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Relevant bibliographies by topics / Palaeoceanography

Academic literature on the topic 'Palaeoceanography'

Author: Grafiati

Published: 4 June 2021

Last updated: 29 January 2023

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Journal articles on the topic "Palaeoceanography"

1

Robinson, Laura F., and Mark Siddall. "Palaeoceanography: motivations and challenges for the future." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 370, no. 1980 (December 13, 2012): 5540–66. http://dx.doi.org/10.1098/rsta.2012.0396.

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The ocean interacts with the atmosphere, biosphere and cryosphere in a complex way, modulating climate through the storage and transport of heat, nutrients and carbon. As such, it is important that we understand the ways in which the ocean behaves and the factors that can lead to change. In order to gain this understanding, we need to look back into the past, on time scales from recent decadal-scale change, through the abrupt changes of the Pleistocene and back to times when the Earth's climate was significantly different than the Holocene. A key challenge facing the field of palaeoceanography is to combine data and modelling in a common framework. Coupling palaeo-data and models should improve our knowledge of how the Earth works, and perhaps of more direct societal relevance, might enable us to provide better predictive capabilities in climate modelling. In this discussion paper, we examine the motivations, past successes and challenges facing palaeoceanographic studies. We then suggest a number of areas and approaches that we believe will allow palaeoceanography to continue to provide new insights into processes that affect future climate change.

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Young, Jeremy R., Jose-Abel Flores, and Mario Cachao. "Quaternary coccolithophore palaeoceanography." Marine Micropaleontology 69, no. 1 (October 2008): 1–2. http://dx.doi.org/10.1016/j.marmicro.2007.11.004.

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Elderfield, H. "North Atlantic Palaeoceanography." Quaternary Science Reviews 8, no. 1 (January 1989): 106–7. http://dx.doi.org/10.1016/0277-3791(89)90032-2.

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Suess, Erwin. "Palaeoceanography: Biomarkers for ancient climates." Nature 320, no. 6058 (March 1986): 107–8. http://dx.doi.org/10.1038/320107a0.

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Gyllencreutz, Richard, Jan Backman, Martin Jakobsson, Catherine Kissel, and Eve Arnold. "Postglacial palaeoceanography in the Skagerrak." Holocene 16, no. 7 (November 2006): 975–85. http://dx.doi.org/10.1177/0959683606hl988rp.

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ROTHWELL, R. G. "NE Atlantic palaeoceanography and climatic change." Journal of the Geological Society 157, no. 3 (May 2000): 641. http://dx.doi.org/10.1144/jgs.157.3.641.

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BERGGREN, W. A. "Deep Sea Data: North Atlantic Palaeoceanography." Science 236, no. 4801 (May 1, 1987): 619–20. http://dx.doi.org/10.1126/science.236.4801.619-a.

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Hald, Morten, Torbjörn Dahlgren, Tor-Eirik Olsen, and Erland Lebesbye. "Late Holocene palaeoceanography in Van Mijenfjorden, Svalbard." Polar Research 20, no. 1 (January 6, 2001): 23–35. http://dx.doi.org/10.3402/polar.v20i1.6497.

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Maryunani, Khoiril Anwar. "Microfossil as proxy for palaeoclimate and palaeoceanography." Berita Sedimentologi 47, no. 3 (December 28, 2021): 77–78. http://dx.doi.org/10.51835/bsed.2021.47.3.363.

