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Статті в журналах з теми "Icehouse"
Porter, Joe Ashby. "Fiction: Icehouse Burgess." Yale Review 88, no. 3 (July 2000): 101–10. http://dx.doi.org/10.1111/0044-0124.00419.
Повний текст джерелаThomas, Ellen. "Descent into the Icehouse." Geology 36, no. 2 (2008): 191. http://dx.doi.org/10.1130/focus022008.1.
Повний текст джерелаPekar, Stephen F. "When did the icehouse cometh?" Nature 455, no. 7213 (October 2008): 602–3. http://dx.doi.org/10.1038/455602a.
Повний текст джерелаMontañez, Isabel Patricia. "Current synthesis of the penultimate icehouse and its imprint on the Upper Devonian through Permian stratigraphic record." Geological Society, London, Special Publications 512, no. 1 (September 29, 2021): 213–45. http://dx.doi.org/10.1144/sp512-2021-124.
Повний текст джерелаBurgess, Peter M., Jinyu Zhang, and Ronald Steel. "Narrow is normal: Exploring the extent and significance of flooded marine shelves in icehouse, transitional, and greenhouse climate settings." Geology 50, no. 4 (January 18, 2022): 496–99. http://dx.doi.org/10.1130/g49468.1.
Повний текст джерелаAlgeo, T. J., P. A. Meyers, R. S. Robinson, H. Rowe, and G. Q. Jiang. "Icehouse–greenhouse variations in marine denitrification." Biogeosciences 11, no. 4 (February 27, 2014): 1273–95. http://dx.doi.org/10.5194/bg-11-1273-2014.
Повний текст джерелаAlgeo, T. J., P. A. Meyers, R. S. Robinson, H. Rowe, and G. Q. Jiang. "Icehouse-greenhouse variations in marine denitrification." Biogeosciences Discussions 10, no. 9 (September 6, 2013): 14769–813. http://dx.doi.org/10.5194/bgd-10-14769-2013.
Повний текст джерелаMcKenzie, N. Ryan, and Hehe Jiang. "Earth's Outgassing and Climatic Transitions: The Slow Burn Towards Environmental “Catastrophes”?" Elements 15, no. 5 (October 1, 2019): 325–30. http://dx.doi.org/10.2138/gselements.15.5.325.
Повний текст джерелаSteinhauff, D. Mark, Abduljaleel Abubshait, and Sam J. Purkis. "Red Sea Holocene carbonates: Windward platform margin and lagoon near Al-Wajh, northern Saudi Arabia." Journal of Sedimentary Research 91, no. 8 (August 19, 2021): 847–75. http://dx.doi.org/10.2110/jsr.2021.04.
Повний текст джерелаKvale, Karin F., Katherine E. Turner, Angela Landolfi, and Katrin J. Meissner. "Phytoplankton calcifiers control nitrate cycling and the pace of transition in warming icehouse and cooling greenhouse climates." Biogeosciences 16, no. 5 (March 14, 2019): 1019–34. http://dx.doi.org/10.5194/bg-16-1019-2019.
Повний текст джерелаДисертації з теми "Icehouse"
van, Mourik Caroline A. "The Greenhouse - Icehouse Transition : a dinoflagellate perspective." Doctoral thesis, Stockholm University, Department of Geology and Geochemistry, 2006. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-1073.
Повний текст джерелаThrough the analysis of the stratigraphic and spatial distribution of organic walled dinoflagellate cysts (dinocysts) from climatologically and oceanographically key sites, this project aims to contribute to a better understanding of the Eocene-Oligocene (E/O) environmental changes and their timing. A central issue is to identify the global environmental changes which are responsible for the Eocene cooling and its underlying mechanisms with the focus on the Oligocene isotope-1 (Oi-1) event, thought to mark the onset of major Antarctic glaciation.
Two low-latitude sites were selected, Blake Nose (western North Atlantic) and Massignano (central Italy). For the first time a coherent taxonomy and biostratigraphy of dinocysts was established for the late Eocene at these latitudes. A high resolution correlation was established between the Massignano E/O Stratotype Section and the stratigraphically more extended ‘Massicore’. The composite section was used to analyse sea surface temperature (SST) change across the greenhouse-icehouse transition by means of dinocyst distribution.
At Massignano, the Oi-1 event was recognised both qualitatively and quantitatively. In the power spectrum of the SSTdino the ~100 and ~400 kyr eccentricity cycles may be distinguished and correlated with La04. When orbitally tuned, the E/O GSSP dates ~100 kyr older than the Oi-1 event. The boundary’s age could either be ~33.75 or ~34.1 Ma, both differ significantly from the ~33.9 Ma age in the GTS 2004.
