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Articoli di riviste sul tema "Quaternary climate change"

Autore: Grafiati

Pubblicato: 4 giugno 2021

Ultima modifica: 6 febbraio 2022

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1

Adams, Jonathan, Mark Maslin, and Ellen Thomas. "Sudden climate transitions during the Quaternary." Progress in Physical Geography: Earth and Environment 23, no. 1 (March 1999): 1–36. http://dx.doi.org/10.1177/030913339902300101.

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The time span of the past few million years has been punctuated by many rapid climate transitions, most of them on timescales of centuries to decades. The most detailed information is available for the Younger Dryas-to-Holocene stepwise change around 11 500 years ago, which seems to have occurred over a few decades. The speed of this change is probably representative of similar but less well studied climate transitions during the last few hundred thousand years. These include sudden cold events (Heinrich events/stadials), warm events (interstadials) and the beginning and ending of long warm ph

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2

Preusser, Frank, and Dirk Radies. "Quaternary climate change in south-eastern Arabia." PAGES news 14, no. 1 (April 2006): 38–39. http://dx.doi.org/10.22498/pages.14.1.38.

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Ogola, Christine A. "Eastern African Quaternary Climate change and variability." Past Global Changes Magazine 22, no. 1 (April 2014): 53. http://dx.doi.org/10.22498/pages.22.1.53.

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4

Olson, Carolyn. "The Soil Record of Quaternary Climate Change." Quaternary International 162-163 (March 2007): 1–2. http://dx.doi.org/10.1016/j.quaint.2006.11.010.

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5

Weigelt, Patrick, Manuel Jonas Steinbauer, Juliano Sarmento Cabral, and Holger Kreft. "Late Quaternary climate change shapes island biodiversity." Nature 532, no. 7597 (March 30, 2016): 99–102. http://dx.doi.org/10.1038/nature17443.

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6

Darling, W. G. "The isotope hydrology of quaternary climate change☆." Journal of Human Evolution 60, no. 4 (April 2011): 417–27. http://dx.doi.org/10.1016/j.jhevol.2010.05.006.

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7

Claussen, M. "Late Quaternary vegetation – climate feedbacks*." Climate of the Past Discussions 5, no. 1 (February 24, 2009): 635–70. http://dx.doi.org/10.5194/cpd-5-635-2009.

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Abstract. Feedbacks between vegetation and other components of the climate system are discussed with respect to their influence on climate dynamics during the late Quaternary, i.e., the last glacial – interglacial cycles. When weighting current understanding based on interpretation of palaeobotanic and palaeoclimatic evidence by numerical climate system models, a number of arguments speak in favour of vegetation dynamics being an amplifier of orbital forcing. (a) The vegetation – snow albedo feedback in synergy with the sea ice – albedo feedback tends to amplify Northern Hemisphere and global

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8

Claussen*, M. "Late Quaternary vegetation-climate feedbacks." Climate of the Past 5, no. 2 (June 3, 2009): 203–16. http://dx.doi.org/10.5194/cp-5-203-2009.

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Abstract. Feedbacks between vegetation and other components of the climate system are discussed with respect to their influence on climate dynamics during the late Quaternary, i.e., the last glacial-interglacial cycles. When weighting current understanding based on interpretation of palaeobotanic and palaeoclimatic evidence by numerical climate system models, a number of arguments speak in favour of vegetation dynamics being an amplifier of orbital forcing. (a) The vegetation-snow albedo feedback in synergy with the sea-ice albedo feedback tends to amplify Northern Hemisphere and global mean t

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9

Webb III, Thompson, Katherine H. Anderson, Patrick J. Bartlein, and Robert S. Webb. "Late quaternary climate change in eastern North America." Quaternary Science Reviews 17, no. 6-7 (April 1998): 587–606. http://dx.doi.org/10.1016/s0277-3791(98)00013-4.

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10

Ogola, Christine, Asfawossen Asrat, Stephen Rucina, and Elgidius B. Ichumbaki. "Equatorial eastern Africa: Quaternary climate change and variability." Quaternary International 369 (May 2015): 1–2. http://dx.doi.org/10.1016/j.quaint.2015.04.012.

