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Relevant bibliographies by topics / Late

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Academic literature on the topic 'Late'

Author: Grafiati

Published: 4 June 2021

Last updated: 15 June 2025

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Journal articles on the topic "Late"

1

Zevenbergen, Chantal, Marcel E. Meima, Elaine C. Lima de Souza, et al. "Transport of Iodothyronines by Human L-Type Amino Acid Transporters." Endocrinology 156, no. 11 (2015): 4345–55. http://dx.doi.org/10.1210/en.2015-1140.

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Thyroid hormone (TH) transporters facilitate cellular TH influx and efflux, which is paramount for normal physiology. The L-type amino acid transporters LAT1 and LAT2 are known to facilitate TH transport. However, the role of LAT3, LAT4, and LAT5 is still unclear. Therefore, the aim of this study was to further characterize TH transport by LAT1 and LAT2 and to explore possible TH transport by LAT3, LAT4, and LAT5. FLAG-LAT1–5 constructs were transiently expressed in COS1 cells. LAT1 and LAT2 were cotransfected with the CD98 heavy chain. Cellular transport was measured using 10 nM 125I-labeled T4, T3, rT3, 3,3′-T2, and 10 μM [125I]3′-iodotyrosine (MIT) as substrates. Intracellular metabolism of these substrates was determined in cells cotransfected with either of the LATs with type 1 or type 3 deiodinase. LAT1 facilitated cellular uptake of all substrates and LAT2 showed a net uptake of T3, 3,3′-T2, and MIT. Expression of LAT3 or LAT4 did not affect transport of T4 and T3 but resulted in the decreased cellular accumulation of 3,3′-T2 and MIT. LAT5 did not facilitate the transport of any substrate. Cotransfection with LAT3 or LAT4 strongly diminished the cellular accumulation of 3,3′-T2 and MIT by LAT1 and LAT2. These data were confirmed by metabolism studies. LAT1 and LAT2 show distinct preferences for the uptake of the different iodocompounds, whereas LAT3 and LAT4 specifically facilitate the 3,3′-T2 and MIT efflux. Together our findings suggest that different sets of transporters with specific influx or efflux capacities may cooperate to regulate the cellular thyroid state.

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Bos, Z. "The Late November Lake." Literary Imagination 12, no. 1 (2009): 90–91. http://dx.doi.org/10.1093/litimag/imp070.

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Briggs, Richard W., Steven G. Wesnousky, and Kenneth D. Adams. "Late Pleistocene and Late Holocene Lake Highstands in the Pyramid Lake Subbasin of Lake Lahontan, Nevada, USA." Quaternary Research 64, no. 2 (2005): 257–63. http://dx.doi.org/10.1016/j.yqres.2005.02.011.

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AbstractShoreline geomorphology, shoreline stratigraphy, and radiocarbon dates of organic material incorporated in constructional beach ridges record large lakes during the late Pleistocene and late Holocene in the Pyramid Lake subbasin of Lake Lahontan, Nevada, USA. During the late Holocene, a transgression began at or after 3595 ± 35 14C yr B.P. and continued, perhaps in pulses, through 2635 ± 40 14C yr B.P., resulting in a lake as high as 1199 m. During the latest Pleistocene and overlapping with the earliest part of the Younger Dryas interval, a lake stood at approximately 1212 m at 10,820 ± 35 14C yr B.P. and a geomorphically and stratigraphically distinct suite of constructional shorelines associated with this lake can be traced to 1230 m. These two lake highstands correspond to periods of elevated regional wetness in the western Basin and Range that are not clearly represented in existing northern Sierra Nevada climate proxy records.

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Bosanquet, D. C., S. Vaughan, and B. M. Stephenson. "Late mesh sepsis: how late is late?" Hernia 19, no. 6 (2015): 1035–36. http://dx.doi.org/10.1007/s10029-015-1364-7.

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Mäusbacher, R., K. van den Borg, G. Daut, E. Kroemer, J. Müller, and J. Wallner. "Late Pleistocene and Holocene environmental changes in NW Spitsbergen - evidence from lake sediments." Zeitschrift für Geomorphologie 46, no. 4 (2002): 417–39. http://dx.doi.org/10.1127/zfg/46/2002/417.