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Recent global warming has been addressed due to human activity that causes increased greenhouse gases. However, there are inherent uncertainties in the statement, one of them is the level of natural variability inherent in the climate system. Climate data from measuring instruments are not long enough to evaluate climate variability and current climate evolution. Therefore, we need climate data that has a long back span. To get adequate past climate data, we need natural phenomena which are climate dependent. This natural phenomenon provides a proxy record of the climate. This study of proxy data is the foundation of palaeoclimatology and paleoceanography. Microfossils (i.e., foraminifera, palynomorphs, nannofossils) which in geology are used as a standard tool in biostratigraphy for both age determination and paleoenvironment and correlation, can also be used as a proxy for obtaining paleoclimate and paleoceanography data. Using microfossil as a proxy to study past climate and paleoceanography, we need an understanding of the type of proxy data available and methods used in their analysis.In addition to the dating method (biostratigraphy), there are many climate and oceanography parameters that can be obtained from microfossil proxies such as: sea surface temperature (SST), sea surface salinity, (SST) climate (warm, cold, dry, wet), precipitation, productivity, oxygen content and organic carbon level, deep sea current and ventilation/upwelling, thermocline and mixed layer, variability deep water properties, CCD, bathymetry, sea level change and dissolution. The methods to obtain data fall into some categories e.g., faunal/floral displacement, morphology changes, transfer function/modern analog and isotopic content. Another method that can be used is observing microfossil assemblages and link them to ecological changes associated with climate change and its paleoceanography.A paleoclimate and paleoceanography study using microfossil proxies has been conducted in the Cendrawasih bay, Papua, Indonesia. The study shows that climate in the tropical west Pacific margin (Cendrawasih bay) during Late Pleistocene to Holocene shows high variability. There are nineteen climate changes occurred during Holocene. Early Holocene dated as ca. 11,800-year BP marked by rapid warming with SST differences to last glacial is about 4oC. Early to Middle Holocene (ca. 5960-year BP) marked by increasing temperature up to 2oC, interrupted by cooling at ca. 11230-, 8310- and 7120-years BP. At Middle Holocene temperature decreased rapidly and reached its peak at around ca. 3150-year BP. After cooling at ca. 3150-year BP, temperature increased and then decreased with its peak at ca. 1710-year BP. Since ca. 1710-year BP to Recent, temperature shows warming trend. SST from MAT indicates warming environment near to 1.5oC. The warming trend was interrupted by rapid cooling and warming at ca. 300-year BP. This last warming trend indicates that global warming had started before industrial era and rapid cooling, or warming can occur without anthropogenic gases influence. The typical Holocene climate of warm-wet, dry-cold reverse and become warm-dry, cold-wet during ca. 790-370-year BP and then reversed back to preceding state.Semi-restricted basin occurred since last glacial with anaerobic condition and estuarine circulation system. Warming during interstadial 1e-1a, causing reverse water circulation and basin become sub-aerobic with anti-estuarine circulation. A lot of terrestrial organic matter flow to the bay and increase acidity and carbonate dissolution. High sedimentation found occurred during glacial period especially at the end of glacial period. Rapid warming during late glacial to middle Holocene, rising relative sea level and the bay become more open marine with well oxygenated bottom water and high marine productivity. Warm temperature and deeper thermocline depth (~ 250 m) in west Pacific occurred up to ca. 5960-year BP. Decreasing Sea surface temperature at ca. 5960-year BP and drop of relative sea level causing sub-aerobic condition inside bay. The semi-restricted state with sub-aerobic condition occurred up to Recent.Distribution of Sphaeroidinella group in the tropical west Pacific shows strong correlation with thermocline depth and reflect El Niño frequency event. Early middle Holocene dominated by La Niña-like condition and since Middle Holocene (ca. 5960-year BP) frequent El Niño event began to occur.

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Pados-Dibattista, Teodora, Christof Pearce, Henrieka Detlef, Jørgen Bendtsen, and Marit-Solveig Seidenkrantz. "Holocene palaeoceanography of the Northeast Greenland shelf." Climate of the Past 18, no. 1 (January 20, 2022): 103–27. http://dx.doi.org/10.5194/cp-18-103-2022.

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Abstract. The Northeast Greenland shelf is highly sensitive to climate and ocean variability because it is swept by the East Greenland Current, which, through the western Fram Strait, forms the main pathway of export of sea ice and cold water masses from the Arctic Ocean into the North Atlantic Ocean. In order to reconstruct the variability of the East Greenland Current and general palaeoceanographic conditions in the area during the Holocene, we carried out benthic foraminiferal assemblage, stable isotope, and sedimentological analyses of a marine sediment core retrieved from the Northeast Greenland shelf (core DA17-NG-ST07-73G). The results reveal significant variations in the water masses and thus in the strength of the East Greenland Current over the last ca. 9.4 kyr. Between 9.4 and 8.2 ka the water column off Northeast Greenland was highly stratified, with cold, sea-ice-loaded surface waters and a strong influx of warm Atlantic Water in the subsurface. At ∼ 8.4 ka a short-lived peak in terrestrial elements may be linked to an influx of iceberg-transported sediments and thus to the so-called 8.2 ka event. Conditions similar to those of the Holocene Thermal Maximum prevailed from 8.2 to 6.2 ka, with a strong influence of the Return Atlantic Current and a weakened transport of Polar Water in the upper East Greenland Current. After 6.2 ka we recorded a return to a more stratified water column with sea-ice-loaded surface waters and still Atlantic-sourced subsurface waters. After 4.2 ka increased Polar Water at the surface of the East Greenland Current and a reduction in the Return Atlantic Water at subsurface levels signifies freshening and reduced stratification of the water column and (near) perennial sea-ice cover. The neoglaciation started at 3.2 ka at our location, characterized by a strengthened East Greenland Current. Cold subsurface-water conditions with possible sea-ice cover and minimum surface-water productivity persisted here throughout the last ∼ 3 kyr.

