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Journal articles on the topic 'IODP 313'

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Author: Grafiati

Published: 10 December 2022

Last updated: 29 January 2023

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1

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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2

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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3

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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4

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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5

Mountain, G., and J. N. Proust. "The New Jersey Margin Scientific Drilling Project (IODP Expedition 313): Untangling the Record of Global and Local Sea-Level Changes." Scientific Drilling 10 (September 1, 2010): 26–34. http://dx.doi.org/10.5194/sd-10-26-2010.

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6

Nilsson, A., Y. S. Lee, I. Snowball, and M. Hill. "Magnetostratigraphic importance of secondary chemical remanent magnetizations carried by greigite (Fe3S4) in Miocene sediments, New Jersey shelf (IODP Expedition 313)." Geosphere 9, no. 3 (April 4, 2013): 510–20. http://dx.doi.org/10.1130/ges00854.1.

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7

Kotthoff, U., D. R. Greenwood, F. M. G. McCarthy, K. Müller-Navarra, and S. P. Hesselbo. "Vegetation and climate development on the North American Atlantic Coastal Plain from 33 to 13 million years ago (IODP Expedition 313)." Climate of the Past Discussions 9, no. 6 (December 13, 2013): 6551–603. http://dx.doi.org/10.5194/cpd-9-6551-2013.

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Abstract. We have investigated the palynology of sediment cores from Sites M0027 and M0029 of IODP Expedition 313 on the New Jersey shallow shelf, east coast of North America, spanning an age range of 33 to 13 million years before present. Additionally, a pollen assemblage from the Pleistocene was examined. The palynological results were statistically analyzed and complemented with pollen-based quantitative climate reconstructions. Transport-related bias of the pollen assemblages was identified via analysis of the ratio of terrestrial to marine palynomorphs, and considered when interpreting palaeovegetation and palaeoclimate from the pollen data. Results indicate that from the early Oligocene to the middle Miocene, the hinterland vegetation of the New Jersey shelf was characterized by oak-hickory forests in the lowlands and conifer-dominated vegetation in the highlands. The Oligocene witnessed several expansions of conifer forest, probably related to cooling events. The pollen-based climate data imply an increase in annual temperatures from ~12 °C to more than 15 °C during the Oligocene. The Mi-1 cooling event at the onset of the Miocene is reflected by an expansion of conifers and an annual temperature decrease by almost 3 °C, from 15 °C to 12.5 °C around 23 million years before present. Particularly low annual temperatures are also recorded for an interval around ~20 million years before present, which probably reflects the Mi-1aa cooling event. Generally, the Miocene ecosystem and climate conditions were very similar to those of the Oligocene in the hinterland of the New Jersey shelf. Miocene grasslands, as known from other areas in the USA during that time period, are not evident for the hinterland of the New Jersey shelf. Surprisingly, the palaeovegetation data for the hinterland of the New Jersey shelf do not show extraordinary changes during the Mid-Miocene climatic optimum at ~15 million years before present, except for a minor increase in deciduous-evergreen mixed forest taxa and a decrease in swamp forest taxa. Pollen-based annual temperature reconstructions show average annual temperatures of ~14 °C during the Mid-Miocene climatic optimum. We conclude that vegetation and regional climate in the hinterland of the New Jersey shelf did not react as sensitively to Oligocene and Miocene climate changes as other regions in North America or Europe. An additional explanation for the relatively low regional temperatures reconstructed for the Mid-Miocene climatic optimum could be an uplift of the Appalachian Mountains during the Miocene. The Pleistocene pollen assemblage probably derives from the Marine Isotope Chron 7 or 5e and shows climate conditions similar to present-day.

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8

Pierre, Catherine, Marie-Madeleine Blanc-Valleron, Omar Boudouma, and Johanna Lofi. "Carbonate and silicate cementation of siliciclastic sediments of the New Jersey shelf (IODP Expedition 313): relation with organic matter diagenesis and submarine groundwater discharge." Geo-Marine Letters 37, no. 6 (April 8, 2017): 537–47. http://dx.doi.org/10.1007/s00367-017-0506-6.

