Gotowe bibliografie tematyczne / Paleoecology - Quaternary

Gotowa bibliografia na temat „Paleoecology - Quaternary”

Autor: Grafiati
Data publikacji: 4 czerwca 2021
Data aktualizacji: 30 stycznia 2023

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Artykuły w czasopismach na temat "Paleoecology - Quaternary"

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Fontana, Sonia L., i Keith D. Bennett. "Quaternary paleoecology: Reconstructing past environments". Past Global Changes Magazine 22, nr 1 (kwiecień 2014): 46. http://dx.doi.org/10.22498/pages.22.1.46.

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Fontana, Sonia L., i Keith D. Bennett. "Quaternary paleoecology: Reconstructing past environments". Past Global Change Magazine 23, nr 2 (grudzień 2015): 77. http://dx.doi.org/10.22498/pages.23.2.77.

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Heusser, C. J. "Quaternary paleoecology of Fuego-Patagonia". Revista do Instituto Geológico 15, nr 1-2 (1994): 7–26. http://dx.doi.org/10.5935/0100-929x.19940002.

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Jackson, Stephen T., i Jessica L. Blois. "Community ecology in a changing environment: Perspectives from the Quaternary". Proceedings of the National Academy of Sciences 112, nr 16 (21.04.2015): 4915–21. http://dx.doi.org/10.1073/pnas.1403664111.

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Community ecology and paleoecology are both concerned with the composition and structure of biotic assemblages but are largely disconnected. Community ecology focuses on existing species assemblages and recently has begun to integrate history (phylogeny and continental or intercontinental dispersal) to constrain community processes. This division has left a “missing middle”: Ecological and environmental processes occurring on timescales from decades to millennia are not yet fully incorporated into community ecology. Quaternary paleoecology has a wealth of data documenting ecological dynamics at these timescales, and both fields can benefit from greater interaction and articulation. We discuss ecological insights revealed by Quaternary terrestrial records, suggest foundations for bridging between the disciplines, and identify topics where the disciplines can engage to mutual benefit.
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Maldonado, Antonio, i Claudio Latorre. "International Workshop on Methods in Quaternary Paleoecology". PAGES news 16, nr 1 (styczeń 2008): 38. http://dx.doi.org/10.22498/pages.16.1.38.

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Delcourt, Paul A., i Hazel R. Delcourt. "Quaternary paleoecology of the Lower Mississippi Valley". Engineering Geology 45, nr 1-4 (grudzień 1996): 219–42. http://dx.doi.org/10.1016/s0013-7952(96)00015-4.

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Martínez, S. "Quaternary continental molluscs from Northern Uruguay: distribution and paleoecology". Quaternary International 114, nr 1 (2004): 123–28. http://dx.doi.org/10.1016/s1040-6182(03)00047-8.

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Aksu, A. E., i P. J. Mudie. "Late Quaternary stratigraphy and paleoecology of northwest Labrador Sea". Marine Micropaleontology 9, nr 6 (grudzień 1985): 537–57. http://dx.doi.org/10.1016/0377-8398(85)90017-9.

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Martı́nez, Sergio, Martı́n Ubilla, Mariano Verde, Daniel Perea, Alejandra Rojas, Rosario Guérèquiz i Graciela Piñeiro. "Paleoecology and Geochronology of Uruguayan Coastal Marine Pleistocene Deposits". Quaternary Research 55, nr 2 (marzec 2001): 246–54. http://dx.doi.org/10.1006/qres.2000.2204.

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AbstractMinimum radiocarbon ages of marine Pleistocene molluscs from Uruguay range from 29,500±600 to 35,500±1900 14C yr B.P. Because knowledge of the marine Quaternary stratigraphy of Uruguay remains inadequate, no attempt is made to correlate between these deposits and recognized lithostratigraphic units. Analysis of the temperature and salinity ranges of the various molluscs suggests the establishment of a poly-euhaline fauna that inhabited waters warmer than present at the same latitude. This is supported by a northward retreat in the recent distribution of Chrysallida cf. C. gemmulosa, Nioche subrostrata, and probably Anomalocardia brasiliana. These marine Pleistocene deposits can probably be correlated with the last interglaciation (oxygen-isotopic substage 5e). At that time the fluvial-marine front of the Rio de la Plata was displaced much further northwestward than previously supposed. Chrysallida cf. C. gemmulosa and Limaria sp. are recorded in Uruguayan Quaternary deposits for the first time.
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Mancini, María. "Late Quaternary paleoecology in Southern Patagonia (46º-52º S), Argentina". Revista del Museo Argentino de Ciencias Naturales 5 (2003): 273–83. http://dx.doi.org/10.22179/revmacn.5.57.

