509 a Αab. See Fractionation Factor Aardwolf, 298 Abiotic Triggers In

Total Page:16

File Type:pdf, Size:1020Kb

509 a Αab. See Fractionation Factor Aardwolf, 298 Abiotic Triggers In Index A and maize, 316–317 α ab. See Fractionation factor plant domestication in, 302 Aardwolf, 298 savanna ecosystems in, 415 Abiotic triggers in angiosperm radiation, urban society development in, 309 155–156 African mammals, environmentally-driven Abutilon theophrasti, 236–238, 243–245 dietary adaptations in, 258–270 Acanthaceae, 192–194 discussion, 269–270 Acclimation, physiological, 449–451 equids, 261–262 Acid rain, 167 giraffids, 266–269 ACR (Antarctic Cold Reversal), 68 methods and materials, 259 Adrar Bous, 306 proboscideans, 262–264 Aerva, 193, 194 suids, 264–266 Africa, 275 tooth enamel as paleoenvironmental re- age of C4 photosynthesis in, 196, 197 corder, 260–261 C3 and C4 grasses in, 221 African rice, 302, 309 C4 monocot distribution in, 222 Afropollis-type pollen, 152 diet of mammals in ancient, 279 Age domestication of plants in, 294, 304– of ice vs. air, 64–65 310 of soils, 19–20 geographical evolution of C4 photosyn- Agriculture, development of, 294 thesis in, 193, 194 Aizoaceae, 193, 194 glacial periods and C4 expansion in, Albedo effects, 235 223 Albian Age, 134, 136, 137, 157 hominins in, 294–300, 300 Alert station, 86 509 510 Index Algae, 189 and environmental trends/events, 136– Alkaloids, 478–479 140 Alkenone-based estimates of past CO2 material and methods, 140–142 levels, 35, 45–56 and other abiotic triggers in angio- and errors in ∆ε, 49–52 sperm radiation, 155–156 and isotopic biogeochemistry of and plant fossil record evidence, 153– alkenone-producing organisms, 39– 155 40 results and discussion, 142–158 measured properties, 45–48 vegetation composition during Creta- Miocene, estimates for, 54 ceous, 142–146 Paleozoic studies, 54–56 Animals, domestication of, 301 and phosphate concentrations, 51–54 Annual plants, 420 propagation of errors in calculation of, Anomalous biospheric flux (Fano,bio), 94, 48–49 96, 97, 101, 102, 104, 105, 107 sediment test of alkenone method, 43, Anomalous oceanic flux (Fano,oce), 94, 101, 45, 46 102, 104, 105, 107 Alkenones, 35, 39–40, 45 Antarctic Cold Reversal (ACR), 68 Allometry, 237–239 Antarctic ice cores, 330, 332–334 Alternanthera, 193, 194 Antarctic records, 62–63, 65, 66, 68–78, Altitude, 24, 25 84 Amaranthaceae, 189, 192–195, 219 Anthropogenic perturbation of carbon cy- Amaranthus retroflexus, 243–245 cle, 329–331 Amazon basin, 174 Aptian Age, 134, 136, 137, 153, 157 Americas Arabidopsis thaliana, 236–238, 248, 249, domestication of maize in, 310–314 457 humans in, 301 Archaefructus liaoningensis, 134 plant domestication in, 302 Arctic ecosystem, herbivores in. See Her- See also North America; South America bivores in Arctic ecosystem AmeriFlux, 83 Arctic plants, 371–373 Ancient CO2 levels, alkenone-based esti- Arctic stations, 92 mates of, 45–56 Arid and semi-arid ecosystems, 415– See also Alkenone-based estimates of 433 past CO2 levels community responses of, to rising at- Andes mountains, 124, 174, 294, 313 mospheric CO2, 419–424 plant domestication in, 302 geographical evolution of C4 photosyn- Angiosperms thesis in, 193, 194 C4 photosynthesis in, 189–191, 214– and multiple global change factors, 428– 216 431 and C4 photosynthetic evolution, 124 physiological responses of plants from, and dinosaurs, 478–479 416–419 radiation and diversification of, 134– and precipitation, 429 136 and rising atmospheric CO2, 424–428 water conduction in, 150 and temperature, 428–429 Angiosperms and Cretaceous CO2 de- Aridity cline, 133–159 and angiosperm origins, 155–156 causal factors in, 156–158 and C4 adaptations, 220–221 and CO2 fluctuations/trends, 138–140 and C4-photosynthesis evolution, 124, comparative plant ecophysiologic evi- 126, 186, 197–199, 204–206 dence, 146–153 Arizona, 