Aboriginal People See Indigenous People Acid Sulfate Soils, 465

Total Page:16

File Type:pdf, Size:1020Kb

Aboriginal People See Indigenous People Acid Sulfate Soils, 465 Cambridge University Press 978-0-521-67982-4 - Environmental Biology Edited by Mike Calver, Alan Lymbery, Jen McComb and Mike Bamford Index More information Index Aboriginal people tissue formation, 259–65 see Indigenous people transportation of sugars, 273 acid sulfate soils, 465 underground organs, 266 agricultural ecosystems, 9–10, 357 water acquisition and use, 270–1 energy inputs, 11 woody habit, 266–8 productivity of, 11 xylem and phloem, 263 slash-and-burn farming, 10 animals, 286–301 agriculture, 154, 356, 401, 403 adaptation to hot, dry environments, 529 Akaike information criterion, 36 adaptation to low nutrients, 532–3 algae, 422 adaptation to aquatic life, 490–1 brown algae, 213 adaptation to cold environments, 525–7 green algae, 212, 422 adaptation to extreme conditions, 507 macroalgae, 422–3 animal ethics, 26 microphytobenthos, 422 bilateral symmetry, 295, 299 phytoplankton, 422 body plans, 294, 297, 299–300 red algae, 211, 445 classifi cation of, 299–300, 336 Alveolata, 213 coelom, 297, 318 amensalism, 390 common problems faced, 289 amino acids, 92 defi nition, 287–9 amoebozoans, 208–9 dietary strategies, 532 amphibians, 348–50 diversity of, 286–301 chytridiomycosis, 221 domestication of, 9, 116 angiosperms, 231, 254–7 embryonic development, 295 apical meristems, 259–65 excretion of nitrogenous wastes, 294 body form, 258–60 features of, 289 characteristics of, 256 the freshwater environment and, 291–2 classifi cation of, 256 hibernation, 525 dispersal, 273–81 impact of urban development, 30–2 fl ower structure, 273–5 infl uence of the environment on, 289–94 fruit and seed dispersal, 278–9 invertebrates, 304–31 fruit development, 278 lifestyles, 294–6 herbaceous habit, 265 the marine environment and, 290–1 identifi cation of, 256–7 mark-release-recapture techniques, internal transport systems, 270–3 370–72 leaves, 268–70 osmotic regulation in, 291 life cycle, 273 radial symmetry, 295, 299 nutrient uptake, 272 removal methods, 369 pollination, 277 sampling populations of, 367, 369, 370–2, reproduction, 273–81 387 seed development, 27–8 sectional planes of, 288–9 seed germination, 279–81 size of, 297–8 sexual reproduction, 275–7 the terrestrial environment and, 293–4 structure of, 257–68 vertebrates, 335–58 structure of wood, 266–8 water loss by evaporation, 293 © in this web service Cambridge University Press www.cambridge.org Cambridge University Press 978-0-521-67982-4 - Environmental Biology Edited by Mike Calver, Alan Lymbery, Jen McComb and Mike Bamford Index More information 654 Index annelids numerical superiority of, 321 see segmented worms reproduction, 324 antibiotic resistance, 191 respiration and circulation, 323 apicomplexans, 215–16 skeleton and locomotion, 322 aquaculture, 419 asexual reproduction, 106, 439 aquatic environments, inland, 452–77 Atherton to the Alps, 579–80 acidity or alkalinity in, 464–5 atmosphere, circulation of, 502 biodiversity and functionality of, 473, 482 ATP (adenosine triphosphate), 59, 66, chemical stratifi cation, 475–7 67, 77 colour, 459–60 Australia consequences of stratifi cation, 475–7 arid ecosystems of, 153, 611 density of, 473 arrival of Aboriginal people, 152–5 dissolved oxygen, 463–4 Atherton to the Alps project, 579–80 diversity of, 453–7 biodiversity, 138, 304 ecology of, 481–97 biomes, 509 environmental factors in, 458–77 Bush Heritage Australia, 566 eutrophication, 472 cave spiders, 395 human impacts on, 461, 462, 465, 467, climate, 507 472–3 climate change, 358 importance of, 482 conservation of vertebrates, 356–8 lakes, 464, 475, 477 declining ecosystems in, 405 lentic environments, 482–91 desert frogs, 529 light, 458 deserts, 152 lotic environments, 491–6 dingo, 380 nutrients, 468–73 effi ciency of water use of fl ora, 271 osmoregulation in, 467 endemic fauna, 507 salinity, 466–7 endemic fl ora, 249 stratifi cation, 473–7 Environment Protection and Biodiversity temperature, 462 Conservation Act 1999 (Cth), 357, 542, thermal stratifi cation, 464–75 545, 572, 573, 604 threats to, 482 environmental awareness and turbidity, 460–61 responsibility, 613 vulnerability to secondary salinisation, 