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Mellen, Joan. "Late Ozu, Late Naruse." Film Quarterly 61, no. 4 (2008): 24–32. http://dx.doi.org/10.1525/fq.2008.61.4.24.

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Abstract This essay reflects on the shared qualities of the late works of Yasujiro Ozu and Mikio Naruse. Both worked in the shomin-geki genre of middle-class life, depicting the often unhappy social conditions, notably among women, in post-war Japan. But while Ozu is tender and pitying, Naruse is agonized and outraged at injustice.

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Shaw, P. A., and D. S. G. Thomas. "Lake Caprivi: A late Quaternary link between the Zambezi and middle Kalahari drainage systems." Zeitschrift für Geomorphologie 32, no. 3 (1988): 329–37. http://dx.doi.org/10.1127/zfg/32/1988/329.

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Barrows, Timothy T., Kathryn E. Fitzsimmons, Stephanie C. Mills, Jacqui Tumney, Daryl Pappin, and Nicola Stern. "Late Pleistocene lake level history of Lake Mungo, Australia." Quaternary Science Reviews 238 (June 2020): 106338. http://dx.doi.org/10.1016/j.quascirev.2020.106338.

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Konno, Michiko. "Stay Away from Dementias: Too Late or Not Too Late." Journal of Nihon University Medical Association 74, no. 3 (2015): 129–33. http://dx.doi.org/10.4264/numa.74.129.

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Raju, Tonse N. K. "The “Late Preterm” Birth—Ten Years Later." Pediatrics 139, no. 3 (2017): e20163331. http://dx.doi.org/10.1542/peds.2016-3331.

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Dissertations / Theses on the topic "Late"

1

Sapota, Tomasz. "Late Cenozoic Geoarchives from Lake Baikal, Siberia." Doctoral thesis, Uppsala University, Department of Earth Sciences, 2004. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-4552.

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<p>Three long sediment cores (BDP-98 – 600 m, BDP-96 – 200 m and BDP-93 – 100 m) drilled in Lake Baikal (Siberia) have been studied with the aims of establishing an absolute chronology and reconstructing paleoclimatic and paleoenvironmental changes in the region. The location of the lake at relatively high latitude and continental interior and a thick continuous sedimentary archive that developed in a rift system tectonic setting provide unique material for this investigation. The cosmogenic isotope <sup>10</sup>Be was used for dating and the results indicate time spans of 8 (+0.8\-0.6) Myr for BDP-98, 5.5 (±0.13) Myr for BDP-96 and >0.7 Myr for BDP-93. Two major sedimentary facies (deltaic and hemipelagic) are distinguished by textural geochemical and mineralogical data. Detrital mineral composition suggests negligible change in provenance during the period studied. Formation of authigenic minerals, such as framboidal pyrite, vivianite and siderite, reflects variable environmental conditions in the lake and climate change in the region. Biogenic silica content shows climatic influence, which is modified by the supply of detrital material and postdepositional alterations. <sup>10</sup>Be dating, combined with lithological analysis of the sediments, makes it possible to place temporal constrains on climate cooling at the Miocene/Pliocene boundary (5 Myr ago) and at the Early/Late Pliocene boundary (3.6 Myr ago) as well as the beginning of the northern hemisphere glaciation at about 2.5–2.6 Myr ago. The regional east-west tectonic extension of south-east Asia, related to Tibetan Plateau uplift, was confined in the Baikal area to between about 7 and 5 Myr ago, with a rifting rate calculated at 7 mm year<sup>-1</sup>. Furthermore, the <sup>10</sup>Be data suggest that geomagnetic field intensity strengthened around the Miocene/Pliocene boundary.</p>

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Lacey, Jack H. "Late Quaternary palaeoenvironmental reconstruction from Lake Ohrid." Thesis, University of Nottingham, 2016. http://eprints.nottingham.ac.uk/31993/.