224 Index 511 Asia Body size, 286–287, 374–375, 381–382 C4 monocot distribution in, 222 Bogota basin, 223 geographical evolution of C4 photosyn- Bølling-Allerød period, 68–70 thesis in, 193, 194 Boraginaceae, 148, 192–194 plant domestication in, 302 Bordered pits, 147–149 savanna ecosystems in, 415 Borehole temperatures and climate Asteraceae, 148, 190, 192–194 change, 487–505 Atlantic Ocean, 195 alternative multicentury records, 502– Atmosphere-to-ocean CO2 flux (Fam), 95– 505 96 geothermal data, 489–493 Atmospheric pCO2 model, 23–30 geothermal method, 488–489 Atriplex, 219 meteorological records vs., 496–501 Australia, 136, 193, 194, 415 observations, 493–495 Australopithecines, 297, 299 SGT and SAT comparisons, 501–502 Avena, 236 Borszczowia aralocaspica, 189, 204 BP (Before Present), 301 B Brachiopods, 27 Bagra Formation, 11, 17–19, 21, 22, 25–30 Brachyphyllum, 156 Barakar Formation, 24 Bradley & Jones nth hemisphere tempera- Barbed wire syndrome, 471 ture anomalies, 341 Barley, 294, 301–305, 308, 309 Brassica, 236 Barremian Age, 134 Brassicaceae, 192–195 Base cation supply, 167, 171–175, 179– Breeding season, 370, 378, 379, 386 180 Brent geese, 377, 378 Beech, 457 Bristlecone pine trees, 225 Before Present (BP), 301 Bromus japonicus, 240 Belliolum, 147 Bromus tectorum, 241 Bennettites, 136 Browsing animals, 258–268 Bennettittales, 147 deer and tapirs as, 278 Beohari (India), 16 evolution of, 480 Bern model, 71, 72 giraffids as, 267, 268, 270 Berriasian Age, 146, 157 and Great C3-C4 Transformation, 281, Betulaceae, 147 283–288 Bienertia cycloptera, 189, 204 proboscideans as, 263–264 Bijori Formation, 24 suids as, 264 Bioapatite, 260 Bruniaceae, 155 Biogeochemical models, 140, 409 Bubbia, 147 Biomass production Buluk, 263 above- vs. below-ground, 237–238, 424 Bundle sheath cells, 186–189, 193, 202– allocation of, to reproduction, 238–239 203, 216 and CO2 levels, 248–250 Bush pig, 264 and herbivores, 285, 286 Byrd station, 68, 70, 72–74, 76, 77 and leaf area, 243, 245 in low atmospheric CO2, 235–236 C BIOME4, 224 C37,40 Biome-BGC model, 352, 365, 409 C3 photosynthesis Biospheric exchange flux (Fbio), 93–102, C4 photosynthesis vs., 215, 217–219 104, 105, 108 as CO2-unsaturated biochemical reac- Bison, 278, 472 tion, 416 512 Index C4 photosynthesis, 185–207, 214–229 selection responses of modern plants, as adaptation, 219–221 249–251 age of, 194–197 summary of responses, 252 C3 vs., 215, 217–219 C4 plants ecological factors affecting, 226–228 availability of, 477–478 ecological scenarios for evolution of, defenses in, 476 204–206 and diet of mammals (see African factors promoting origin of, 197–204 mammals, environmentally-driven geographic evolution of, 193–194 dietary adaptations in) during glacial periods, 223–225 domestication of, 303–310 impact of, 185 as food resources, 285–286 and low atmospheric CO2, 198–202, and fossil grazing-mammal teeth, 281 216–219 and human evolution, 293–300 and monocot abundance, 222–228 isotopic discrimination in, 97 multiple evolutions of, 191–193 and low CO2 levels, 234, 242–245 seasonality’s effect on, 225–226 paleobotanical evidence for, 275–277, taxonomic distribution of, 189–191 460 C3 plants pathway dominance in C3 vs., 421–422 availability of, 477–478 photosynthetic pathway of, 122–125 C4 cycle in, 189 seasonality’s impact on growth of, 225– and CO2 compensation point, 201, 202 226 defenses in, 476 Caeca length, 385 and diet of mammals (see African Caffeine, 471 mammals, environmentally-driven Calcareous glebules, 17, 19 dietary adaptations in) Calcareous rhizocretions, 12, 17 domestication of, 301–303 Calcic paleosols, 11, 12 evolution of, at low CO2, 246–251 Calcium silicates, weathering of, 176–178 as food resources, 285–286 Caliche carbonate analyses, 224 and fossil grazing-mammal teeth, 281 California, 196, 226 growth of, at low atmospheric CO2, Calligonum, 193, 