Statistical importance was given at p < 0.05. Results Fail rate and intraoperative conversion of canaloplasty to other surgery (trabeculotomy due to extensive cheese-wiring) accounted for 12% (6 eyes), while a mandatory usage of the iTrack 250A microcatheter to successfully overcome intracanalicular bridging of the Schlemmʼs canal accounted for 20% (10 eyes). The most common early postoperative complications in both groups were hyphema, cheese wiring, and transient IOP rising. The mean IOP in Group A reduced from 23.67 ± 6.06 mmHg to 13.35 ± 4.23 mmHg and in Group B, it reduced from 23.55 ± 6.19 mmHg to 12.75 ± 1.5 mmHg at 6 months (p < 0.001). Group Aʼs absolute success rates accounted for a) 44%, b) 47.1%, and c) 52.9% in comparison to Group B [a) 50%, b) 50%, and c) 56.3%] at 6 months (p < 0.05). Qualified success with or without medication showed no statistical differences between the groups. The mean medication reduction was significantly lower (p < 0.001) in both groups (Group A from baseline 3.2 ± 1.23 to 0.95 ± 1.35 and Group B from 3.12 ± 0.88 to 1.12 ± 0.75 at 6 months, respectively). Five eyes (10%) required additional glaucoma surgery. Conclusions Ab externo canaloplasty by exclusively using only a nonabsorbable suture as a standalone operation or combined with phacoemulsification seems to lower the mean IOP and medication sufficiently. However, they pose a greater surgical challenge and intraoperative complication rate. Additional glaucoma surgery or medication following both procedures may be necessary to achieve an optimal target IOP.

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Milliken, Kitty L., and Robert M. Reed. "Multiple causes of diagenetic fabric anisotropy in weakly consolidated mud, Nankai accretionary prism, IODP Expedition 316." Journal of Structural Geology 32, no. 12 (December 2010): 1887–98. http://dx.doi.org/10.1016/j.jsg.2010.03.008.

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33

Fujita, Kazuhiko, and Akitoshi Omori. "Modern and Pleistocene large-sized benthic foraminifers from Tahiti, French Polynesia, collected during IODP Expedition 310." Island Arc 24, no. 1 (May 20, 2014): 47–60. http://dx.doi.org/10.1111/iar.12069.

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34

Kitamura, Yujin, Toshiya Kanamatsu, and Xixi Zhao. "Structural evolution in accretionary prism toe revealed by magnetic fabric analysis from IODP NanTroSEIZE Expedition 316." Earth and Planetary Science Letters 292, no. 1-2 (March 15, 2010): 221–30. http://dx.doi.org/10.1016/j.epsl.2010.01.040.

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35

Ivanov, D. I., and V. N. Nikitin. "Surgical Treatment of Patients with Dislocation of IOL — Fibrosed Capsule Bag Complexes." Ophthalmology in Russia 19, no. 2 (June 30, 2022): 307–17. http://dx.doi.org/10.18008/1816-5095-2022-2-307-317.

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Violation of the correct location of the complex IOL capsule bag (CICB) in the delayed postoperative period occurs with a frequency of 0.2 to 2.8 %. The basis of the pathogenesis of this complication is the destruction of the zonal ligament due to progressive pseudoexfoliative syndrome, as well as the process of fibrosing the capsule bag. The stage of the flow and the different degree of severity of each mechanisms determines the variety of clinical manifestations. CICB dislocation in combination of these two mechanisms requires a special approach to treatment.Objective: to develop a system of surgical treatment of IOL dislocations in contract capsule syndrome, with varying degrees of severity, combined with the weakness of the ligament apparatus of the lens, and to present the results of its use.Patients and methods. Retrospective analysis of 55 cases of CICB dislocations with the observation period of more than 4 years operated in 2014-2016. Number of dislocations with certain IOL type: Hydrophilic monolithic — 27, Hydrophilic monolithic — 11, Hydrophilic three-part — 10, Hard — 7. The selection criterion was the presence of CICB dislocation in the combination of weakness of the ligament apparatus (II–III st. of severity) and contraction capsule syndrome, with varying degrees of severity. A system is proposed to allow a low-invasive repositioning of intraocular lenses dislocated with a fibrous capsule bag with subsequent suture fixation to the iris. Signs used for choice of surgical technique: localization of capsule bag fibrosis, contract effect of capsule bag fibrosis on IOL position and correct location of haptic elements, size, and severity of equatorial lens masses (Semmering ring). In cases when insufficiency of the ligament apparatus prevails, with insignificant fibrosis of the capsule bag, without contractional influence, fixation of KIKM to iris is carried out without cutting of the capsule bag (method 1). As the fibrous changes of the front or back leaf of the capsule progress without changing the position of IOL inside the capsule bag due to contraction, along with fixation of KIKM, the fibrous front/back capsule is excised (method 2). The variant of complete removal of the fibrous capsule bag is used in faraway stages of CCS with further fixation of IOL to the iris (method 3).Results. The data of BCVA and IOP of patients treated by a certain method (before the operation, early postoperative period (2–5 days), delayed period (more than 4 years)) are presented.Conclusion. Surgical treatment of patients with CICB dislocation combining manifestations of Capsule contraction syndrome and weakness of the lens ligament apparatus can now be standardized using a proper approach and certain methods of treatment, but requires a comprehensive assessment of such parameters as the safety of the ligament apparatus, the localization and degree of fibrous changes of the anterior / posterior capsule, the contractional effect of the capsule bag fibrosis on the front position of the IOL optics and the correct location of the haptic elements, the severity of the ring.