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Lake Ohrid is a large, deep, ancient lake located on the Balkan Peninsula and has an extraordinary degree of endemic biodiversity. A deep drilling campaign was carried out in 2013 as part of the Scientific Collaboration on Past Speciation Conditions in Lake Ohrid (SCOPSCO) project to better understand the influence of climate and environmental change on evolutionary patterns and endemism. Initial results from a 569 m sediment succession drilled in the centre of the basin indicate continuous lacustrine conditions over the past ca. 1.2 Ma. This thesis presents new stable isotope data from carbonate within the upper 248 m of the composite profile, covering the last ca. 640 ka at a millennial-scale resolution (≈ 0.5 ka). Isotope data are used to provide a long-term palaeoenvironmental reconstruction, which is supported by a quantitative model of modern lake water isotope composition and a detailed multi-proxy investigation of climate evolution since the last glacial period. Water balance calculations confirm Ohrid to be an evaporative system with a complex hydrology. Variations in the isotope composition of modern lake water are suggested to represent long-term fluctuations in water balance. A trend from wetter to drier conditions through the Holocene is consistent with regional and hemispheric processes related to changes in insolation. Over the last ca. 640 ka, endogenic calcite is precipitated in abundance during warm stages, however carbonate is negligible during glacial periods with the exception of discrete horizons comprising early diagenetic authigenic siderite. The oxygen isotope composition of lake water, calculated using calcite and siderite, indicates more evaporated conditions during warm stages and fresher lake water in glacial phases. Low frequency variability shown by calcite isotope data suggests relatively stable conditions before ca. 450 ka, a transition to a wetter climate between ca. 400-250 ka, and a trend to drier climate conditions after ca. 250 ka. Higher frequency millennial-scale oscillations and abrupt climate events observed during warm stages are likely associated with regional climate change as a function of orbital forcing. This study emphasises the potential of Lake Ohrid as a valuable archive of climate change in the central Mediterranean region and demonstrates the efficacy of isotope data for palaeoenvironmental reconstruction at Lake Ohrid.

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Olago, Daniel Ochieng. "Late Quaternary lake sediments of Mount Kenya, Kenya." Thesis, University of Oxford, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.296036.

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Griffiths, S. J. "Late Quaternary palaeoclimatology of Lake Kopais, central Greece." Thesis, Swansea University, 2001. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.507951.

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Schnellmann, Michael P. Schnellmann Michael P. "Late quaternary mass movements in a perialpine lake (Lake Lucerne, Switzerland) /." [S.l.] : [s.n.], 2004. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=15533.

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Woodbridge, Jessie. "Late-Holocene lake diatom-inferred palaeoclimate from central Tturkey." Thesis, University of Plymouth, 2009. http://hdl.handle.net/10026.1/1308.

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In the semi-arid environment of the Eastern Mediterranean, water can be a limiting resource and its availability is influenced by different climate factors. Knowledge of late Holocene water balance is limited for this region. Lake systems and organisms respond to environmental variability and can be used as a proxy for palaeoclimate. The aims of this research project were to reconstruct late Holocene palaeoclimate using diatom frustules preserved within crater lake sediments in central Turkey. Two lakes (Nar Gölü and Kratergöl), located in the same climate region, were selected for this purpose. Modem lake samples and sediment cores collected between 1999-2006 were subsampled at high resolution for diatom analysis, Nar G610 provided an uninterrupted annually-laminated late Holocene sequence covering the last 1720 years. The varied lake sedimentation rate of Kratergöl was evident in sediment core coarse sandy sections and the sequence was thought to represent the mid-late 20`h century. A diatom-salinity transfer function was employed using existing training sets from the European Diatom Database to infer past water balance. The reconstruction was calibrated with instrumental meteorological data. Reconstructed salinity was limited by poor analogue matching between the palaeo-diatom assemblage and the modem training set. This was partly associated with the presence of a previously undescribed diatom genus (newly named Clipeoparvus anatolicus), which was highly abundant in the Nar modern environment and sediment record. Additional methods to extract palaeoenvironmental information from the diatom record were explored. This included calibrating diatom DCA axes with instrumental temperature in order to reconstruct palaeo-temperature, identifying mono-specific diatom bloom events in situ on core thin section slides, calculating diatom biovolume, concentration, diversity and grouping species according to their habitat preferences. Comparison of the Nar and Kratergöl records highlighted the advantages of annually laminated lake sediments for palaeoenvironmental research and the limitations of sediment sequences from lakes with a varied sedimentation rate and poor chronological control. The primary meteorological control on the Nar diatom population was identified as summer temperature, via the link with lake water salinity. The Nar diatom sequence was compared with an oxygen isotope (palaeo-evaporation) and pollen record (human land use) from the same sediment cores and palaeoclimate reconstructions from other sites and regions. Nar diatoms and oxygen isotopes revealed that Cappadocia experienced high aridity prior to AD 540 and mono-specific diatom bloom events have become increasingly common during the most recent -400 years. A diatom assemblage shift at AD 2001 also indicated a recent change in the system. Human land use evident in the pollen sequence may have influenced the diatom relationship with climatic variability in the later part of the record. The Kratergöl diatom record indicated environmental variability throughout the mid-late 20`h century; however, interpretations were limited due to chronological discrepancies. The annually laminated Nar diatom record has provided a detailed account of palaeoenvironmental variability in central Anatolia throughout the late Holocene and contributes towards our understanding of Eastern Mediterranean palaeoclimate.