194 235–236 CAM. See Crassulacean Acid Metabolism and human evolution, 294 Cameroon, 223 isotopic discrimination in, 97–98 Campanian Age, 134, 137, 138, 140 in low atmospheric CO2, 198 Canada, 180, 375, 376 and low CO2 levels, 234, 242–245 Canada goose, 380–385 paleobotanical evidence for, 275–277, Canadian model scenario, 407, 408 460 Canopy conductance, 404, 406 pathway dominance in C4 vs., 421–422 Canopy productivity index (CPI), 448 photorespiration vs. photosynthesis in, Cape Kumukahi, 86, 92 217 Capparales, 148 photosynthetic pathway of, 122–125 Caprifoliaceae, 147, 148 seasonality’s impact on growth of, 225– Carbon allocation, 238–239, 446–449 226 Carbon assimilation rate, 243, 244 See also C3 plants, low CO2 and evolu- Carbon conservation, 202 tion of Carbon cycle, ice core data of C3 plants, low CO2 and evolution of, 246– anthropogenic perturbation of, 329–346 252 double deconvolution modeling of, genetic variation of modern plants, 247– 338, 340–345 249 forward modeling of, 334–338 Index 513 single deconvolution modeling of, 338, and isotopic discrimination by terres- 339 trial vegetation, 97–101 Carbon cycle models, 138–140 and organic burial rate, 5 Carbon cycle(s), 1–3 and short-term variability in global car- in arid and semi-arid ecosystems, 424– bon cycle, 107 426 13C fractionation, 85 GEOCARB model of, 3–5 Cenomanian Age, 136, 137, 140, 146, geochemical model of, 115 153 processes affecting, 468–469 Cenozoic Era short-term variability in the global, 107 horses in (see Fossil horses, effect of Carbon dioxide (CO2) atmospheric CO2 on) global fluxes in levels of, 101–106 paleobotanical evidence for C3 and C4 as plant resource, 232–233 plants during, 275–277 Carbon flow (during marine photosyn- Central America thetic carbon fixation), 36 domestication of plants in, 294 Carbon isotope fractionation glacial periods and C4 expansion in, See Fractionation of carbon isotopes 223 during photosynthesis seasonality’s impact on plant growth Carbon isotope ratios, 223 in, 226 See also 13C/12C
Recommended publications
  • "National List of Vascular Plant Species That Occur in Wetlands: 1996 National Summary."
    Intro 1996 National List of Vascular Plant Species That Occur in Wetlands The Fish and Wildlife Service has prepared a National List of Vascular Plant Species That Occur in Wetlands: 1996 National Summary (1996 National List). The 1996 National List is a draft revision of the National List of Plant Species That Occur in Wetlands: 1988 National Summary (Reed 1988) (1988 National List). The 1996 National List is provided to encourage additional public review and comments on the draft regional wetland indicator assignments. The 1996 National List reflects a significant amount of new information that has become available since 1988 on the wetland affinity of vascular plants. This new information has resulted from the extensive use of the 1988 National List in the field by individuals involved in wetland and other resource inventories, wetland identification and delineation, and wetland research. Interim Regional Interagency Review Panel (Regional Panel) changes in indicator status as well as additions and deletions to the 1988 National List were documented in Regional supplements. The National List was originally developed as an appendix to the Classification of Wetlands and Deepwater Habitats of the United States (Cowardin et al.1979) to aid in the consistent application of this classification system for wetlands in the field.. The 1996 National List also was developed to aid in determining the presence of hydrophytic vegetation in the Clean Water Act Section 404 wetland regulatory program and in the implementation of the swampbuster provisions of the Food Security Act. While not required by law or regulation, the Fish and Wildlife Service is making the 1996 National List available for review and comment.