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Dissertations / Theses on the topic "Palaeoceanography"

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Beveridge, Neil Alexander Stewart. "Palaeoceanography of the Eastern Atlantic." Thesis, University of Cambridge, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.337952.

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Grigorov, Ivo. "Southern Ocean palaeoceanography from Thalassiothrix antarctica deposits." Thesis, University of Southampton, 2004. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.413434.

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King, Stephen Charles. "Late Quaternary palaeoceanography of the Peru Margin." Thesis, University of Southampton, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.239459.

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Chepstow-Lusty, Alexander John. "Nannoplankton as indicators of climatic variability in the Upper Pliocene." Thesis, University of Cambridge, 1991. https://www.repository.cam.ac.uk/handle/1810/239128.

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Discoasters are the remains of an enigmatic group of nannoplankton, whose last representatives disappeared globally at 1.89 Ma. The one million years prior to their extinction has been analysed in high time resolution and a global database has been developed from ten sites in the Atlantic, Indian and Pacific Oceans. It has been shown that the variability in Discoaster abundance at low latitudes cannot be attributed solely to changes in sea-surface temperature; discoasters were demonstrated to be suppressed at upwelling sites. In combination with global satellite images of phytoplankton blooms (Lewis, 1989) and maps of modern sea-surface temperatures (CLIMAP, 1981), Discoaster abundance variations were interpreted in terms of the interplay between productivity pressure and sea-surface temperature. Discoasters thrived in the Indian Ocean at Site 709 (4°S) in warm waters with little productivity pressure, whereas Discoaster abundance was suppressed at Sites 677 (l°N) and 662 (l°S) in the Pacific and Atlantic, which although located in warm waters, were affected by upwelling. In addition to the reduced Discoaster abundances associated with upwelling, sea-surface temperature gradients are a significant factor when comparing high and low latitude sites. A marked drop in Discoaster abundance is apparent between 41°N and 56°N (i.e., between Sites 607 and 552). Relative abundances of species in the Discoaster assemblage revealed clearly their contrasting environmental preferences; D. brouweri was produced under a wide range of conditions, favouring warm, low productivity waters; D. asymmetricus and D. tamalis were produced in higher abundances relative to D. brouweri during cooler, low productivity episodes; D. pentaradiatus showed highest absolute abundance in warm, low productivity waters, although increasing in relative abundance at higher latitudes; D. surculus increased in relative abundance in high productivity regions and in cooler waters. At all sites, though most markedly at higher latitudes, Discoaster abundances declined after 2.4 Ma, when glaciation began in the North Atlantic.

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Whiteley, N. J. P. "Investigating of palaeo-circulation in the Southern Atlantic, Southern and Northern Indian Oceans over the last 14Ma using hydrogenetic ferromanganese crusts." Thesis, University of Oxford, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.365325.

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Hart, Stephen Francis. "Palaeoceanography and sedimentology of a mid-Cretaceous Greensand." Thesis, University of Oxford, 1991. http://ora.ox.ac.uk/objects/uuid:ac7da904-aad1-4525-8d11-9c520fc131d3.