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11

Lamy, Klump, Hebbeln, and Wefer. "Late Quaternary rapid climate change in northern Chile." Terra Nova 12, no. 1 (February 2000): 8–13. http://dx.doi.org/10.1046/j.1365-3121.2000.00265.x.

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12

Su, Tao, Jonathan M. Adams, Torsten Wappler, Yong-Jiang Huang, Frédéric M. B. Jacques, Yu-Sheng (Christopher) Liu, and Zhe-Kun Zhou. "Resilience of plant-insect interactions in an oak lineage through Quaternary climate change." Paleobiology 41, no. 1 (January 2015): 174–86. http://dx.doi.org/10.1017/pab.2014.11.

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AbstractPlant-insect interactions are vital for structuring terrestrial ecosystems. It is still unclear how climate change in geological time might have shaped plant-insect interactions leading to modern ecosystems. We investigated the effect of Quaternary climate change on plant-insect interactions by observing insect herbivory on leaves of an evergreen sclerophyllous oak lineage (QuercussectionHeterobalanus, HET) from a late Pliocene flora and eight living forests in southwestern China. Among the modern HET populations investigated, the damage diversity tends to be higher in warmer and wette

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13

Kehl, Martin. "Quaternary climate change in Iran – the state of knowledge." ERDKUNDE 63, no. 1 (2009): 1–17. http://dx.doi.org/10.3112/erdkunde.2009.01.01.

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14

Davies, Purvis, and Gittleman. "Quaternary Climate Change and the Geographic Ranges of Mammals." American Naturalist 174, no. 3 (2009): 297. http://dx.doi.org/10.2307/40306059.

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15

McCarroll, Danny. "Future climate change and the British Quaternary research community." Quaternary Science Reviews 29, no. 13-14 (June 2010): 1661–72. http://dx.doi.org/10.1016/j.quascirev.2010.04.003.

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16

Davies, T. Jonathan, Andy Purvis, and John L. Gittleman. "Quaternary Climate Change and the Geographic Ranges of Mammals." American Naturalist 174, no. 3 (September 2009): 297–307. http://dx.doi.org/10.1086/603614.

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17

Davis, M. B. "Range Shifts and Adaptive Responses to Quaternary Climate Change." Science 292, no. 5517 (April 27, 2001): 673–79. http://dx.doi.org/10.1126/science.292.5517.673.

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18

Prost, Stefan, Johannes Klietmann, Thijs van Kolfschoten, Robert P. Guralnick, Eric Waltari, Klaas Vrieling, Mathias Stiller, et al. "Effects of late quaternary climate change on Palearctic shrews." Global Change Biology 19, no. 6 (March 9, 2013): 1865–74. http://dx.doi.org/10.1111/gcb.12153.

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19

Berger, Wolfgang H., Michael Schulz, and Gerold Wefer. "Quaternary oceans and climate change: lessons for the future?" International Journal of Earth Sciences 99, S1 (May 16, 2010): 171–89. http://dx.doi.org/10.1007/s00531-010-0553-y.

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20

Lioubimtseva, Elena. "Climate change in arid environments: revisiting the past to understand the future." Progress in Physical Geography: Earth and Environment 28, no. 4 (December 2004): 502–30. http://dx.doi.org/10.1191/0309133304pp422oa.

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Arid regions are expected to undergo significant changes under a scenario of climate warming, but there is considerable variability and uncertainty in these estimates between different scenarios. The complexities of precipitation changes, vegetation-climate feedbacks and direct physiological effects of CO2 on vegetation present particular challenges for climate change modelling of arid regions. Great uncertainties exist in the prediction of arid ecosystem responses to elevated CO2 and global warming. Palaeodata provide important information about the past frequency, intensity and subregional p

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21

Colinvaux, P. A. "Quaternary forcing of diversity in neotropical forests." Paleontological Society Special Publications 6 (1992): 65. http://dx.doi.org/10.1017/s2475262200006250.