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Rozprawy doktorskie na temat "Paleoecology - Quaternary"

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Sawada, Michael Charles. "Late quaternary paleoclimates and biogeography of North America". Thesis, University of Ottawa (Canada), 2001. http://hdl.handle.net/10393/9031.

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Pollen, spores, and dinoflagellate cysts are used with the modern analog technique (MAT) to provide paleoclimate reconstructions for terrestrial and marine environments in northeastern North America. Multivariate analysis of marine and nearby terrestrial pollen sequences from Hudson Bay, Labrador and the St. Lawrence, differentiate tundra, boreal and deciduous forest assemblages in time and space. These three regions had differing climate histories with respect to deglaciation and air mass boundaries. Prior to 6000 14C yr BP, cooler temperatures reconstructed along the Labrador margins agree with climate simulations indicating a persistent anticyclone over the Quebec-Labrador ice sheet. A late Holocene cooling at forest-tundra sites suggests a recent southern movement in the mean position of the polar front. The degree to which those critical thresholds of dissimilarity, that are used to identify non-analog pollen assemblages, are due to limitations of the modern pollen database or critical decisions within the MAT are explored by means of stochastic simulation, spatial statistics and graphical techniques. Critical thresholds of SQD, as derived by the expected value under randomization, become greater as the number of taxa in the pollen set increases. Larger pollen sets, with continentally infrequent but regionally abundant taxa, better distinguish between continental vegetation zones. Global and local spatial autocorrelation within climate anomalies indicate where the modern sample network induces biases in the climate reconstruction using the MAT. The spatial scale of terrestrial climate or vegetation reconstructions from pollen in lake-sediments is investigated through the study of pollen source area in southern Quebec. Despite the different regional vegetation, estimated pollen source areas and relevant pollen productivity for Pinus, Picea, Abies, Fagus, Quercus and Tsuga are consistent with studies from Michigan, Wisconsin and Sweden. These estimates are robust with respect to various plant abundance distance-weighting schemes and imply that the same inferences can be made regarding plant abundance from pollen throughout a lake-derived fossil pollen sequence. Stochastic simulations illustrate that the definition of relevant pollen source area requires consistent within-site vegetation heterogeneity within a network of pollen sites. Underutilized proxy-climate data from wetland taxa are demonstrated to contain climate signals at the continental scale and have the potential to further our climatic and biogeographic picture of North America over the past 21,000 years. Pollen and spores from modern wetland taxa conform to their geographic ranges and allow interpretations of their past range changes. The climatic tolerances that govern their geographic distributions are used to interpret past range changes in climatic terns. Sphagnum spore distributions suggest major peatland developments after 9 ka and 5 ka. Sphagnum, Potamogeton, Isoetes, Myriophyllum Typha/Sparganium, and Menyanthes trifoliata were in Alaska during the last glacial maximum (LGM) and moved into the ice-free corridor by 13 ka. Since the LGM, four migration routes for aquatic taxa are identified in response to the climate changes of the late Quaternary.
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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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Simpson, Emily. "Paleoecology and Land-Use of Quaternary Megafauna from Saltville, Virginia". Digital Commons @ East Tennessee State University, 2019. https://dc.etsu.edu/etd/3590.