467 eudicotyledons, 256 archaea, 185–6 extinctions, 610 cell walls, 185 extinctions of Australian fl ora, 249, 357 plasma membranes, 185 fauna of, 354, 507–8, 513 tRNA, 185 feral pigs, 108 Archaeplastida, 209–212 fi re, 153, 357, 402–3, 501 chloroplastids (green algae), 212 fl oods and droughts, 493 glaucophytes, 211 fl ora of, 507 rhodophyceae (red algae), 211 fossil record, 152 Armistead, Rodney, 526 fossils, 336 arthropods, 321–4 Gondwanalink, 579–80 body plan, 322 granite rock formations, 519 classifi cation of, 322 grasslands, 513 excretion, 323 habitat degradation and loss, 356 exoskeleton, 322 history of Australian biota, 151–2 feeding and digestion, 323 hunting, 357 nervous and endocrine systems, 323–4 Intertidal Protected Areas, 567 © in this web service Cambridge University Press www.cambridge.org Cambridge University Press 978-0-521-67982-4 - Environmental Biology Edited by Mike Calver, Alan Lymbery, Jen McComb and Mike Bamford Index More information Index 655 introduced species, 198, 249, 357, 363, 378, bioaccumulation, 401 379, 508 biodiversity, 361 isolation of, 506 arguments for conservation of, 561–3, Kakadu wetlands, 452 563–5 Landcare acrivities, 566 defi nitions of, 160 lizards, 351 and urban development, 30 mallee growth form, 528 biodiversity conservation, 155, 598 management of small macropods, 381 biodiversity hotspots, 550 Marine Protected Areas in Victoria, 444 biogeography, 114, 139–44 Martu people of Western Australia, 9 biological control, 198 megafauna, 154, 155 population ecology and, 379–80 Mount Hotham, 526 virally vectored immunocontraception, 198 Murray-Darling river system, 614 biomes, 508–16 National Strategy for the Conservation of changes in, 515–16 Australia’s Biological Diversity, 604 southern and northern views of, 509 nectar-feeding honey possum, 108 BIOPAT, 175 plant adaptation to fi re-prone bioregions, 141 environments, 501 biosphere, 3 Project Aware on the Rocks, 567–8 ecosystems and, 405 rainforest, 151, 153, 511 energy fl ow in, 81–4 reptiles, 352 Birch, Charles, 609 Riversleigh fauna, 153 birds savannas, 513 endothermy, 353 seagrasses, 424 features of, 352–3 sheep, 609 habitats of, 353 smoke and germination, 279–81 migration, 353, 573 soils, 272, 507 parental care of young, 353 susceptibility to ENSO, 507, 527 removal of excess salt, 435 tree ferns, 241 reproduction, 353 wetlands, 490–1 Birds Australia, 616 Australian Conservation Foundation, 444, 566 black-footed rock-wallabies, 28–9 Australian Marine Conservation Society, 444 Blumenbach, Johnan, 335 autotrophs, 67, 82, 187, 389 bogong moths, 601 brine shrimp, 291 bacillariophyta, 213 broad-toothed rat, 37 Bacillus thuringiensis, 198 Brock, Thomas, 182 bacteria, 185–6 Brooks, Shane, 589 cell walls, 185 brown algae, 213, 422 extremophilic, 186 Brown, Robert, 45 plasma membranes, 185 brush-tailed phascogale, 32 thermophilic, 182 bryophytes, 231, 232–3 tRNA, 185 Bush Heritage Australia, 566 bacteriophages, 57 Baltimore, David, 195 Californian condor, 53 basidomycetes, 225 Calvin cycle, 73–6 Bayesian approach to science, 36–8 CAM plants, 75–6, 528 Beadle, Noel, 531 camoufl age, 390–1 bettong, 363, 381 cane toads, 128, 380 Biejerinck, Martinus, 193 Cape Range National Park, 395 © in this web service Cambridge University Press www.cambridge.org Cambridge University Press 978-0-521-67982-4 - Environmental Biology Edited by Mike Calver, Alan Lymbery, Jen McComb and Mike Bamford Index More information 656 Index Capel Wetlands Centre, Western Australia, 481 chondrichthyes, 345–6 captive breeding programs, 113, 126, 331 chordates, 335–58 carbohydrates, 44 defi nition, 336 carbon cycle, 399 features of, 336 Catchment Management Authorities, Victoria, Chromalveolata, 212–16 589–90 apicomplexans, 215–16 cats, and wildlife, 216 bacillariophyta (diatoms), 213 cave spiders, 395 ciliates, 215 cell theory, 43–61, 65–84, 88–109 dinofl agellates, 214 cells oomycetes (water moulds), 213–14 cell cycle, 100 phaeophyceae (brown algae), 213 cell division, 61, 100 chromosomes, 89, 103, 106 characteristics of, 48 see also DNA, genes chloroplasts, 59 chytridiomycosis, 221 control of cell function, 94–9 chytrids, 223–4 cytoskeleton and movement, 60 ciliates, 215 division of, 100–7 citric acid cycle, 78 DNA in chloroplasts and mitochondria, 60 cladistic