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The Upper Albian (mid-Cretaceous) sediments of the Anglo-Paris Basin display a range of condensation phenomena, including glauconitic and phosphoritic sands, glauconitic intraformational pebble beds, and mineralised nodular hardgrounds. These are interpreted as the result of sedimentation rate fluctuations controlled by small-scale relative sea-level changes of at least regional nature. The regional signal was modified by local tectonics, including occasional synsedimentary faulting and the development of thinned successions and complex condensation horizons over broad submarine highs. Candidate sequence boundaries, marine flooding surfaces and systems tracts are proposed. Episodic, high-energy storm events record a spectrum of storm intensities and periodicities in the Upper Greensand Formation. Storm processes interacted with early submarine lithification to produce a suite of pebble-shell beds, simple and amalgamated coquinas, and storm-scoured hardgrounds. Analysis of shell bed fabrics and taphonomy indicates the important role of high-energy storms in generating a distinct event stratigraphy. Stable isotope analysis has detected a positive secular change in carbon-isotopic ratios within carbonates of dispar zone age, resolved as two smaller positive shifts across nodular hardgrounds. This correlates with the development of organic-rich sediments in a range of settings world-wide. Analytical problems, including silica diagenesis, have been addressed by a series of parallel control studies. Geochemical and petrographic analysis has confirmed the widespread development of glauconitic minerals throughout the Upper Greensand, and has been used to investigate grain evolution in a range of lithologies. A review of the global development of the Cretaceous glauconitic facies has been used to compile depositional models for a range of settings. Volumetric calculations of Cretaceous glauconite production rates have shown secular changes, with peak Aptian to Santonian values linked to transgressions across the broad shelf seas which developed globally during this time of rising sea-levels and sea-level highstand.

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Chapman, Mark Robert. "Late Pliocene planktonic foraminifera : palaeoceanography and faunal evolution." Thesis, University of East Anglia, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.332388.

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Sexton, Philip. "Foraminiferal taphonomy, palaeoecology and palaeoceanography of the Eocene." Thesis, University of Southampton, 2005. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.416473.

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Little, Mark G. "Late Quaternary palaeoceanography of the Benguela upwelling system." Thesis, University of Edinburgh, 1997. http://hdl.handle.net/1842/12437.

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Planktonic foraminifera recovered from nine cores in the Benguela Current system are used to ascertain the variability of upwelling intensity for the Late Quaternary and its impact on atmosphere-ocean-cryosphere linkages. The analyses from high-resolution planktonic foraminiferal records for cores GeoB 1706, GeoB 1711 and PG/PC 12, reveal striking variations in upwelling intensity during the last 160,000 years. Four species make up over 95% of the variation within the cores, and enable the record to be divided into episodes characterised by particular planktonic foraminiferal assemblages which have meaningful ecological significance when compared to those of the present-day and the relationship to their environment. The cold-water planktonic foraminifer, Neogloboquadrina pachyderma sinistral [N. pachyderma (s))], dominates the modern-day, coastal upwelling centres, and Neogloboquadrina pachyderma dextral and Globigerina bulloides characterise the fringes of the upwelling cells. Globorotalia inflata is representative of the offshore boundary between newly upwelled waters and the transitional, reduced nutrient levels of the sub-tropical waters. In the fossil record, episodes of high N. pachyderma (s) abundances are interpreted as evidence of increased upwelling intensity and the associated increase in nutrients. The N. pachyderma (s) record suggests rapid shifts in the intensity of upwelling, and corresponding trophic domains, that do not follow the typical glacial - interglacial pattern, but instead reflect the shifts of the Angola-Benguela front situated to the north of the Walvis Ridge. Absence of high abundances of N. pachyderma (s) from the continental slope of the southern Cape Basin indicate that Southern Ocean surface water advection has not exerted a major influence on the Benguela Current system. The periods of high abundance in N. pachyderma (s) are referred to as 'PS events' and indicate increased intensity and zonality of the South Atlantic trade winds controlling the Benguela upwelling system. During these intense upwelling phases, total organic carbon, abundance of N. pachyderma (s) and the benthic/planktonic foraminiferal ratio, provide the best indicators for palaeoproductivity away from coastal re-suspension. The offshore record of GeoB 1711 is used as the indicator for maximum offshore divergence and shelf-edge upwelling and is regarded as the best indicator for palaeoceanographic and palaeoproductivity variability.

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Park, Laura Anne. "Late Quaternary palaeoceanography in Disko Bugt, West Greenland." Thesis, Durham University, 2003. http://etheses.dur.ac.uk/1284/.