Furthermore, when the data from the low-latitude sites were combined with extensive datasets from the Proto North Atlantic and adjacent regions, a suite of species sensitive to changes in SST was recognised. Their first and last occurrences reflect seven distinct phases of decreasing SSTs during the Middle Eocene to earliest Oligocene.
These results clearly indicate that atmospheric cooling together with higher frequency orbital forcing played a key role in the transition from the Greenhouse to the Icehouse world.
Van, Mourik Caroline A. "The greenhouse - icehouse transition : a dinoflagellate perspective /." Stockholm : Department of Geology and Geochemistry, Stockholm University, 2006. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-1073.
Повний текст джерелаForsythe, G. T. W. "Construction and ecology of icehouse algal reefs." Thesis, University of Cambridge, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.599129.
Повний текст джерелаPaterson, Richard James. "Carbonate diagenesis and sedimentology in an icehouse world." Thesis, University of Bristol, 2007. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.492466.
Повний текст джерелаSpringate, Megan Elizabeth. "Keeping it cool, investigations around the Benares icehouse, Mississauga, Ontario." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1997. http://www.collectionscanada.ca/obj/s4/f2/dsk3/ftp04/mq21703.pdf.
Повний текст джерелаCanile, Fernanda Maciel. "Evidências geológicas de mudanças climáticas (greenhouse-icehouse) na Antártica Ocidental durante a passagem Eoceno-Oligoceno." Universidade de São Paulo, 2010. http://www.teses.usp.br/teses/disponiveis/44/44141/tde-08012011-203025/.
Повний текст джерелаDuring the Eocene and Oligocene (55 23 Ma) the Earth was undergoing a period of great climatic changes. Geological records, reinforced by climate models indicate that global climate during this period went from a stage in which the Earth was virtually free of polar ice caps to a stage close to what we find today in Antarctica. Most of these records are indirect, taken from the deep-sea cores or fossil material. Clear terrestrial evidence of climate change (greenhouse-icehouse) for the Eocene-Oligocene transition is found in Wesele Cove, King George Island, West Antarctica. This evidence includes a succession of at least thirteen, few meters thick, basaltic lava flows overlain disconformably by diamictite and sandstone. The basaltic section is correlated with the Mazurek Point/Hennequin Formation, radiometric dated as Eocene, and the diamictite and sandstone correspond to the Krakowiak Glacier Member of the Polonez Cove Formation, dated as Early Oligocene, on paleontological and radiometric basis. Each tholeiitic basalt layer exhibits a lower, thicker (1 to few meters) fresh zone, transitionally followed up by a zone of saprolith, varying from decimeters to 1-1.5 m in thickness. The entire basalt package of around 60 m, is tilted 25º to the east. The succession has been recently exposed due to fast retreat of the present Wyspianski Glacier. The initial field evidence suggests that the succession represents the geological record of paleoclimatic variation from mild to glacial conditions, that could correlate with the change from the late Eocene optimum climatic (greenhouse) to icehouse conditions in the Oligocene, as recorded on the Cenozoic paleotemperature curve established by 18O determinations on calcareous foram tests. This study had focus on the stratigraphy and geochemistry analysis of the occurrence, in order to interpret the succession of palaeoclimatic events documented in outcrop and analyze them in the context of paleoclimatic history of Antarctica. Data obtained consistently showed that the supposed transition from unaltered to altered zones observed in each basalt layer may in fact be assigned to the moderated action of weathering processes on top of each flow. They also demonstrate a glacial, in partly subglacial with marine contribution, origin for the overlying diamictites, which has features such clasts of diverse lithologies and sizes, faceted and striated clasts, bullet shaped clasts, clasts broken by freezing and thaw, intraformational striae and marine fossils found in the matrix of the diamictite. The mild paleoclimatic conditions responsible for weathering of the basalt lasted until the emplacement of the highest lava horizon, followed by tectonic movement that tilted the package. These events indicate a relatively long paleoclimatic mild conditions during the Eocene, preceding the establishment and displacement of the Oligocene ice-sheet in this part of Antarctica.
Via, Rachael Kathleen. "Evolution of Atlantic deep-water circulation: from the greenhouse to the icehouse." Texas A&M University, 2005. http://hdl.handle.net/1969.1/2609.
Повний текст джерелаKeech, Andrew R. "Chemical weathering in an icehouse world : the record from soils and lakes." Thesis, University of Bristol, 2011. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.556963.
Повний текст джерелаNewsam, C. "Calcareous nannoplankton evolution and the Paleogene greenhouse to icehouse climate-mode transition." Thesis, University College London (University of London), 2017. http://discovery.ucl.ac.uk/1541282/.