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The climate of the Amazon during the last northern glaciation may be taken to represent the normal climate of the basin throughout the Quaternary, since boundary conditions for Amazon and neotropical environments had not otherwise changed since the Andean orogeny and emplacment of the Isthmus of Panama late in the Teritary.The few radiocarbon dated data describing the climate of the ice age Amazon suggest that the principal climatic forcing was cooling in excess of 6 o C, associated with modest reductions in precipitation. Unlike Africa, the New World tropics were not noticeably arid. The evid

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22

MacDonald, G. M., K. D. Bennett, S. T. Jackson, L. Parducci, F. A. Smith, J. P. Smol, and K. J. Willis. "Impacts of climate change on species, populations and communities: palaeobiogeographical insights and frontiers." Progress in Physical Geography: Earth and Environment 32, no. 2 (April 2008): 139–72. http://dx.doi.org/10.1177/0309133308094081.

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Understanding climate change and its potential impact on species, populations and communities is one of the most pressing questions of twenty-first-century conservation planning. Palaeobiogeographers working on Cenozoic fossil records and other lines of evidence are producing important insights into the dynamic nature of climate and the equally dynamic response of species, populations and communities. Climatic variations ranging in length from multimillennia to decades run throughout the palaeo-records of the Quaternary and earlier Cenozoic and have been shown to have had impacts ranging from

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23

Han, Yongming, Zhisheng An, Jennifer R. Marlon, Raymond S. Bradley, Changlin Zhan, Richard Arimoto, Youbin Sun, et al. "Asian inland wildfires driven by glacial–interglacial climate change." Proceedings of the National Academy of Sciences 117, no. 10 (February 24, 2020): 5184–89. http://dx.doi.org/10.1073/pnas.1822035117.

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Wildfire can influence climate directly and indirectly, but little is known about the relationships between wildfire and climate during the Quaternary, especially how wildfire patterns varied over glacial–interglacial cycles. Here, we present a high-resolution soot record from the Chinese Loess Plateau; this is a record of large-scale, high-intensity fires over the past 2.6 My. We observed a unique and distinct glacial–interglacial cyclicity of soot over the entire Quaternary Period synchronous with marine δ18O and dust records, which suggests that ice-volume-modulated aridity controlled wildf

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24

Hodell, David A., and James E. T. Channell. "Mode transitions in Northern Hemisphere glaciation: co-evolution of millennial and orbital variability in Quaternary climate." Climate of the Past 12, no. 9 (September 7, 2016): 1805–28. http://dx.doi.org/10.5194/cp-12-1805-2016.

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Abstract. We present a 3.2 Myr record of stable isotopes and physical properties at IODP Site U1308 (reoccupation of DSDP Site 609) located within the ice-rafted detritus (IRD) belt of the North Atlantic. We compare the isotope and lithological proxies at Site U1308 with other North Atlantic records (e.g., sites 982, 607/U1313, and U1304) to reconstruct the history of orbital and millennial-scale climate variability during the Quaternary. The Site U1308 record documents a progressive increase in the intensity of Northern Hemisphere glacial–interglacial cycles during the late Pliocene and Quate

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25

Willis, Katherine J., and Karl J. Niklas. "The role of Quaternary environmental change in plant macroevolution: the exception or the rule?" Philosophical Transactions of the Royal Society of London. Series B: Biological Sciences 359, no. 1442 (February 29, 2004): 159–72. http://dx.doi.org/10.1098/rstb.2003.1387.

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The Quaternary has been described as an important time for genetic diversification and speciation. This is based on the premise that Quaternary climatic conditions fostered the isolation of populations and, in some instances, allopatric speciation. However, the ‘Quaternary Ice–Age speciation model’ rests on two key assumptions: (i) that biotic responses to climate change during the Quaternary were significantly different from those of other periods in Earth's history; and (ii) that the mechanisms of isolation during the Quaternary were sufficient in time and space for genetic diversification t

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26

Guiot, Joël. "Late Quaternary Climatic Change in France Estimated from Multivariate Pollen Time Series." Quaternary Research 28, no. 1 (July 1987): 100–118. http://dx.doi.org/10.1016/0033-5894(87)90036-6.