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36

Teagle, D. A. H., B. Ildefonse, and P. Blum. "IODP Expedition 335: Deep Sampling in ODP Hole 1256D." Scientific Drilling 13 (April 1, 2012): 28–34. http://dx.doi.org/10.5194/sd-13-28-2012.

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Observations of the gabbroic layers of untectonized ocean crust are essential to test theoretical models of the accretion of new crust at mid-ocean ridges. Integrated Ocean Drilling Program (IODP) Expedition 335 ("Superfast Spreading Rate Crust 4") returned to Ocean Drilling Program (ODP) Hole 1256D with the intention of deepening this reference penetration of intact ocean crust a significant distance (~350 m) into cumulate gabbros. Three earlier cruises to Hole 1256D (ODP 206, IODP 309/312) have drilled through the sediments, lavas, and dikes and 100 m into a complex dike-gabbro transition zone. <br><br> Operations on IODP Expedition 335 proved challenging throughout, with almost three weeks spent re-opening and securing unstable sections of the hole. When coring commenced, the comprehensive destruction of the coring bit required further remedial operations to remove junk and huge volumes of accumulated drill cuttings. Hole-cleaning operations using junk baskets were successful, and they recovered large irregular samples that document a hitherto unseen sequence of evolving geological conditions and the intimate coupling between temporally and spatially intercalated intrusive, hydrothermal, contact-metamorphic, partial melting, and retrogressive processes. <br><br> Hole 1256D is now clean of junk, and it has been thoroughly cleared of the drill cuttings that hampered operations during this and previous expeditions. At the end of Expedition 335, we briefly resumed coring before undertaking cementing operations to secure problematic intervals. To ensure the greatest scientific return from the huge efforts to stabilize this primary ocean lithosphere reference site, it would be prudent to resume the deepening of Hole 1256D in the nearest possible future while it is open to full depth. <br><br> doi:<a href="http://dx.doi.org/10.2204/iodp.sd.13.04.2011" target="_blank">10.2204/iodp.sd.13.04.2011</a>

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Vitish-Sharma, P., AG Acheson, C. Maxwell-Armstrong, K. Mohiuddin, B. Bharathan, K. Thomas, R. Stead, JA Sharp, and A. King. "PTH-317 The effect of trendelenburg positioning during laparoscopic colorectal surgery on intra-ocular pressure (IOP)." Gut 64, Suppl 1 (June 2015): A549.1—A549. http://dx.doi.org/10.1136/gutjnl-2015-309861.1203.

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38

Yamane, Masako, Yusuke Yokoyama, Yosuke Miyairi, Hisami Suga, Hiroyuki Matsuzaki, Robert B. Dunbar, and Naohiko Ohkouchi. "Compound-Specific 14C Dating of IODP Expedition 318 Core U1357A Obtained Off the Wilkes Land Coast, Antarctica." Radiocarbon 56, no. 3 (2014): 1009–17. http://dx.doi.org/10.2458/56.17773.

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This study applied compound-specific radiocarbon analysis (CSRA) to a 186-m-long sediment core (U1357A) taken from Adélie Basin located on the continental shelf off Wilkes Land, East Antarctica. The CSRA targeted C16 fatty acid as well as C16., fatty acid and cyclopheophorbide-a-enol isolated from the sediment. Due to their high degradation rate, these compounds are expected to occur in low abundances in relict organic matter deposited at this site. Twelve compound-specific (CS) 14C ages were obtained that are mostly consistent with their stratigraphic order. The CS 14C results of all samples are Holocene in age (9800 to 440 cal BP). These results suggest that significant sedimentation started ∼10,000 cal BP. Moreover, the data suggest that 14C measurements of C16:1 fatty acid and cyclopheophorbide-a-enol are useful for dating sediments from the Southern Ocean.