    [Show full text]
  • Isotopic Dietary Reconstructions of Pliocene Herbivores at Laetoli: Implications for Early Hominin Paleoecology ⁎ John D
    Palaeogeography, Palaeoclimatology, Palaeoecology 243 (2007) 272–306 www.elsevier.com/locate/palaeo Isotopic dietary reconstructions of Pliocene herbivores at Laetoli: Implications for early hominin paleoecology ⁎ John D. Kingston a, , Terry Harrison b a Department of Anthropology, Emory University, 1557 Dickey Dr., Atlanta, GA 30322, United States b Center for the Study of Human Origins, Department of Anthropology, New York University, 25 Waverly Place, New York, NY 10003, United States Received 20 September 2005; received in revised form 1 August 2006; accepted 4 August 2006 Abstract Major morphological and behavioral innovations in early human evolution have traditionally been viewed as responses to conditions associated with increasing aridity and the development of extensive grassland-savanna biomes in Africa during the Plio- Pleistocene. Interpretations of paleoenvironments at the Pliocene locality of Laetoli in northern Tanzania have figured prominently in these discussions, primarily because early hominins recovered from Laetoli are generally inferred to be associated with grassland, savanna or open woodland habitats. As these reconstructions effectively extend the range of habitat preferences inferred for Pliocene hominins, and contrast with interpretations of predominantly woodland and forested ecosystems at other early hominin sites, it is worth reevaluating the paleoecology at Laetoli utilizing a new approach. Isotopic analyses were conducted on the teeth of twenty-one extinct mammalian herbivore species from the Laetolil Beds (∼4.3–3.5 Ma) and Upper Ndolanya Beds (∼2.7–2.6 Ma) to determine their diet, as well as to investigate aspects of plant physiognomy and climate. Enamel samples were obtained from multiple localities at different stratigraphic levels in order to develop a high-resolution spatio-temporal framework for identifying and characterizing dietary and ecological change and variability within the succession.
    [Show full text]
  • Hipparion” Cf
    ©Verein zur Förderung der Paläontologie am Institut für Paläontologie, Geozentrum Wien Beitr. Paläont., 30:15-24, Wien 2006 Hooijer’s Hypodigm for “ Hipparion” cf. ethiopicum (Equidae, Hipparioninae) from Olduvai, Tanzania and comparative Material from the East African Plio-Pleistocene by Miranda A rmour -Chelu 1}, Raymond L. Bernor 1} & Hans-Walter Mittmann * 2) A rmour -C helu , M., Bernor , R.L. & M ittmann , H.-W., 2006. Hooijer’s Hypodigm for “ Hipparion” cf. ethiopicum (Equidae, Hipparioninae) from Olduvai, Tanzania and comparative Material from the East African Plio-Pleistocene. — Beitr. Palaont., 30:15-24, Wien. Abstract cranialen Elemente die Hooijer zu diesem Taxon gestellt hat, auf die er sich bezogen hat oder die in irgendeiner We review here the problematic history of the nomen Beziehung dazu stehen, haben wir wiedergefunden. Selbst “Hipparion”cf. ethiopicum and Hooijer’s efforts to bring zusätzliche Fundstücke aus zeitgleichen Horizonten haben some taxonomic sense to the later Pliocene - Pleistocene wir miteinbezogen, in der Absicht, die Gültigkeit von Eu­ hipparion record. We review his reasoning, and the shifts rygnathohippus cf.“ethiopicum" und seines Verwandten in taxonomic allocation made by him and other equid Eurygnathohippus cornelianus und weiterer Formen, von researchers during the 1970’s. We have relocated many denen Hooijer geglaubt hat, dass sie in einem evolutionären of the postcranial specimens attributed by Hooijer to Zusammenhang mit „ Hipparion“ cf. ethiopicum stehen, “Hipparion” cf. ethiopicum, as well as other specimens zu testen. Wir machen statistische und vergleichende which he referred to, or related to this species. We have Analysen um dieses Hypodigma zu klären. also considered additional specimens from contempo­ raneous horizons, in order to reevaluate the efficacy of Eurygnathohippus cf “ethiopicum” and its apparent rela­ 1.