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AbstractIn regions like southern France, where usual analytical techniques are unsatisfactory due to the heavy influence of human activity and the existence of a complex climate, the quantitative reconstruction of climate from pollen is particularly difficult. That is why an original method has been performed. The first step of the method, based on best analogs estimation and multiple regression, is to calculate a relationship between climate (monthly temperature and precipitation) and modern pollen spectra for data from 182 sites. The result is called the “analog climate.” The second step of

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27

Schlütz, Frank. "Climate change in the central Himalaya during the late Quaternary." Quaternary International 279-280 (November 2012): 435. http://dx.doi.org/10.1016/j.quaint.2012.08.1418.

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28

Anonymous. "Methane Hydrates in Quaternary Climate Change: The Clathrate Gun Hypothesis." Eos, Transactions American Geophysical Union 83, no. 45 (2002): 513. http://dx.doi.org/10.1029/2002eo000359.

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29

Schmidt, Daniela N., Sabrina Renaud, and Jörg Bollmann. "Response of planktic foraminiferal size to late Quaternary climate change." Paleoceanography 18, no. 2 (May 22, 2003): n/a. http://dx.doi.org/10.1029/2002pa000831.

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30

Hocknull, Scott A., Jian-xin Zhao, Yue-xing Feng, and Gregory E. Webb. "Responses of Quaternary rainforest vertebrates to climate change in Australia." Earth and Planetary Science Letters 264, no. 1-2 (December 2007): 317–31. http://dx.doi.org/10.1016/j.epsl.2007.10.004.

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31

Erb, Michael P., Charles S. Jackson, and Anthony J. Broccoli. "Using Single-Forcing GCM Simulations to Reconstruct and Interpret Quaternary Climate Change." Journal of Climate 28, no. 24 (December 15, 2015): 9746–67. http://dx.doi.org/10.1175/jcli-d-15-0329.1.

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Abstract The long-term climate variations of the Quaternary were primarily influenced by concurrent changes in Earth’s orbit, greenhouse gases, and ice sheets. However, because climate changes over the coming century will largely be driven by changes in greenhouse gases alone, it is important to better understand the separate contributions of each of these forcings in the past. To investigate this, idealized equilibrium simulations are conducted in which the climate is driven by separate changes in obliquity, precession, CO2, and ice sheets. To test the linearity of past climate change, anomal

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32

Ghodrati, Alireza, Payam Alemi Safaval, and Mir Ahmad Lashteh Neshaei. "Climate Change Impact of the Caspian Sea Level Changes in the Quaternary Sediment." Frontiers in Environmental Engineering 5 (2016): 1. http://dx.doi.org/10.14355/fiee.2016.05.001.

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33

Ficetola, Gentile Francesco, Mattia Falaschi, Anna Bonardi, Emilio Padoa-Schioppa, and Roberto Sindaco. "Biogeographical structure and endemism pattern in reptiles of the Western Palearctic." Progress in Physical Geography: Earth and Environment 42, no. 2 (April 2018): 220–36. http://dx.doi.org/10.1177/0309133318765084.

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The analysis of biogeographical structure and patterns of endemism are central topics of biogeography, but require exhaustive distribution data. A lack of accurate broad-scale information on the distribution of reptiles has so far limited the analyses of biogeographical structure. Here we analysed the distribution of reptiles within the broad-sense Western Palearctic to assess biogeographical regionalization using phylogenetic and non-phylogenetic approaches, identified areas of endemism and evaluated the environmental factors promoting community uniqueness and endemism. We gathered distributi

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34

Seppä, Heikki, and K. D. Bennett. "Quaternary pollen analysis: recent progress in palaeoecology and palaeoclimatology." Progress in Physical Geography: Earth and Environment 27, no. 4 (December 2003): 548–79. http://dx.doi.org/10.1191/0309133303pp394oa.

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During the last decade Quaternary pollen analysis has developed towards improved pollen-taxonomical precision, automated pollen identification and more rigorous definition of pollen assemblage zones. There have been significant efforts to model the spatial representation of pollen records in lake sediments which is important for more precise interpretation of the pollen records in terms of past vegetation patterns. We review the difficulties in matching modelled post-glacial plant migration patterns with pollen-based palaeorecords and discuss the potential of DNA analysis of pollen to investig

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35

Rother, H., and J. Shulmeister. "Synoptic climate change as a driver of late Quaternary glaciations in the mid-latitudes of the Southern Hemisphere." Climate of the Past 2, no. 1 (May 12, 2006): 11–19. http://dx.doi.org/10.5194/cp-2-11-2006.