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This thesis uses foraminiferal, sedimentological and isotope analysis from three piston cores from different depositional environments in Disko Bugt, West Greenland to understand the nature of the relationship between deglacial activity and palaeo-water mass circulation. It has increased the spatial and temporal resolution of marine multiproxy data in the region through the development of a tight radiocarbon chronology. High resolution sampling has furthered the understanding of modes of Holocene palaeoceanographic irculation in Disko Bugt and West Greenland,a nd linked them to likely operating mechanisms of change. Information about past variations in the strength of the dominant water current in West Greenland (the West Greenland Current - WGC), has been successful through the application of foraminiferal water mass indicator species and isotope techniques. New dating relating to the timing of the final retreat of Jakobshavns Isbrae, the most important ice stream draining the West Greenland Ice Sheet, has been determined through evidence of meltwater and sediment fluxes from the calving margin. The high resolution records produced in this thesis clearly document the rapid instability and subsequent retreat of the ice stream to be related to rapid atmospheric warming following the well-documented "8.2 event". Mid-Holocene climatic changes are recorded in the fjord mouth setting of Kangersuneq. Despite considerable dissolution processes operating in the fjord (which are in fact a product of climatic change themselves), a high resolution record of variable and declining warmth of the WGC is recorded from c. 6.3 ka cal BP, prior to the onset of full Neoglacial conditions around 4.1 ka cal BP. The maximum cooling during the Neoglacial period is clearly seen from c. 3.2 to 2.2 ka cal BP in two cores. A distinct warming of the WGC takes place around 2.2 ka cal BP, which can be linked to an increased component of Irminger Current Water. This is also seen in the records from East Greenland and the Nordic Seas. The foraminiferal assemblagesfr om one of the cores show evidence of a distinct climatic amelioration which is associated with the Medieval Warm Period. There is some evidence for a deterioration of oceanographic conditions which is linked to the onset of the Little Ice Age.

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Books on the topic "Palaeoceanography"

1

Chapman, M. R. Late Pliocene planktonic foraminifera: Palaeoceanography and faunal evolution. Norwich: University of East Anglia, 1992.

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Hooper, P. W. P. Late neogene planktonic foraminifera and palaeoceanography of the North Atlantic. Norwich: University of East Anglia, 1988.

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Swallow, Jane E. Plio-pleistocene palaeoceanography of the Equatorial Indian Ocean: (quantitative and geochemical analyses of planktonic foraminifera from ODP hole 709C). Norwich: University of East Anglia, 1992.

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Walker, Deborah Ann. Carbonates in marine polar sediments: Palaeoceanographic and diagenetic studies. Birmingham: University of Birmingham, 1996.

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North Atlantic Palaeoceanography. Blackwell Science Inc, 1986.

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Pinxian, Wang, and W. A. Berggren, eds. Marine Geology and Palaeoceanography. CRC Press, 2020. http://dx.doi.org/10.1201/9780429070884.

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S, Kemp A. E., Geological Society of London, and IGCP 374, eds. Palaeoclimatology and palaeoceanography from laminated sediments. London: Geological Society, 1996.

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Kemp, Anthony E. Palaeoclimatology and Palaeoceanography from Laminated Sediments. Geological Society of London, 1996.

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Late Quaternary Palaeoceanography of the North Atlantic Margins. Geological Society of London, 1996.

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A, Scrutton R., and Geological Society of London, eds. The tectonics, sedimentation, and palaeoceanography of the North Atlantic Region. London: The Geological Society, 1995.

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Book chapters on the topic "Palaeoceanography"

1

Sijinkumar, A. V., B. Nagender Nath, and Pavan Miriyala. "Late Quaternary Chronostratigraphy, Carbonate Mass Accumulation Rates and Palaeoceanography of the Andaman Sea." In Society of Earth Scientists Series, 289–313. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-39843-9_14.

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Kuhnt, Wolfgang, Ann E. Holbourn, Janika Jöhnck, and Julia Lübbers. "Miocene to Pleistocene Palaeoceanography of the Andaman Region: Evolution of the Indian Monsoon on a Warmer-Than-Present Earth." In Society of Earth Scientists Series, 261–88. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-39843-9_13.