    [Show full text]
  • Arctic National Wildlife Refuge Volume 2
    Appendix F Species List Appendix F: Species List F. Species List F.1 Lists The following list and three tables denote the bird, mammal, fish, and plant species known to occur in Arctic National Wildlife Refuge (Arctic Refuge, Refuge). F.1.1 Birds of Arctic Refuge A total of 201 bird species have been recorded on Arctic Refuge. This list describes their status and abundance. Many birds migrate outside of the Refuge in the winter, so unless otherwise noted, the information is for spring, summer, or fall. Bird names and taxonomic classification follow American Ornithologists' Union (1998). F.1.1.1 Definitions of classifications used Regions of the Refuge . Coastal Plain – The area between the coast and the Brooks Range. This area is sometimes split into coastal areas (lagoons, barrier islands, and Beaufort Sea) and inland areas (uplands near the foothills of the Brooks Range). Brooks Range – The mountains, valleys, and foothills north and south of the Continental Divide. South Side – The foothills, taiga, and boreal forest south of the Brooks Range. Status . Permanent Resident – Present throughout the year and breeds in the area. Summer Resident – Only present from May to September. Migrant – Travels through on the way to wintering or breeding areas. Breeder – Documented as a breeding species. Visitor – Present as a non-breeding species. * – Not documented. Abundance . Abundant – Very numerous in suitable habitats. Common – Very likely to be seen or heard in suitable habitats. Fairly Common – Numerous but not always present in suitable habitats. Uncommon – Occurs regularly but not always observed because of lower abundance or secretive behaviors.
    [Show full text]
  • The First Occurrence of Eurygnathohippus Van Hoepen, 1930 (Mammalia, Perissodactyla, Equidae) Outside Africa and Its Biogeograph
    TO L O N O G E I L C A A P I ' T A A T L E I I A Bollettino della Società Paleontologica Italiana, 58 (2), 2019, 171-179. Modena C N O A S S. P. I. The frst occurrence of Eurygnathohippus Van Hoepen, 1930 (Mammalia, Perissodactyla, Equidae) outside Africa and its biogeographic signifcance Advait Mahesh Jukar, Boyang Sun, Avinash C. Nanda & Raymond L. Bernor A.M. Jukar, Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, Washington DC 20013, USA; [email protected] B. Sun, Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China; University of Chinese Academy of Sciences, Beijing 100039, China; College of Medicine, Department of Anatomy, Laboratory of Evolutionary Biology, Howard University, Washington D.C. 20059, USA; [email protected] A.C. Nanda, Wadia Institute of Himalayan Geology, Dehra Dun 248001, India; [email protected] R.L. Bernor, College of Medicine, Department of Anatomy, Laboratory of Evolutionary Biology, Howard University, Washington D.C. 20059, USA; [email protected] KEY WORDS - South Asia, Pliocene, Biogeography, Dispersal, Siwalik, Hipparionine horses. ABSTRACT - The Pliocene fossil record of hipparionine horses in the Indian Subcontinent is poorly known. Historically, only one species, “Hippotherium” antelopinum Falconer & Cautley, 1849, was described from the Upper Siwaliks. Here, we present the frst evidence of Eurygnathohippus Van Hoepen, 1930, a lineage hitherto only known from Africa, in the Upper Siwaliks during the late Pliocene. Morphologically, the South Asian Eurygnathohippus is most similar to Eurygnathohippus hasumense (Eisenmann, 1983) from Afar, Ethiopia, a species with a similar temporal range.