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Abstract. The relative timing of late Quaternary glacial advances in mid-latitude (40-55° S) mountain belts of the Southern Hemisphere (SH) has become a critical focus in the debate on global climate teleconnections. On the basis of glacial data from New Zealand (NZ) and southern South America it has been argued that interhemispheric synchrony or asynchrony of Quaternary glacial events is due to Northern Hemisphere (NH) forcing of SH climate through either the ocean or atmosphere systems. Here we present a glacial snow-mass balance model that demonstrates that large scale glaciation in the tem

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36

Rother, H., and J. Shulmeister. "Synoptic climate change as a driver of late Quaternary glaciations in the mid-latitudes of the Southern Hemisphere." Climate of the Past Discussions 1, no. 3 (December 1, 2005): 231–53. http://dx.doi.org/10.5194/cpd-1-231-2005.

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Abstract. The relative timing of late Quaternary glacial advances in mid-latitude (40–55° S) mountain belts of the Southern Hemisphere (SH) has become a critical focus in the debate on global climate teleconnections. On the basis of glacial data from New Zealand and southern South America it has been argued that interhemispheric synchrony or asynchrony of Quaternary glacial events is due to Northern Hemisphere (NH) forcing of SH climate through either the ocean or atmosphere systems. Here we present a glacial snow-mass balance model that demonstrates that large scale glacial advances in the te

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37

Sandom, Christopher, Søren Faurby, Brody Sandel, and Jens-Christian Svenning. "Global late Quaternary megafauna extinctions linked to humans, not climate change." Proceedings of the Royal Society B: Biological Sciences 281, no. 1787 (July 22, 2014): 20133254. http://dx.doi.org/10.1098/rspb.2013.3254.

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The late Quaternary megafauna extinction was a severe global-scale event. Two factors, climate change and modern humans, have received broad support as the primary drivers, but their absolute and relative importance remains controversial. To date, focus has been on the extinction chronology of individual or small groups of species, specific geographical regions or macroscale studies at very coarse geographical and taxonomic resolution, limiting the possibility of adequately testing the proposed hypotheses. We present, to our knowledge, the first global analysis of this extinction based on comp

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38

Beerling, David J., C. Nicholas Hewitt, John A. Pyle, and John A. Raven. "Critical issues in trace gas biogeochemistry and global change." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 365, no. 1856 (May 18, 2007): 1629–42. http://dx.doi.org/10.1098/rsta.2007.2037.

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The atmospheric composition of trace gases and aerosols is determined by the emission of compounds from the marine and terrestrial biospheres, anthropogenic sources and their chemistry and deposition processes. Biogenic emissions depend upon physiological processes and climate, and the atmospheric chemistry is governed by climate and feedbacks involving greenhouse gases themselves. Understanding and predicting the biogeochemistry of trace gases in past, present and future climates therefore demands an interdisciplinary approach integrating across physiology, atmospheric chemistry, physics and

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39

Goldner, A., M. Huber, N. Diffenbaugh, and R. Caballero. "Implications of the permanent El Niño teleconnection "blueprint" for past global and North American hydroclimatology." Climate of the Past 7, no. 3 (July 13, 2011): 723–43. http://dx.doi.org/10.5194/cp-7-723-2011.

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Abstract. Substantial evidence exists for wetter-than-modern continental conditions in North America during the pre-Quaternary warm climate intervals. This is in apparent conflict with the robust global prediction for future climate change of a northward expansion of the subtropical dry zones that should drive aridification of many semiarid regions. Indeed, areas of expected future aridification include much of western North America, where extensive paleoenvironmental records are documented to have been much wetter before the onset of Quaternary ice ages. It has also been proposed that climate

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Hoek, Wim Z. "The interactions between Quaternary Geology and Archaeology." Netherlands Journal of Geosciences - Geologie en Mijnbouw 89, no. 1 (July 2010): 1–2. http://dx.doi.org/10.1017/s0016774600000779.