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Volbers, A. N. A., H. S. Niebler, J. Giraudeau, H. Schmidt, and R. Henrich. "Palaeoceanographic Changes in the Northern Benguela Upwelling System over the last 245.000 Years as Derived from Planktic Foraminifera Assemblages." In The South Atlantic in the Late Quaternary, 601–22. Berlin, Heidelberg: Springer Berlin Heidelberg, 2003. http://dx.doi.org/10.1007/978-3-642-18917-3_26.

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Houghton, Simon D. "Recent Coccolith Sedimentation Patterns and Transport in the North Sea: Implications for Palaeoceanographic Studies of Marginal and Continental Shelf Seas." In Applied Micropalaeontology, 1–39. Dordrecht: Springer Netherlands, 1993. http://dx.doi.org/10.1007/978-94-017-0763-3_1.

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Francesca, Lozar, Violanti Donata, Bernardi Elisa, Dela Pierre Francesco, and Natalicchio Marcello. "Calcareous Microfossils as Tracers of Major Palaeoceanographic Perturbations: The Case of the Onset of the Messinian Salinity Crisis in the Tertiary Piedmont Basin (Northwestern Italy)." In Springer Geology, 1123–27. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_215.

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Pascual, Ana, Alejandro Cearreta, Julio Rodríguez-Lázaro, and Adolfo Uriarte. "Geology and Palaeoceanography." In Elsevier Oceanography Series, 53–73. Elsevier, 2004. http://dx.doi.org/10.1016/s0422-9894(04)80041-2.

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Kinoshita, Hajimu, Yukari Nakasa, Liu Zaoshu, and Xia Kanyuan. "Geophysical Survey in the South China Sea with a Special Focus on the Backarc Basin Formation." In Marine Geology and Palaeoceanography, 1–32. CRC Press, 2020. http://dx.doi.org/10.1201/9780429070884-1.

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Li, Jiabiao. "The Rifting and Collison of The South China Sea Terrain System." In Marine Geology and Palaeoceanography, 33–46. CRC Press, 2020. http://dx.doi.org/10.1201/9780429070884-2.

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Jin, Xianglong. "The Evolution of Marginal Seas off China." In Marine Geology and Palaeoceanography, 47–56. CRC Press, 2020. http://dx.doi.org/10.1201/9780429070884-3.

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Wei, Wuchang, and Alyssa Peleo-Alampay. "Onset of North Atlantic Deep Water 11.5 million years ago triggered by climate cooling." In Marine Geology and Palaeoceanography, 57–64. CRC Press, 2020. http://dx.doi.org/10.1201/9780429070884-4.

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Conference papers on the topic "Palaeoceanography"

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Kershaw, James, Laura Robinson, Joseph Stewart, Ana Samperiz, and Ivo Strawson. "Ba/Ca ratios of stylasterid coral skeletons: implications for palaeoceanography and coral biomineralisation." In Goldschmidt2021. France: European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.4459.

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Ownsworth, Emma, David Selby, and Jeremy Lloyd. "MILLENNIAL-SCALE GLACIAL PALAEOCEANOGRAPHY OF WEST GREENLAND: GEOCHEMICAL TRACKING OF ICE SHEET BREAKUP, ADVANCE AND RETREAT." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-319121.

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Balota, Eseroghene J., Martin J. Head, and Makoto Okada. "WESTERN PACIFIC PALAEOCEANOGRAPHY ACROSS THE EARLY–MIDDLE PLEISTOCENE BOUNDARY (~773 KA): DINOFLAGELLATE CYSTS OF THE CHIBA COMPOSITE SECTION, JAPAN. KEYWORDS: PALEOCEANOGRAPHY, DINOFLAGELLATES, PLEISTOCENE, JAPAN, MIS 19." In Joint 52nd Northeastern Annual Section and 51st North-Central Annual GSA Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017ne-291298.

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Peral, Marion, Franck Bassinot, Mathieu Daëron, Dominique Blamart, William Gray, Jérôme Bonnin, Frans Jorissen, et al. "The contribution of the foraminiferal Mg/Ca ratio, clumped and conventional stable isotope paleothermometers combination for palaeoceanographic studies." In Goldschmidt2021. France: European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.6146.

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