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Land-use, feeding habits, and response to seasonality by Quaternary megaherbivores in Saltville, Virginia, is poorly understood. Stable isotope analyses of serially sampled Bootherium and Equus enamel from Saltville were used to explore seasonally calibrated (δ18O) patterns in megaherbivore diet (δ13C) and land-use (87Sr/86Sr). Overall, this dataset suggests an open forest with relatively constant temperatures year round that were similar to modern conditions. Neither Bootherium or Equus individuals spent a significant amount of time at higher elevations in the nearby Blue Ridge geologic province. These analyses provide a unique perspective on long-term response of large mammals to climatic shifts and their impact on local ecosystems. Results are also relevant to modern conservation decisions, especially those surrounding highland grassy balds in the Appalachians, and their maintenance by grazing pressure.
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Herring, Erin Mauryeen. "Late Quaternary and Holocene paleoecology of interior mesic forests of northern Idaho". Thesis, University of Oregon, 2014. http://pqdtopen.proquest.com/#viewpdf?dispub=3644438.

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The mesic forests distributed within the Rocky Mountains of northern Idaho are unique because many species contained within the forest are separated from their main distribution along the Pacific Northwest coast. It remains unclear whether most species within the inland disjunction survived the glacial periods of the Pleistocene, or whether they were more recently dispersed from coastal populations. To see if the dominant tree taxa of the mesic forests today could have persisted in a refugium south of the large ice sheets, four sediment cores were used to reconstruct the vegetation and climate history of the region. A nearly continuous record of pollen and sediment composition (biogenic silica and inorganic and organic matter) over the last ca. 120,000 years provides evidence of a dynamic ecosystem. Over a long timescale, the slow shifts in vegetation are attributed to the changes in climate. During the last interglacial period, the region was warmer and drier with a Pinus dominated mixed conifer forest. Approximately 71,000 years ago, a Pseudotsuga/Larix forest became established in the area as a response to the increased available moisture. As climate cooled and glaciers expanded the Pinus and Picea forest was the dominant vegetation type until ca. 40,000 years ago. The environment during the Last Glacial Maximum (LGM) was so harsh that no vegetation record was recorded. After the LGM, climate warmed, enabling a Pinus and Picea forest to establish and persist until the Holocene.

The mesic taxa that dominate the modern forests did not arrive in northern Idaho until the mid- to late-Holocene. The recent arrival of the dominant tree species, Thuja plicata and Tsuga mertensiana, suggests that they likely did not persist in a refugium during the last glaciation. Instead, these species recently dispersed from coastal populations, but expansion into their interior distributions was likely limited by both climate and species competition in already established forests. During the late-Quaternary, the deposition of thick tephra layers (>20 cm) from the eruptions of Glacier Peak (ca. 13,400 years ago) and Mt. Mazama (ca. 7,600 years ago) also facilitated an abrupt and persistent change in vegetation in northern Idaho.

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Bergolc, Melanie L. "A Paleoenvironmental Analysis Using Fossil Insects in Late Quaternary Deposits in Indiana and Ohio". Bowling Green State University / OhioLINK, 2004. http://rave.ohiolink.edu/etdc/view?acc_num=bgsu1092940677.

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Hu, Feng Sheng. "An ecosystem approach to the study of late-Quaternary environmental change in southwestern Alaska /". Thesis, Connect to this title online; UW restricted, 1994. http://hdl.handle.net/1773/5577.

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Herring, Erin. "Late Quaternary and Holocene Paleoecology of Interior Mesic Forests of Northern Idaho". Thesis, University of Oregon, 2014. http://hdl.handle.net/1794/18509.