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Meisenzahl, Anne Marie. "It's late." Tallahassee, Florida : Florida State University, 2009. http://etd.lib.fsu.edu/theses/available/etd-11052009-125626/.

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Thesis (M.A.)--Florida State University, 2009.<br>Advisors: Barbara Hamby and David Kirby, Florida State University, College of Arts and Sciences, Dept. of English. Title and description from dissertation home page (viewed on May 5, 2010). Document formatted into pages; contains vii, 50 pages.

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Nobles, Allyson M. "Late Bloomer." ScholarWorks@UNO, 2017. https://scholarworks.uno.edu/td/2427.

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Metcalfe, Elisabet Joan. "Late-glacial through Holocene Stratigraphy and Lake-level Record of Rangely Lake, Western Maine." Fogler Library, University of Maine, 2007. http://www.library.umaine.edu/theses/pdf/MetcalfeEJ2007.pdf.

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Lacourse, Terri. "Late Quaternary vegetation history of Sulphur Lake, southwest Yukon Territory, Canada." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1998. http://www.collectionscanada.ca/obj/s4/f2/dsk2/tape15/PQDD_0005/MQ36711.pdf.

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Books on the topic "Late"

1

O'Connor, Jane. Fancy Nancy and the late, late, late night. HarperFestival, 2010.

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Suárez, Patricia. Late. Alción, 2003.

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Carter, Alan. Late. RosaBooks, 1985.

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Michael, Hamburger. Late. Anvil Press Poetry, 1997.

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Mitchell, Gladys. Late, late in the evening. Chivers/Thorndike, 2004.

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Kelman, James. How late it was, how late. W.W. Norton & Co., 1995.

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Kelman, James. How late it was, how late. Delta, 1996.

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Hocks, Teun. Het late uur =: The late hour. De Geus, 1999.

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Kelman, James. How late it was, how late. Norton, 2005, c1994., 2005.

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How late it was, how late. Minerva, 1994.

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Book chapters on the topic "Late"

1

Ziegler, Peter A. "Late Early And Late Permian." In Evolution of Laurussia. Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-0469-9_9.

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Colarusso, Calvin A. "Late and Late Late Adulthood (Age 60 and beyond)." In Child and Adult Development. Springer US, 1992. http://dx.doi.org/10.1007/978-1-4757-9673-5_12.

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Christie, Neil. "Late Roman and Late Antique Italy." In A Companion to Roman Italy. John Wiley & Sons, Ltd, 2016. http://dx.doi.org/10.1002/9781118993125.ch8.

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Morbidelli, Alessandro, and Bernard J. Wood. "Late Accretion and the Late Veneer." In The Early Earth. John Wiley & Sons, Inc, 2015. http://dx.doi.org/10.1002/9781118860359.ch4.

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Eeg-Olofsson, Karin Edebol. "Late Responses." In Pediatric Electromyography. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-61361-1_7.

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Eldridge, C. C. "‘Too Late’." In The Imperial Experience. Macmillan Education UK, 1996. http://dx.doi.org/10.1007/978-1-349-24950-3_8.

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Ziegler, Peter A. "Late Devonian." In Evolution of Laurussia. Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-0469-9_5.

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Ziegler, Peter A. "Late Carboniferous." In Evolution of Laurussia. Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-0469-9_7.

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Bienenfeld, David. "Late Life." In Psychiatry. John Wiley & Sons, Ltd, 2008. http://dx.doi.org/10.1002/9780470515167.ch13.