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This special issue focuses on the interactions between Quaternary Geology and Archaeology and results from the INQUA-NL Symposium: ‘Late Quaternary Climate Change: a Human Perspective’ held on April 14th2009, KNAW Trippenhuis, Amsterdam. The symposium was attended by over 125 scientists and students with interest in the fields of Quaternary Geology and Archaeology. The symposium was organized for the INQUA Netherlands commission (INQUA-NL) by Wim Hoek, Faculty of Geosciences, Utrecht University (UU), Henry Hooghiemstra, Faculty of Science, University of Amsterdam (UvA), and Jos Deeben, Nationa

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Miller, Charlotte, Jemma Finch, Trevor Hill, Francien Peterse, Marc Humphries, Matthias Zabel, and Enno Schefuß. "Late Quaternary climate variability at Mfabeni peatland, eastern South Africa." Climate of the Past 15, no. 3 (June 27, 2019): 1153–70. http://dx.doi.org/10.5194/cp-15-1153-2019.

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Abstract. The scarcity of continuous, terrestrial, palaeoenvironmental records in eastern South Africa leaves the evolution of late Quaternary climate and its driving mechanisms uncertain. Here we use a ∼7 m long core from Mfabeni peatland (KwaZulu-Natal, South Africa) to reconstruct climate variability for the last 32 000 years (cal ka BP). We infer past vegetation and hydrological variability using stable carbon (δ13Cwax) and hydrogen isotopes (δDwax) of plant-wax n-alkanes and use Paq to reconstruct water table changes. Our results indicate that late Quaternary climate in eastern South Afri

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Claußen, M. "Abrupt African Quaternary climate and vegetation change: concepts, modelling, and data." Quaternary International 404 (June 2016): 175. http://dx.doi.org/10.1016/j.quaint.2015.08.096.

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Cronin, Thomas M., Dawn M. DeMartino, Gary S. Dwyer, and Julio Rodriguez-Lazaro. "Deep-sea ostracode species diversity: response to late Quaternary climate change." Marine Micropaleontology 37, no. 3-4 (September 1999): 231–49. http://dx.doi.org/10.1016/s0377-8398(99)00026-2.

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Thomas, Michael F., Jonathan Nott, Andrew S. Murray, and David M. Price. "Fluvial response to late Quaternary climate change in NE Queensland, Australia." Palaeogeography, Palaeoclimatology, Palaeoecology 251, no. 1 (July 2007): 119–36. http://dx.doi.org/10.1016/j.palaeo.2007.02.021.

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Sugden, David. "Quaternary climate change and South America: a tribute to Chalmers Clapperton." Journal of Quaternary Science 15, no. 4 (2000): 299. http://dx.doi.org/10.1002/1099-1417(200005)15:4<299::aid-jqs546>3.0.co;2-4.

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Nott, Jonathan. "Tropical cyclones, global climate change and the role of Quaternary studies." Journal of Quaternary Science 26, no. 5 (June 14, 2011): 468–73. http://dx.doi.org/10.1002/jqs.1524.

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Sandel, B., L. Arge, B. Dalsgaard, R. G. Davies, K. J. Gaston, W. J. Sutherland, and J. C. Svenning. "The Influence of Late Quaternary Climate-Change Velocity on Species Endemism." Science 334, no. 6056 (October 6, 2011): 660–64. http://dx.doi.org/10.1126/science.1210173.

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Waters, Michael R., and C. Vance Haynes. "Late Quaternary arroyo formation and climate change in the American Southwest." Geology 29, no. 5 (2001): 399. http://dx.doi.org/10.1130/0091-7613(2001)029<0399:lqafac>2.0.co;2.

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Ridgwell, Andy J. "Implications of the glacial CO2“iron hypothesis” for Quaternary climate change." Geochemistry, Geophysics, Geosystems 4, no. 9 (September 2003): n/a. http://dx.doi.org/10.1029/2003gc000563.

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Edwards, R. L., D. X. Yuan, Z. S. An, Y. J. Wang, A. S. Auler, H. Cheng, H. Rowe, X. F. Wang, M. J. Kelly, and C. A. Dykoski. "Timing and nature of late Quaternary climate change from cave deposits." Geochimica et Cosmochimica Acta 70, no. 18 (August 2006): A155. http://dx.doi.org/10.1016/j.gca.2006.06.1376.

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