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The mesic forests distributed within the Rocky Mountains of northern Idaho are unique because many species contained within the forest are separated from their main distribution along the Pacific Northwest coast. It remains unclear whether most species within the inland disjunction survived the glacial periods of the Pleistocene, or whether they were more recently dispersed from coastal populations. To see if the dominant tree taxa of the mesic forests today could have persisted in a refugium south of the large ice sheets, four sediment cores were used to reconstruct the vegetation and climate history of the region. A nearly continuous record of pollen and sediment composition (biogenic silica and inorganic and organic matter) over the last ca. 120,000 years provides evidence of a dynamic ecosystem. Over a long timescale, the slow shifts in vegetation are attributed to the changes in climate. During the last interglacial period, the region was warmer and drier with a Pinus dominated mixed conifer forest. Approximately 71,000 years ago, a Pseudotsuga/Larix forest became established in the area as a response to the increased available moisture. As climate cooled and glaciers expanded the Pinus and Picea forest was the dominant vegetation type until ca. 40,000 years ago. The environment during the Last Glacial Maximum (LGM) was so harsh that no vegetation record was recorded. After the LGM, climate warmed, enabling a Pinus and Picea forest to establish and persist until the Holocene. The mesic taxa that dominate the modern forests did not arrive in northern Idaho until the mid- to late-Holocene. The recent arrival of the dominant tree species, Thuja plicata and Tsuga mertensiana, suggests that they likely did not persist in a refugium during the last glaciation. Instead, these species recently dispersed from coastal populations, but expansion into their interior distributions was likely limited by both climate and species competition in already established forests. During the late-Quaternary, the deposition of thick tephra layers (>20 cm) from the eruptions of Glacier Peak (ca. 13,400 years ago) and Mt. Mazama (ca. 7,600 years ago) also facilitated an abrupt and persistent change in vegetation in northern Idaho.
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Woolfenden, Wallace Bird 1941. "Late Quaternary vegetation history of the southern Owens Valley region, Inyo County, California". Diss., The University of Arizona, 1996. http://hdl.handle.net/10150/282184.

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This study analyzes the pollen, spores, and algae in the upper 90 m section of a mostly continuous, well dated, 323 m core (OL-92) from Owens Lake, southeastern California. The entire core has produced a paleoclimatic record for the past ∼800 ka. The 90 m interval dates from ∼9 ka to ∼151 ka beginning with the penultimate glaciation and ending during the termination of the last glaciation. The record shows high amplitude fluctuations in the abundances of pine, juniper, saltbush, sagebrush, chenopods/amaranths, and Ambrosia-type pollen. High percentages of juniper pollen with low percentages of desertscrub pollen during the intervals ∼150 ka to ∼120 ka and 73 ka to ∼20 ka alternate with low juniper pollen and relatively high percentages of desertscrub and oak pollen during the intervals ∼118 ka to ∼103 ka and ∼18 ka ∼10 ka and into the Holocene. Sagebrush pollen varies with juniper pollen but has a tendency to lead it in time. Pine and fir pollen tends to vary inversely with juniper over the long term. These trends are interpreted as vegetation change in response to glacial-interglacial cycles: During cold-wet glacial climates there was a downslope expansion of juniper woodland and sagebrush scrub, contraction of Sierra Nevada mixed conifer forest, and displacement of warm desertscrub, suggesting average temperature and precipitation departures from modern values ranging from -2°C to -6°C and from +100 mm to +350 mm. Conversely under warmer and drier interglacials warm desert shrubs expanded their range in the lowlands, juniper and sagebrush retreated upslope, and the Sierran forests expanded. Estimated average temperature and precipitation departures from modern values ranged from -0.5°C to +3.7°C and +13 to -26 mm. Comparison of the pollen spectra spanning the penultimate and ultimate glacial maxima shows the former to have been longer and more intense, in accord with the Sierra Nevada glacial record. Similarly, the higher abundances of Ambrosia pollen during the last interglaciation, compared to the Holocene, indicate warmer temperatures in the former. The presence of high oak percentages also during the last interglaciation suggest an expansion of the summer monsoon. Finally, the match of the juniper curve with the marine oxygen isotope chronostratigraphy suggests a link between vegetation change in the southern Owens Valley and global climate.
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Anshari, Gusti Zakaria. "Late quaternary vegetation and environments in the Lake Sentarum Wildlife Reserve, West Kalimantan, Indonesia". Monash University, School of Geography and Environmental Science, 2000. http://arrow.monash.edu.au/hdl/1959.1/9252.

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Sugden, Jean Mary. "Late quaternary palaeoecology of the central and marginal uplands of the Karoo, South Africa". Doctoral thesis, University of Cape Town, 1990. http://hdl.handle.net/11427/18278.