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van Merkesteyn, J. P. R. "Late radiatieschade." In Praktijkboek tandheelkunde. Bohn Stafleu van Loghum, 2008. http://dx.doi.org/10.1007/978-90-313-7318-5_42.

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Conference papers on the topic "Late"

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Steele, Jack Cowan, and William H. Amidon. "LATE PLEISTOCENE CHRONOLOGY OF LAKE TERRETON, SOUTHEASTERN IDAHO." In 51st Annual Northeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016ne-272806.

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"Late contributions." In 2016 IEEE International Conference on Industrial Technology (ICIT). IEEE, 2016. http://dx.doi.org/10.1109/icit.2016.7475102.

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"Late Contributions." In 2018 IEEE 27th International Symposium on Industrial Electronics (ISIE). IEEE, 2018. http://dx.doi.org/10.1109/isie.2018.8433810.

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Tretz, Christophe. "Late News." In 2006 IEEE international SOI. IEEE, 2006. http://dx.doi.org/10.1109/soi.2006.284483.

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"Late News." In 2006 IEEE international SOI Conferencee Proceedings. IEEE, 2006. http://dx.doi.org/10.1109/soi.2006.284484.

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Sethumadhavan, Simha, Franziska Roesner, Joel S. Emer, Doug Burger, and Stephen W. Keckler. "Late-binding." In the 34th annual international symposium. ACM Press, 2007. http://dx.doi.org/10.1145/1250662.1250705.

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"Late Paper." In 2019 14th International Conference on Advanced Technologies, Systems and Services in Telecommunications (TELSIKS). IEEE, 2019. http://dx.doi.org/10.1109/telsiks46999.2019.9002363.

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Arto Rantala, Matti Sopanen, and Markku Aberg. "Late news." In 2004 International Semiconductor Conference. CAS 2004 Proceedings. IEEE, 2004. http://dx.doi.org/10.1109/smicnd.2004.1403059.

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"Late papers." In 1985 IEEE Power Electronics Specialists Conference (ESA SP-230). IEEE, 1985. http://dx.doi.org/10.1109/pesc-esasp.1985.7069807.

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"Late Papers." In Proceedings of the 2006 IEEE Sensors Applications Symposium, 2006. IEEE, 2006. http://dx.doi.org/10.1109/sas.2006.1634274.

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Reports on the topic "Late"

1

Richmond, K. A., and L. G. Goldsborough. Late Holocene paleolimnology of Killarney Lake, Manitoba. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1999. http://dx.doi.org/10.4095/211113.

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Vilks, G., B. Deonarine, and G. Winters. Late Quaternary marine geology of Lake Melville, Labrador. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/122409.

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Lewis, C. F. M., and B. J. Todd. Sediments and Late Quaternary history of Lake Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1995. http://dx.doi.org/10.4095/205054.

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Brooks, G. R., and A. Grenier. Late Holocene pollen stratigraphy of Lake Louise, Manitoba. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2001. http://dx.doi.org/10.4095/212115.

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Morrissey, M. F. Late Washing efficiency. Office of Scientific and Technical Information (OSTI), 1992. http://dx.doi.org/10.2172/6678480.

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Bisin, Alberto, and Andrea Moro. LATE for History. National Bureau of Economic Research, 2020. http://dx.doi.org/10.3386/w28113.

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Morrissey, M. F. Late Washing efficiency. Office of Scientific and Technical Information (OSTI), 1992. http://dx.doi.org/10.2172/10124866.

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Kersh, Steve. Late March 2020 Tornadic Thunderstorm. Office of Scientific and Technical Information (OSTI), 2020. http://dx.doi.org/10.2172/1777919.

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Blandhol, Christine, John Bonney, Magne Mogstad, and Alexander Torgovitsky. When is TSLS Actually LATE? National Bureau of Economic Research, 2022. http://dx.doi.org/10.3386/w29709.

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Brooks, M. J., and G. T. Hanson. Late Archaic-Late Woodland adaptive stability and change in the Steel Creek watershed, South Carolina: Final report of the L-Lake prehistoric investigations. Office of Scientific and Technical Information (OSTI), 1989. http://dx.doi.org/10.2172/6298550.

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