    [Show full text]
  • New Insights on the Early Pleistocene Equids from Roca-Neyra (France, Central Europe): Implications for the Hipparion LAD and the Equus FAD in Europe
    Journal of Paleontology, 95(2), 2021, p. 406–425 Copyright © The Author(s), 2020. Published by Cambridge University Press on behalf of The Paleontological Society 0022-3360/21/1937-2337 doi: 10.1017/jpa.2020.99 New insights on the Early Pleistocene equids from Roca-Neyra (France, central Europe): implications for the Hipparion LAD and the Equus FAD in Europe Omar Cirilli,1,2* Raymond L. Bernor,3,4 and Lorenzo Rook2 1Dottorato di Ricerca in Scienze della Terra, Università di Pisa, Via S. Maria 53, 56126 Pisa, Italy <[email protected]> 2Dipartimento di Scienze della Terra, Paleo[Fab]Lab, Università degli Studi di Firenze, Via G. La Pira 4, 50121 Firenze, Italy <lorenzo. rook@unifi.it> 3College of Medicine, Department of Anatomy, Laboratory of Evolutionary Biology, 520 W St. N.W., 20059, Washington D.C., USA <[email protected]> 4Human Origins Program, Department of Anthropology, Smithsonian Institution, 20560, Washington D.C., USA Abstract.—We undertake a redescription of the equid sample from the Early Pleistocene of Roca-Neyra, France. This locality has been recently calibrated at the Pliocene/Pleistocene boundary (2.6 ± 0.2 Ma) and therefore it is of interest for the first appearance of the genus Equus and last appearance of hipparionine horses. The Roca-Neyra equid sample, re- analyzed herein using morphological, morphometrical, and statistical analyses, has revealed the co-occurrence of Plesio- hipparion cf. ?P. rocinantis and Equus cf. E. livenzovensis. The analysis undertaken on several European, African, and Asian “Hipparion” sensu lato species from late Miocene to Early Pleistocene has revealed different remnant Hipparion lineages in the Plio-Pleistocene of Europe: Plesiohipparion, Proboscidippaion, and likely Cremohipparion.
    [Show full text]
  • Literaturverzeichnis
    Literaturverzeichnis Abaimov, A.P., 2010: Geographical Distribution and Ackerly, D.D., 2009: Evolution, origin and age of Genetics of Siberian Larch Species. In Osawa, A., line ages in the Californian and Mediterranean flo- Zyryanova, O.A., Matsuura, Y., Kajimoto, T. & ras. Journal of Biogeography 36, 1221–1233. Wein, R.W. (eds.), Permafrost Ecosystems. Sibe- Acocks, J.P.H., 1988: Veld Types of South Africa. 3rd rian Larch Forests. Ecological Studies 209, 41–58. Edition. Botanical Research Institute, Pretoria, Abbadie, L., Gignoux, J., Le Roux, X. & Lepage, M. 146 pp. (eds.), 2006: Lamto. Structure, Functioning, and Adam, P., 1990: Saltmarsh Ecology. Cambridge Uni- Dynamics of a Savanna Ecosystem. Ecological Stu- versity Press. Cambridge, 461 pp. dies 179, 415 pp. Adam, P., 1994: Australian Rainforests. Oxford Bio- Abbott, R.J. & Brochmann, C., 2003: History and geography Series No. 6 (Oxford University Press), evolution of the arctic flora: in the footsteps of Eric 308 pp. Hultén. Molecular Ecology 12, 299–313. Adam, P., 1994: Saltmarsh and mangrove. In Groves, Abbott, R.J. & Comes, H.P., 2004: Evolution in the R.H. (ed.), Australian Vegetation. 2nd Edition. Arctic: a phylogeographic analysis of the circu- Cambridge University Press, Melbourne, pp. marctic plant Saxifraga oppositifolia (Purple Saxi- 395–435. frage). New Phytologist 161, 211–224. Adame, M.F., Neil, D., Wright, S.F. & Lovelock, C.E., Abbott, R.J., Chapman, H.M., Crawford, R.M.M. & 2010: Sedimentation within and among mangrove Forbes, D.G., 1995: Molecular diversity and deri- forests along a gradient of geomorphological set- vations of populations of Silene acaulis and Saxi- tings.