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Pollen analysis of organic sediments from vleis in upland areas of the Central and marginal Karoo has provided a vegetation history spanning the late Quaternary in the Winterberg, Sneeuberg, Nuweveldberg and Cederberg Mountains. Fossil pollen studies indicate moist conditions at the beginning of the Holocene, followed by a drier period. The second half of the Holocene (4 600 BP) is characterised by moister conditions, becoming drier towards the present and resulting in a decline in grasslands and an increase in Karoo-bushes. In the western Cape, the late Pleistocene (15 000 to 10 000 BP) was characterised by conditions moister than the present. This was followed by a drier period which ameliorated in the late Holocene. Although climatic fluctuations occurred, fynbos has been maintained in situ throughout the sedimentation period (14 600 BP), highlighting the dominant role of the substrate and secondary importance of climate. Climatic changes caused a shuffling of plant communities within the Fynbos Biome - this long uninterrupted history may be one reason for the high species diversity of fynbos. San hunter-gatherers, who occupied southern Africa prior to 4 000 BP, had a negligible impact on the vegetation. Khoi herders, who were first documented in the fossil record about 1 800 BP, had a slight impact on the vegetation, particularly by altering the fire regime. However, the arrival of European Trekboers some four hundred years ago had a significant effect on the environment. Although the general climatic trend in the Karoo is one of a drier phase, the decline in grasses and eastward movement of xeric Karroid elements has been accelerated due to mismanagement and sedentary farming techniques. An extensive contemporary pollen rain study has been undertaken to examine the representivity of these fossil pollen data. The investigation shows that contemporary pollen rain is a good reflection of the vegetation communities in the Karoo and Cederberg. Multiple discriminant analysis compares fossil pollen assemblages with contemporary pollen spectra and proved useful for determining whether modern analogues exist for the fossil pollen assemblages. TWISA confirmed the zones derived from discriminant analysis. Environmental changes have occurred in the Karoo during the late Quaternary, resulting in fluctuations and changes in vegetation patterns which have been accelerated in the recent past by human activity. Bibliography: pages 293-318.
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Książki na temat "Paleoecology - Quaternary"

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Smykatz-Kloss, Werner, i Peter Felix-Henningsen, red. Paleoecology of Quaternary Drylands. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/b92353.

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J, Williams M. A., red. Quaternary environments. Wyd. 2. New York: Arnold, 1998.

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H, Birks Hilary, red. Quaternary palaeoecology. Caldwell, N.J: Blackburn Press, 2004.

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J, Williams M. A., red. Quaternary environments. London: Edward Arnold, 1993.

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Madsen, David B. Late Quaternary paleoecology in the Bonneville Basin. [Salt Lake City]: Utah Geological Survey, 2000.

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1948-, Lancaster Nicholas, red. Late Quaternary palaeoenvironments of southern Africa. Oxford [England]: Clarendon Press, 1988.

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K, Shane Linda C., Cushing Edward J. 1933-, National Science Foundation (U.S.). Climate Dynamics Program. i University of Minnesota, red. Quaternary landscapes. Minneapolis: University of Minnesota Press, 1991.

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Walker, M. J. C. 1947-, red. Late Quaternary environmental change: Physical and human perspectives. Wyd. 2. New York: Prentice Hall, 2005.

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Jakab, Gusztáv. Paleoecology of peatlands: Quaternary climate reconstruction from Hungary. Hauppauge, N.Y: Nova Science Publishers, 2009.

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Holmes, Jonathan, i A. R. Chivas. The ostracoda: Applications in Quaternary research. Washington, DC: American Geophysical Union, 2002.

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Części książek na temat "Paleoecology - Quaternary"

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Smykatz-Kloss, W., i P. Felix-Henningsen. "The Importance of Desert Margins as Indicators for Global Climatic Fluctuations (Introduction)". W Paleoecology of Quaternary Drylands, 1–3. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-540-44930-0_1.

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Eitel, Bernhard, Wolf Dieter Blümel i Klaus Hüser. "Palaeoenvironmental Transitions Between 22 ka and 8 ka in Monsoonally Influenced Namibia". W Paleoecology of Quaternary Drylands, 167–94. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-540-44930-0_10.

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Grunert, Jörg, i Frank Lehmkuhl. "Aeolian sedimentation in arid and semi-arid environments of Western Mongolia". W Paleoecology of Quaternary Drylands, 195–218. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-540-44930-0_11.