Повний текст джерелаTremblin, Maxime. "Contraindre la transition greenhouse-icehouse du Paléogène par la géochimie des coccolithes." Electronic Thesis or Diss., Sorbonne université, 2018. https://accesdistant.sorbonne-universite.fr/login?url=https://theses-intra.sorbonne-universite.fr/2018SORUS450.pdf.
Повний текст джерелаAmong the major obstacles in constraining paleoclimates for periods of “greenhouse” type is the poor preservation state of the sedimentary archive, and the existence of limits for each of the different applied geochemical markers. These obstacles lead to great uncertainties on the values and distribution of sea surface temperatures (SSTs) and atmospheric CO2 concentrations. Therefore, the mechanisms that brought the Earth’s system from a “greenhouse” to an “icehouse” regime throughout the Paleogene are not well constrained. In this thesis, we reconstructed the thermal evolution of the superficial ocean and the evolution of atmospheric pCO2 during the Paleogene from the isotopic signal (δ18O and ∆13C) of the fossilized carbonate exoskeleton of coccolithophores: coccoliths. Our data reveal a global cooling of surface waters from the Early to the Middle Eocene. During the Late Eocene and across the Eocene-Oligocene transition, values for pCO2 decrease, and cooling at high latitudes continues, allowing for the set up of an ice sheet in Antarctic, while the tropical belt warms. This change in the distribution of heat fluxes at the Earth’s surface during this period is synchronous to the deepening of the Drake Passage and to the set up of a vigorous Antarctic Circumpolar Current. These results thus highlight the driving role of changing oceanic circulations for climate dynamics during this transition. This thesis also proves the existence of important latitudinal thermal gradients throughout the Paleogene. The hypothesis of a homogeneous distribution of SSTs between the Equator and the poles, which prevails in the literature but remains hard to modelise, can thus be rejected
Книги з теми "Icehouse"
Yolen, Jane. Welcome to the icehouse. New York: Putnam, 1998.
Знайти повний текст джерела1959-, Koeberl Christian, and Montanari Alessandro, eds. The late Eocene Earth: Hothouse, icehouse, and impacts. Boulder, Colo: Geological Society of America, 2009.
Знайти повний текст джерелаname, No. From greenhouse to icehouse: The marine Eocene-Oligocene transition. New York: Columbia University Press, 2003.
Знайти повний текст джерелаBuxbaum, Tim. Icehouses. Buckinghamshire: Shire, 1992.
Знайти повний текст джерелаIcehouses. Buckinghamshire: Shire, 1992.
Знайти повний текст джерелаRobberts, Léo. Les glacières à glace naturelle de Wallonie. [Soiron]: Qualité Village-Wallonie, 1989.
Знайти повний текст джерела1909-, Vermeulen J. G., and Wehdorn Manfred, eds. Eiskeller: Kulturgeschichte alter Kühltechniken. Wien: Böhlau, 1995.
Знайти повний текст джерелаLe ghiacciaie: Architetture dimenticate. Firenze: Alinea, 2007.
Знайти повний текст джерелаLavigne-Louis, Maryannick. Glacières et caves à neige du Rhône. Lyon: Conseil général du Rhône, 2000.
Знайти повний текст джерелаIce houses of Iran: Where, how, why. Costa Mesa, California: Mazda Publishers, 2013.
Знайти повний текст джерелаЧастини книг з теми "Icehouse"
Warny, Sophie, and Rosemary Askin. "Last Remnants of Cenozoic Vegetation and Organic-Walled Phytoplankton in the Antarctic Peninsula's Icehouse World." In Tectonic, Climatic, and Cryospheric Evolution of the Antarctic Peninsula, 167–92. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/2010sp000996.
Повний текст джерелаGastaldo, Robert A., Marion Bamford, John Calder, William A. DiMichele, Roberto Iannuzzi, André Jasper, Hans Kerp, et al. "The Non-analog Vegetation of the Late Paleozoic Icehouse–Hothouse and Their Coal-Forming Forested Environments." In Springer Textbooks in Earth Sciences, Geography and Environment, 291–316. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-35058-1_12.
Повний текст джерелаBuijs, GOvert J. A., and Robert H. Goldstein. "Sequence Architecture and Palaeoclimate Controls on Diagenesis Related to Subaerial Exposure of Icehouse Cyclic Pennsylvanian and Permian Carbonates." In Linking Diagenesis to Sequence Stratigraphy, 55–79. West Sussex, UK: John Wiley & Sons, Inc., 2013. http://dx.doi.org/10.1002/9781118485347.ch3.
Повний текст джерела"Icehouse." In Encyclopedic Dictionary of Archaeology, 627. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-58292-0_90014.