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Tauxe, L., C. E. Stickley, S. Sugisaki, P. K. Bijl, S. M. Bohaty, H. Brinkhuis, C. Escutia, et al. "Chronostratigraphic framework for the IODP Expedition 318 cores from the Wilkes Land Margin: Constraints for paleoceanographic reconstruction." Paleoceanography 27, no. 2 (June 2012): n/a. http://dx.doi.org/10.1029/2012pa002308.

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40

Fujita, Kazuhiko, Akitoshi Omori, Yusuke Yokoyama, Saburo Sakai, and Yasufumi Iryu. "Sea-level rise during Termination II inferred from large benthic foraminifers: IODP Expedition 310, Tahiti Sea Level." Marine Geology 271, no. 1-2 (May 2010): 149–55. http://dx.doi.org/10.1016/j.margeo.2010.01.019.

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41

Khim, Boo-Keun, Buhan Song, Hyen Goo Cho, Trevor Williams, and Carlota Escutia. "Late Neogene sediment properties in the Wilkes Land continental rise (IODP Exp. 318 Hole U1359A), East Antarctica." Geosciences Journal 21, no. 1 (January 17, 2017): 21–32. http://dx.doi.org/10.1007/s12303-016-0037-6.

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42

Katz, M. E., J. V. Browning, K. G. Miller, D. H. Monteverde, G. S. Mountain, and R. H. Williams. "Paleobathymetry and sequence stratigraphic interpretations from benthic foraminifera: Insights on New Jersey shelf architecture, IODP Expedition 313." Geosphere 9, no. 6 (October 11, 2013): 1488–513. http://dx.doi.org/10.1130/ges00872.1.

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43

Breuker, Anja, Susanne Stadler, and Axel Schippers. "Microbial community analysis of deeply buried marine sediments of the New Jersey shallow shelf (IODP Expedition 313)." FEMS Microbiology Ecology 85, no. 3 (May 29, 2013): 578–92. http://dx.doi.org/10.1111/1574-6941.12146.

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44

HEINDEL, KATRIN, MAX WISSHAK, and HILDEGARD WESTPHAL. "Microbioerosion in Tahitian reefs: a record of environmental change during the last deglacial sea-level rise (IODP 310)." Lethaia 42, no. 3 (September 2009): 322–40. http://dx.doi.org/10.1111/j.1502-3931.2008.00140.x.

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45

Camoin, G. F., Y. Iryu, and D. B. McInroy. "IODP Expedition 310 Reconstructs Sea Level, Climatic, and Environmental Changes in the South Pacific during the Last Deglaciation." Scientific Drilling 5 (September 1, 2007): 4–12. http://dx.doi.org/10.5194/sd-5-4-2007.

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46

DeLong, Kristine L., Terrence M. Quinn, Chuan-Chou Shen, and Ke Lin. "A snapshot of climate variability at Tahiti at 9.5 ka using a fossil coral from IODP Expedition 310." Geochemistry, Geophysics, Geosystems 11, no. 6 (June 2010): n/a. http://dx.doi.org/10.1029/2009gc002758.

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47

Proust, Jean-Noël, Hugo Pouderoux, Hisao Ando, Stephen P. Hesselbo, David M. Hodgson, Johanna Lofi, Marina Rabineau, and Peter J. Sugarman. "Facies architecture of Miocene subaqueous clinothems of the New Jersey passive margin: Results from IODP-ICDP Expedition 313." Geosphere 14, no. 4 (June 14, 2018): 1564–91. http://dx.doi.org/10.1130/ges01545.1.

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48

Webster, Gordon, Anna Blazejak, Barry A. Cragg, Axel Schippers, Henrik Sass, Joachim Rinna, Xiaohong Tang, et al. "Subsurface microbiology and biogeochemistry of a deep, cold-water carbonate mound from the Porcupine Seabight (IODP Expedition 307)." Environmental Microbiology 11, no. 1 (January 2009): 239–57. http://dx.doi.org/10.1111/j.1462-2920.2008.01759.x.

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Lu, Zunli, Christian Hensen, Udo Fehn, and Klaus Wallmann. "Halogen and129I systematics in gas hydrate fields at the northern Cascadia margin (IODP Expedition 311): Insights from numerical modeling." Geochemistry, Geophysics, Geosystems 9, no. 10 (October 2008): n/a. http://dx.doi.org/10.1029/2008gc002156.

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Prader, Sabine, Ulrich Kotthoff, Francine M. G. McCarthy, Gerhard Schmiedl, Timme H. Donders, and David R. Greenwood. "Vegetation and climate development of the New Jersey hinterland during the late Middle Miocene (IODP Expedition 313 Site M0027)." Palaeogeography, Palaeoclimatology, Palaeoecology 485 (November 2017): 854–68. http://dx.doi.org/10.1016/j.palaeo.2017.07.028.

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