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9

Kotthoff, U., D. R. Greenwood, F. M. G. McCarthy, K. Müller-Navarra, S. Prader, and S. P. Hesselbo. "Late Eocene to middle Miocene (33 to 13 million years ago) vegetation and climate development on the North American Atlantic Coastal Plain (IODP Expedition 313, Site M0027)." Climate of the Past 10, no. 4 (August 25, 2014): 1523–39. http://dx.doi.org/10.5194/cp-10-1523-2014.

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Abstract. We investigated the palynology of sediment cores from Site M0027 of IODP (Integrated Ocean Drilling Program) Expedition 313 on the New Jersey shallow shelf to examine vegetation and climate dynamics on the east coast of North America between 33 and 13 million years ago and to assess the impact of over-regional climate events on the region. Palynological results are complemented with pollen-based quantitative climate reconstructions. Our results indicate that the hinterland vegetation of the New Jersey shelf was characterized by oak–hickory forests in the lowlands and conifer-dominated vegetation in the highlands from the early Oligocene to the middle Miocene. The Oligocene witnessed several expansions of conifer forest, probably related to cooling events. The pollen-based climate data imply an increase in annual temperatures from ∼11.5 °C to more than 16 °C during the Oligocene. The Mi-1 cooling event at the onset of the Miocene is reflected by an expansion of conifers and mean annual temperature decrease of ∼4 °C, from ∼16 °C to ∼12 °C around 23 million years before present. Relatively low annual temperatures are also recorded for several samples during an interval around ∼20 million years before present, which may reflect the Mi-1a and the Mi-1aa cooling events. Generally, the Miocene ecosystem and climate conditions were very similar to those of the Oligocene. Miocene grasslands, as known from other areas in the USA during that time period, are not evident for the hinterland of the New Jersey shelf, possibly reflecting moisture from the proto-Gulf Stream. The palaeovegetation data reveal stable conditions during the mid-Miocene climatic optimum at ∼15 million years before present, with only a minor increase in deciduous–evergreen mixed forest taxa and a decrease in swamp forest taxa. Pollen-based annual temperature reconstructions show average annual temperatures of ∼14 °C during the mid-Miocene climatic optimum, ∼2 °C higher than today, but ∼1.5 °C lower than preceding and following phases of the Miocene. We conclude that vegetation and regional climate in the hinterland of the New Jersey shelf did not react as sensitively to Oligocene and Miocene climate changes as other regions in North America or Europe due to the moderating effects of the North Atlantic. An additional explanation for the relatively low regional temperatures reconstructed for the mid-Miocene climatic optimum could be an uplift of the Appalachian Mountains during the Miocene, which would also have influenced the catchment area of our pollen record.

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10

Cosgrove, Grace I. E., David M. Hodgson, Nigel P. Mountney, and William D. McCaffrey. "High-resolution correlations of strata within a sand-rich clinothem using grain fabric data, offshore New Jersey, USA." Geosphere 15, no. 4 (June 5, 2019): 1291–322. http://dx.doi.org/10.1130/ges02046.1.