Повний текст джерелаTyrrell, Toby. "Icehouse Earth." In On Gaia. Princeton University Press, 2013. http://dx.doi.org/10.23943/princeton/9780691121581.003.0005.
Повний текст джерелаSummerhayes, Colin. "Icehouse Climates." In The Icy Planet, 28—C2P157. Oxford University PressNew York, 2023. http://dx.doi.org/10.1093/oso/9780197627983.003.0002.
Повний текст джерела"5. Icehouse Earth." In On Gaia, 88–112. Princeton: Princeton University Press, 2013. http://dx.doi.org/10.1515/9781400847914-006.
Повний текст джерела"Into the Icehouse." In Earth's Climate Evolution, 105–31. Chichester, UK: John Wiley & Sons, Ltd, 2015. http://dx.doi.org/10.1002/9781118897362.ch7.
Повний текст джерелаZalasiewicz, Jan, and Mark Williams. "Into the Icehouse." In The Goldilocks Planet. Oxford University Press, 2012. http://dx.doi.org/10.1093/oso/9780199593576.003.0013.
Повний текст джерела"LOCKED IN THE ICEHOUSE." In All Things, Seen and Unseen, 91–93. University of Arkansas Press, 1997. http://dx.doi.org/10.2307/j.ctv1w0xcm5.41.
Повний текст джерелаТези доповідей конференцій з теми "Icehouse"
Hearty, Paul J., and Blair R. Tormey. ""ICEHOUSE, GREENHOUSE, MADHOUSE” – HAVE WE ARRIVED?" In Joint 69th Annual Southeastern / 55th Annual Northeastern GSA Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020se-344766.
Повний текст джерелаYodjaiphet, Anusorn, and Wiwat Tippachon. "The design of IoT system for icehouse manufacturing." In 2018 5th International Conference on Business and Industrial Research (ICBIR). IEEE, 2018. http://dx.doi.org/10.1109/icbir.2018.8391157.
Повний текст джерелаKhameiss, Belkasim, Richard Fluegeman, Ahmed Muftah, William H. Hoyt, Shawn J. Malone, Jeffry D. Grigsby, Randall Bernot, Tykhon Zubkuf, and Saad K. El Ebaidi. "CORAL-ALGAL COMPETITION ON TERTIARY REEFS: GREENHOUSE TO ICEHOUSE TRANSITIONS." In Joint 53rd Annual South-Central/53rd North-Central/71st Rocky Mtn GSA Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019sc-326622.
Повний текст джерелаSardar Abadi, Mehrdad, Gerilyn S. Soreghan, Jeremy D. Owens, Xiaolei Liu, and Theodore R. Them. "ATMOSPHERIC DUST STIMULATED MARINE PRIMARY PRODUCTIVITY DURING EARTH’S PENULTIMATE ICEHOUSE." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-320538.
Повний текст джерелаWade, Bridget S., Abigail Betts, Zara Hickling, Joseph Thorogood, and Paul Upchurch. "WAXING AND WANING OF PLANKTONIC FORAMINIFERAL DIVERSITY IN THE OLIGOCENE ICEHOUSE." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-357086.
Повний текст джерелаDupont-Nivet, Guillaume, Niels Meijer, Mustafa Kaya, Delphine Tardif, Lin Li, Alexis Licht, Natasha Barbolini, et al. "MONSOONS VS. WESTERLIES DURING TIBETAN PLATEAU GROWTH AND GREENHOUSE-ICEHOUSE TRANSITION." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-338825.
Повний текст джерелаGriffis, Neil, Roland Mundil, Isabel Montanez, Jon D. Richey, Pierre Dietrich, Daniel Le Heron, Christoph Kettler, Bastien Linol, and Roberto Iannuzzi. "TIMING AND POTENTIAL CAUSES FOR THE DEMISE OF EARTH’S PENULTIMATE ICEHOUSE." In GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-367955.
Повний текст джерелаConwell, Christopher, Cole Edwards, Elizabeth M. Griffith, and Matthew R. Saltzman. "GLOBAL COOLING LINKED TO BASALTIC WEATHERING DURING THE ORDOVICIAN GREENHOUSE–ICEHOUSE TRANSITION." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-357955.
Повний текст джерелаBentley, Olivia L., Peter A. Allison, Alexandros Avdis, and Matthew D. Piggott. "THE ROLE OF BATHYMETRY IN UPWELLING INDUCED PRODUCTIVITY IN ICEHOUSE AND GREENHOUSE WORLDS." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-284659.
Повний текст джерелаMiller, Kenneth G., James V. Browning, and James D. Wright. "SEA-LEVEL CHANGES DURING CRETACEOUS TO CENOZOIC HOTHOUSE, COOL GREENHOUSE AND ICEHOUSE WORLDS." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-320321.
Повний текст джерела