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Mischke, S., J. Hofmann i M. E. Schudack. "Ostracod ecology of alluvial loess deposits in an eastern Tian Shan palaeo-lake (NW China)". W Paleoecology of Quaternary Drylands, 219–31. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-540-44930-0_12.

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Jäkel, Dieter. "Critical comments on the interpretation and publication of 14C, TL/OSL and 230Th/U dates and on the problem of teleconnections between global climatic processes". W Paleoecology of Quaternary Drylands, 233–42. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-540-44930-0_13.

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Schütt, Brigitta. "The chemistry of playa-lake-sediments as a tool for the reconstruction of Holocene environmental conditions - a case study from the central Ebro basin". W Paleoecology of Quaternary Drylands, 5–30. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-540-44930-0_2.

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Baumhauer, Roland, Erhard Schulz i Simon Pomel. "Environmental changes in the Central Sahara during the Holocene - The Mid-Holocene transition from freshwater lake into sebkha in the Segedim depression, NE Niger". W Paleoecology of Quaternary Drylands, 31–45. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-540-44930-0_3.

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Felix-Henningsen, Peter. "Genesis and Paleo-ecological Interpretation of Swamp Ore Deposits at Sahara Paleo-lakes of East Niger". W Paleoecology of Quaternary Drylands, 47–72. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-540-44930-0_4.

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Sponholz, Barbara. "Fulgurites as palaeoclimatic indicators - the proof of fulgurite fragments in sand samples". W Paleoecology of Quaternary Drylands, 73–78. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-540-44930-0_5.

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Rögner, Konrad, Katharina Knabe, Bernd Roscher, Werner Smykatz-Kloss i Ludwig Zöller. "Alluvial loess in the Central Sinai: Occurrence, origin, and palaeoclimatological consideration". W Paleoecology of Quaternary Drylands, 79–99. Berlin, Heidelberg: Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-540-44930-0_6.

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Streszczenia konferencji na temat "Paleoecology - Quaternary"

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Hodelka, Bailee, Michael McGlue, Manuel R. Palacios-Fest i Susan Zimmerman. "LATE QUATERNARY OSTRACOD STRATIGRAPHY AND PALEOECOLOGY FROM MONO LAKE, CALIFORNIA". W GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-366786.

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McGuire, Jenny L. "MAKING THE MOST OF THE LATE QUATERNARY PALEOECOLOGY OF THE SOUTHEAST". W 65th Annual Southeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016se-273691.

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Hodelka, Bailee N., Michael M. McGlue, Manuel R. Palacios-Fest i Susan H. Zimmerman. "PRELIMINARY LATE QUATERNARY OSTRACODE STRATIGRAPHY AND PALEOECOLOGY FROM MONO LAKE (EASTERN SIERRA NEVADA)". W GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-358164.

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Hidalgo, Claudio. "2021 FAROUK EL-BAZ AWARD: NEW FRONTIERS IN QUATERNARY PALEOECOLOGY OF THE ATACAMA DESERT". W GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-381795.

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George, Christian O. "EVALUATING THE GEOGRAPHIC DISTRIBUTION OF QUATERNARY SHREWS: THE POTENTIAL FOR PALEOECOLOGIC INTERPRETATIONS ABOVE THE SPECIES LEVEL". W GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-308434.

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Raporty organizacyjne na temat "Paleoecology - Quaternary"

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Clague, J. J., i G. M. Macdonald. Paleoecology and paleoclimatology [Chapter 1: Quaternary geology of the Canadian Cordillera]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127943.

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Schweger, C. E. Paleoecology of the western Canadian Ice - Free Corridor [Chapter 7: Quaternary Environments in Canada As Documented By Paleobotanical Case Histories]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131561.

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Pinney, D. S., i D. M. Hopkins. Late Pleistocene paleoecology of Dalton Gulch, Tofty mining district, central Alaska (poster): Canadian Quaternary Association Meeting, Whitehorse, Yukon Territory, Canada, August 20-29, 2001. Alaska Division of Geological & Geophysical Surveys, sierpień 2001. http://dx.doi.org/10.14509/21841.

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