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Abstract Trajectories of successive clinoform rollovers are widely applied to predict patterns of spatio-temporal sand distribution. However, the detailed internal architecture of individual clinothems is rarely documented. Understanding the textural complexities of complete topset-foreset-bottomset clinothem sequences is a key factor in understanding how and when sediment is transferred basinward. This study used high-resolution, core-based analyses of 267 samples from three research boreholes from quasi-coeval topset, foreset, and bottomset deposits of a single Miocene intrashelf clinothem recovered during Integrated Ocean Drilling Program (IODP) Expedition 313, offshore New Jersey, USA. Topset deposits were subdivided into three sedimentary packages based on grain character and facies analysis, consisting of upper and lower river-dominated topset process-regime packages separated by a middle wave- and storm-dominated process-regime package. Temporal variability in topset process regime exerts a quantifiable effect on grain character across the complete depositional profile, which was used here to correlate topset deposits with time-equivalent sedimentary packages in foreset and bottomset positions. River-dominated sedimentary packages have higher sand-to-mud ratios; however, the grain character of river-dominated sedimentary packages is texturally less mature than that of wave- and storm-dominated deposits. Differences in grain character between packages dominated by different process regimes increase basinward. The novel use of quantitative grain-character data allows intraclinothem time lines to be established at a higher resolution than is possible using chronostratigraphic techniques. Additionally, stratigraphic changes in grain character were used to refine the placement of the basal sequence boundary. These results challenge the idea that clinoform trajectories and stacking patterns are sufficient to describe spatio-temporal sand-body evolution across successive clinothems.

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11

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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12

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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13

Ali, Qamar, Zahid Hussain, Muhammad Raza Shah, and Donald VanDerveer. "4-Iodo-3,3′-dimethoxybiphenyl." Acta Crystallographica Section E Structure Reports Online 64, no. 8 (July 5, 2008): o1377. http://dx.doi.org/10.1107/s1600536808019557.

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14

Sohail, Muhammad, Wang Yao-Feng, Wang Qi, and Fu-Xue Chen. "7-Iodo-3,3-diphenyloctahydrobenzofuran." Acta Crystallographica Section E Structure Reports Online 69, no. 4 (March 23, 2013): o585. http://dx.doi.org/10.1107/s1600536813007563.

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15

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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16

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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17

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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18

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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19

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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20

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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21

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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22

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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23

Nicolet, M., O. Stetzer, F. Lüönd, O. Möhler, and U. Lohmann. "Single ice crystal measurements during nucleation experiments with the depolarization detector IODE." Atmospheric Chemistry and Physics 10, no. 2 (January 18, 2010): 313–25. http://dx.doi.org/10.5194/acp-10-313-2010.

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Abstract. In order to determine the efficiency of different aerosol particles to nucleate ice, an Ice Optical DEpolarization detector (IODE) was developed to distinguish between water droplets and ice crystals in ice nucleation chambers. A laser beam polarized linearly (power: 50 mW, wavelength: 407 nm) is directed through the chamber. The scattered light intensity from particles is measured at a scattering angle of Θ=175° in both polarization components (parallel and perpendicular). The ratio between the perpendicular intensity over the total one yields the depolarization ratio δ. Single particle detection is possible, using a peak detection algorithm. For high particle concentrations, a real-time signal averaging method can also be run simultaneously. The IODE detector was used in connection with the Zurich ice nucleation chamber during the ICIS 2007 workshop where ice nucleation experiments were performed with several aerosol types. In presence of ice crystals, a depolarization ratio could be measured on a particle-by-particle basis. Mean values of δ ranged from 0.24 to 0.37 and agree well with theoretical calculations.

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24

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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25

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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26

Channell, J. E. T., T. Sato, T. Kanamatsu, R. Stein, M. Malone, and C. Alvarez-Zarikian. "IODP Expeditions 303 and 306 Monitor Miocene- Quaternary Climate in the North Atlantic." Scientific Drilling 2 (March 1, 2006): 4–10. http://dx.doi.org/10.5194/sd-2-4-2006.

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27

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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28

Barlow, M. G., R. G. Pritchard, S. Tajammal, and A. E. Tipping. "3,3',4,4'-Tetrafluoro-4-iodo-1-phenyl-2,3-cyclobutenonaphthalene." Acta Crystallographica Section C Crystal Structure Communications 47, no. 9 (September 15, 1991): 1982–83. http://dx.doi.org/10.1107/s0108270191002081.

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29

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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30

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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31

Dikmetaş, Özlem, and Bogomil Voykov. "A Study on the intraocular pressure of the affected and unaffected eyes in patients with isolated cranial nerve palsies." Acta Medica 51, no. 1 (March 17, 2020): 15–20. http://dx.doi.org/10.32552/0.actamedica.422.