    [Show full text]
  • Common Plants on the North Slope | the North Slope Borough
    8/17/2020 Common Plants on the North Slope | The North Slope Borough CALENDAR CONTACT Harry K. Brower Jr. , Mayor COMMON PLANTS ON THE NORTH SLOPE Home » Departments » Wildlife Management » Other Topics of Interest » Common Plants on the North Slope Plants are an important subsistence resource for residents across the North Slope. This page provides information on some of the common plants found on the North Slope of Alaska, including plants not used for subsistence. Plant names (common, scientific and Iñupiaq) are provided as well as descriptions, pictures and traditional uses. The resources used for identification are listed here as well as other resources for information on plants. List of Common Plants and others of the North Slope PDF Version Photo Identification of these Common Plants Unknowns - Got any ideas? Please send them to us! Plant Identification and Other Resources Thes pages are a work in progress. If you see any misinformation, misidentifications, or have pictures to add, please contact us. Information on the Iñupiaq names and traditional uses of these plants is especially welcomed. Check out "Unknown" pictures at bottom of page. Thanks! DISCLAIMER: This guide includes traditional uses of plants and other vegetation. The information is not intended to replace the advice of a physician or be used as a guide for self- medication. Neither the author nor the North Slope Borough claims that information in this guide will cure any illness. Just as prescription medicines can have different effects on www.north-slope.org/departments/wildlife-management/other-topics/common-plants-north-slope 1/3 8/17/2020 Common Plants on the North Slope | The North Slope Borough individuals, so too can plants.
    [Show full text]
  • Leeds Thesis Template
    Middle to Late Miocene terrestrial biota and climate by Matthew James Pound M.Sci., Geology (University of Bristol) Submitted in accordance with the requirements for the degree of Doctor of Philosophy The University of Leeds School of Earth and Environment September 2012 - 2 - Declaration of Authorship The candidate confirms that the work submitted is his/her own, except where work which has formed part of jointly-authored publications has been included. The contribution of the candidate and the other authors to this work has been explicitly indicated below. The candidate confirms that appropriate credit has been given within the thesis where reference has been made to the work of others. Chapter 2 has been published as: Pound, M.J., Riding, J.B., Donders, T.H., Daskova, J. 2012 The palynostratigraphy of the Brassington Formation (Upper Miocene) of the southern Pennines, central England. Palynology 36, 26-37. Chapter 3 has been published as: Pound, M.J., Haywood, A.M., Salzmann, U., Riding, J.B. 2012. Global vegetation dynamics and latitudinal temperature gradients during the mid to Late Miocene (15.97 - 5.33 Ma). Earth Science Reviews 112, 1-22. Chapter 4 has been published as: Pound, M.J., Haywood, A.M., Salzmann, U., Riding, J.B., Lunt, D.J. and Hunter, S.J. 2011. A Tortonian (Late Miocene 11.61-7.25Ma) global vegetation reconstruction. Palaeogeography, Palaeoclimatology, Palaeoecology 300, 29-45. This copy has been supplied on the understanding that it is copyright material and that no quotation from the thesis may be published without proper acknowledgement. © 2012, The University of Leeds, British Geological Survey and Matthew J.
    [Show full text]
  • Diplomarbeit
    Diplomarbeit vorgelegt zur Erlangung des Grades eines Diplom-Biologen an der Fakultät für Biologie und Biotechnologie der Ruhr-Universität Bochum Phylogenie der Brandpilzgattung Urocystis von Sascha Lotze-Engelhard Angefertigt im LS Evolution und Biodiversität der Pflanzen, AG Geobotanik Bochum im Dezember 2010 Referent: Prof. Dr. D. Begerow Koreferent: Prof. Dr. R. Tollrian 2 ҅Fungi have a profound impact on global ecosystems. They modify our habitats and are essential for many ecosystem functions. Fungi form soil, recycle nutrients, decay wood, enhance plant growth and cull plants from their environment. They feed us, poison us, parasitize us and cure us. They destroy our crops, homes and libraries, but they also produce valuable biochemicals, such as ethanol and antibiotics. For both practical and intellectual reasons it is important to provide a phylogeny of Fungi on which a classi- fication can be firmly based. ҆ (Blackwell u.a. 2006) Inhaltsverzeichnis 3 Inhaltsverzeichnis Inhaltsverzeichnis ........................................................................................................... 3 Abbildungsverzeichnis .................................................................................................... 6 Tabellenverzeichnis ........................................................................................................ 7 Abkürzungsverzeichnis .................................................................................................. 8 1 Einleitung ............................................................................................................