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Objective: The role of elevated intraocular pressure (IOP) in the incidence and progression of glaucoma is well known. However, the exact mechanisms of IOP regulation are still unclear. Central IOP control has been suggested, but the autonomic pathway through which it acts is not known. The aim of this study was to investigate if isolated cranial nerve (CN) palsies of the third, fourth and sixth nerves are associated with an IOP difference between the affected and the unaffected eyes. Materials and Methods: This was a retrospective study including patients diagnosed with a third, fourth and sixth nerve palsy at a single tertiary centre. We included only patients with an isolated unilateral palsy. Patients with a history of strabismus, orbital disease or neurosurgical cases were excluded. Results: The charts of 1712 patients were reviewed. Third, fourth and sixth nerve palsies were found in 469 patients, 314 patients and 929 patients, respectively. Of all patients, 190 (10.6%) were eligible for inclusion in the study. A third nerve, fourth nerve or sixth nerve palsy was present in 85 (44.7%), 65 (34.2%) and 40 (21.1%) patients, respectively. The mean IOP of the affected eyes and the unaffected eyes was not statistically significant different: 14.1 ± 3.1 mmHg vs. 14.6 ± 2.7 mmHg in the CN3 group (p=0.087); 13.6 ± 2.6 mmHg vs. 13.7 ± 2.3 mmHg in the CN4 group (p=0.69); and 14.3 ± 2.7 mmHg vs. 14.9 ± 3.3 mmHg in the CN6 group (p=0.089). There was no statistically significant difference between the mean IOP differences of the affected and unaffected eyes among the three groups (p=0.47). Conclusion: Our study demonstrated no difference in IOP between affected and unaffected eyes in patients with an isolated cranial nerve palsy. These findings are the first and important for ophthalmology practice.

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32

Toczko, S. T., A. J. Kopf, and E. Araki. "The IODP Expedition 332 : Eyes on the Prism, The NanTroSEIZE Observatories." Scientific Drilling 14 (September 1, 2012): 34–38. http://dx.doi.org/10.5194/sd-14-34-2012.

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The Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE) is a major long-term drilling project designed to investigate the seismogenic behavior of subduction zone plate boundaries. Integrated Ocean Drilling Program (IODP) Expedition 332 deployed a long-term borehole monitoring system (LTBMS), an advanced Circulation Obviation Retrofit Kit (CORK)-type observatory. The recovery of pressure and temperature data from a temporary observatory (SmartPlug) deployed during IODP Expedition 319 helped prove the SmartPlug concept. The permanent LTBMS was deployed n the upper 1000 m of Site C0002, while the SmartPlug was recovered from Site C0010 and replaced with a more capable "GeniusPlug", incorporating an extension with a geochem-ical sampler and biological experiment to the original SmartPlug design. SmartPlug pressure and temperature data showed signs of transient pressure events. <br><br> doi:<a href="http://dx.doi.org/10.2204/iodp.sd.14.04.2012" target="_blank">10.2204/iodp.sd.14.04.2012</a>

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33

Meira-Freitas, Daniel, Angelino Julio Cariello, Ruth Cardoso Vita, Ângela Tabosa, and Luiz Alberto S. Melo. "Short-Term Effect of Acupuncture on Intraocular Pressure in Healthy Subjects." Acupuncture in Medicine 28, no. 1 (March 2010): 25–27. http://dx.doi.org/10.1136/aim.2009.001081.

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Purpose To evaluate the short-term effect of acupuncture on the intraocular pressure (IOP) in healthy subjects. Methods A randomised controlled double-blinded trial was performed. 48 healthy volunteers (94 eyes) were randomly allocated to three groups: acupuncture group—19 subjects (38 eyes) were submitted to a 20 min session of acupuncture (GB1, GB14 and BL1); sham group—14 subjects (27 eyes) were submitted to a 20 min session of acupuncture with needles inserted in false points; and control group—15 subjects (29 eyes) who underwent no intervention. All subjects had the IOP measured by a masked investigator using Goldmann applanation tonometry immediately before intervention, as well as 20 min and 24 h after. Results The mean (SD) IOP in the acupuncture group was 17.9 (3.3) mm Hg at baseline, 16.4 (3.9) mm Hg at 20 min and 16.3 (3.3) mm Hg at 24 h. The mean (SD) IOP in the sham group was 18.6 (3.3) mm Hg at baseline, 17.7 (2.6) mm Hg at 20 min and 15.9 (3.6) mm Hg at 24 h. The mean (SD) IOP in the control group was 16.9 (3.5) mm Hg at baseline, 16.5 (3.8) mm Hg at 20 min and 15.8 (3.3) mm Hg at 24 h. There was no statistically significant difference in the IOP variation (post-intervention minus baseline measurements) between groups after 20 min (p=0.13) and 24 h (p=0.21). Conclusion Acupuncture in the studied points did not produce significant short-term effect on the IOP of healthy individuals in comparison with control groups. Clinical Trials Registration Number: NCT00639977

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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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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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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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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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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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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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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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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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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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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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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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45

Jiang, Zhiwei, Longlei Hou, Chunjie Ni, Jiangfei Chen, Dong Wang, and Xiaofeng Tong. "Enantioselective construction of quaternary tetrahydropyridines by palladium-catalyzed vinylborylation of alkenes." Chemical Communications 53, no. 30 (2017): 4270–73. http://dx.doi.org/10.1039/c7cc01488k.

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The Pd(0)-catalyzed asymmetric vinylborylation of (Z)-1-iodo-dienes with B₂pin₂ is reported, which provides access to 3,3-disubstituted tetrahydropyridine with excellent enantioselectivity.

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46

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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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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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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Dessì, Alessandro, Paola Peluso, Roberto Dallocchio, Robin Weiss, Giuseppina Andreotti, Mariateresa Allocca, Emmanuel Aubert, Patrick Pale, Victor Mamane, and Sergio Cossu. "Rational Design, Synthesis, Characterization and Evaluation of Iodinated 4,4′-Bipyridines as New Transthyretin Fibrillogenesis Inhibitors." Molecules 25, no. 9 (May 8, 2020): 2213. http://dx.doi.org/10.3390/molecules25092213.

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The 3,3′,5,5′-tetrachloro-2-iodo-4,4′-bipyridine structure is proposed as a novel chemical scaffold for the design of new transthyretin (TTR) fibrillogenesis inhibitors. In the frame of a proof-of-principle exploration, four chiral 3,3′,5,5′-tetrachloro-2-iodo-2′-substituted-4,4′- bipyridines were rationally designed and prepared from a simple trihalopyridine in three steps, including a Cu-catalysed Finkelstein reaction to introduce iodine atoms on the heteroaromatic scaffold, and a Pd-catalysed coupling reaction to install the 2′-substituent. The corresponding racemates, along with other five chiral 4,4′-bipyridines containing halogens as substituents, were enantioseparated by high-performance liquid chromatography in order to obtain pure enantiomer pairs. All stereoisomers were tested against the amyloid fibril formation (FF) of wild type (WT)-TTR and two mutant variants, V30M and Y78F, in acid mediated aggregation experiments. Among the 4,4′-bipyridine derivatives, interesting inhibition activity was obtained for both enantiomers of the 3,3′,5,5′-tetrachloro-2′-(4-hydroxyphenyl)-2-iodo-4,4′-bipyridine. In silico docking studies were carried out in order to explore possible binding modes of the 4,4′-bipyridine derivatives into the TTR. The gained results point out the importance of the right combination of H-bond sites and the presence of iodine as halogen-bond donor. Both experimental and theoretical evidences pave the way for the utilization of the iodinated 4,4′-bipyridine core as template to design new promising inhibitors of TTR amyloidogenesis.

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