    [Show full text]
  • A Fossil History of Southern African Land Mammals
    Downloaded from https://www.cambridge.org/core. IP address: 85.187.181.254, on 09 Jun 2020 at 11:41:52, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://www.cambridge.org/core/product/41969EC1E7739F4775954E6ADA8EA036 Downloaded from https://www.cambridge.org/core. IP address: 85.187.181.254, on 09 Jun 2020 at 11:41:52, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://www.cambridge.org/core/product/41969EC1E7739F4775954E6ADA8EA036 A Fossil History of Southern African Land Mammals There is an ever-growing wealth of mammalian fossil material being collected from palaeontological and archaeological sites in southern Africa. This reference provides comprehensive information on the taxonomy and distribution in time and space of all currently recognised southern African fossil mammals. After an introductory background chapter on southern Africa, mammals, sites and dating, the following chapters are presented by epoch, covering the Eocene, Miocene, Pliocene, Pleistocene and Holocene. Individual maps provide information on where in the landscape specific taxa have been found, and a comprehensive index lists all the fauna and site locations. It ends with a chapter on how the book can be used, and lines of future research. Collecting a vast amount of information together in an accessible format, this is an essential reference for non-specialist taxonomists and palaeontologists, as well as for those using fossil data for other applications, such as archaeology, neontology and nature conservation. This title is also available as Open Access on Cambridge Core. D. Margaret Avery is Emeritus Associate of Cenozoic Studies at Iziko Museums of South Africa, and Honorary Researcher at the Evolutionary Studies Institute at the University of Witwatersrand.
    [Show full text]
  • Perissodactyla, Mammalia) from the Late Miocene of China
    Rivista Italiana di Paleontologia e Stratigrafia (Research in Paleontology and Stratigraphy) vol. 124(1): 1-22. March 2018 SIVALHIPPUS PTYCHODUS AND SIVALHIPPUS PLATYODUS (PERISSODACTYLA, MAMMALIA) FROM THE LATE MIOCENE OF CHINA BOYANG SUN1,2,4, XIAOXIAO ZHANG1,2,3, YAN LIU1 & RAYMOND L. BERNOR⁴ 1Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044. 2University of Chinese Academy of Sciences, Beijing 100039. 3Tianjin Natural History Museum, Tianjin 300201. 4Corresponding Author. College of Medicine, Department of Anatomy, Laboratory of Evolutionary Biology, Howard University, Washington D.C. 20059. E-mail: [email protected]. To cite this article: Sun B., Zhang X., Liu Y. & Bernor R.L. (2018) - Sivalhippus ptychodus and Sivalhippus platyodus (Perissodactyla, Mammalia) from the Late Miocene of China. Riv. It. Paleontol. Strat., 124(1): 1-22. Keywords: Sivalhippus ptychodus; Sivalhippus platyodus; late Miocene; Evolution; Biogeography. Abstract. Herein, the authors report on skulls, mandibles and postcranial specimens of two species of Chinese Sivalhippus, S. ptychodus and S. platyodus. We frame our description and analyses within the context of newly described characters of the cheek teeth of Hippotherium from the Pannonian C of the Vienna Basin, the oldest and most primitive Old World hipparions. Our report includes original skull, mandibular and limited postcranial ma- terial of Sivalhippus ptychodus and skulls and dentitions of Sivalhippus platyodus from the Paleontological Museum of Uppsala (PMU, Uppsala, Sweden), the American Museum of Natural History (AMNH, New York, USA) and the Licent Collection in Tianjin Natural History Museum (Tianjin, China). The skull, maxillary and mandibular material we attribute to Sivalhippus ptychodus and Sivalhippus platyodus exhibit some primitive features for Old World hipparions and synapamorphies of the face and dentition that unite it with the Sivalhippus clade.
    [Show full text]