analysis, 167, 169 energy conversion, 59–60 classifi cation, 160–6, 171 eukaryotic cells, 49–51 domains, 178 fungal cells, 50 evolutionary, 163–5, 166, 171 mitochondrion, 59–60 importance of, 165 nucleus, 56–7 kingdoms, 178 organelles, 56–9 molecular, 301 photosynthesis, 68–76 phylogenetic approach, 171, 300 plant cells, 50 political ramifi cations of, 165 prokaryotic cells, 49 superkingdoms, 178 respiration, 76–81 taxa, 176–7 ribosomes, 60 taxonomy, 161–3 size of cells, 46–8 classifi cation and identifi cation, Chagas disease, 218 160–178 characters, 117 climate analogous, 168, 170 El Niño-Southern Oscillation, 504 ancestral, 169 infl uence of isolation and seasons, 502–3 continuous, 121, 122, 129 landscape and, 503 derived, 169 Code of Practice for the Care and Use of Animals discrete, 121, 122 for Scientifi c Purposes, 26 homologous, 168, 170 commensalism, 390 molecular, 169–70 communities, 380–405 Chase, Martha, 57 animal communities, 387 chemosysthesis, 66 characteristics of, 385–9 China-Australia Migratory Bird Agreement, comparing communities, 387 572, 573 competition, 392 chlorophyll, 72 conservation of, 549 chloroplastids (green algae), 212 and ecosystems, 393–401 life
Recommended publications
  • SUPPLEMENTARY INFORMATION for a New Family of Diprotodontian Marsupials from the Latest Oligocene of Australia and the Evolution
    Title A new family of diprotodontian marsupials from the latest Oligocene of Australia and the evolution of wombats, koalas, and their relatives (Vombatiformes) Authors Beck, RMD; Louys, J; Brewer, Philippa; Archer, M; Black, KH; Tedford, RH Date Submitted 2020-10-13 SUPPLEMENTARY INFORMATION FOR A new family of diprotodontian marsupials from the latest Oligocene of Australia and the evolution of wombats, koalas, and their relatives (Vombatiformes) Robin M. D. Beck1,2*, Julien Louys3, Philippa Brewer4, Michael Archer2, Karen H. Black2, Richard H. Tedford5 (deceased) 1Ecosystems and Environment Research Centre, School of Science, Engineering and Environment, University of Salford, Manchester, UK 2PANGEA Research Centre, School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney, New South Wales, Australia 3Australian Research Centre for Human Evolution, Environmental Futures Research Institute, Griffith University, Queensland, Australia 4Department of Earth Sciences, Natural History Museum, London, United Kingdom 5Division of Paleontology, American Museum of Natural History, New York, USA Correspondence and requests for materials should be addressed to R.M.D.B (email: [email protected]) This pdf includes: Supplementary figures Supplementary tables Comparative material Full description Relevance of Marada arcanum List of morphological characters Morphological matrix in NEXUS format Justification for body mass estimates References Figure S1. Rostrum of holotype and only known specimen of Mukupirna nambensis gen. et. sp. nov. (AMNH FM 102646) in ventromedial (a) and anteroventral (b) views. Abbreviations: C1a, upper canine alveolus; I1a, first upper incisor alveolus; I2a, second upper incisor alveolus; I1a, third upper incisor alveolus; P3, third upper premolar. Scale bar = 1 cm.
    [Show full text]
  • Bandicoot Fossils and DNA Elucidate Lineage Antiquity Amongst Xeric
    www.nature.com/scientificreports OPEN Bandicoot fossils and DNA elucidate lineage antiquity amongst xeric-adapted Received: 31 May 2016 Accepted: 31 October 2016 Australasian marsupials Published: 24 November 2016 Benjamin P. Kear1,2, Ken P. Aplin3 & Michael Westerman4 Bandicoots (Peramelemorphia) are a unique order of Australasian marsupials whose sparse fossil record has been used as prima facie evidence for climate change coincident faunal turnover. In particular, the hypothesized replacement of ancient rainforest-dwelling extinct lineages by antecedents of xeric-tolerant extant taxa during the late Miocene (~10 Ma) has been advocated as a broader pattern evident amongst other marsupial clades. Problematically, however, this is in persistent conflict with DNA phylogenies. We therefore determine the pattern and timing of bandicoot evolution using the first combined morphological + DNA sequence dataset of Peramelemorphia. In addition, we document a remarkably archaic new fossil peramelemorphian taxon that inhabited a latest Quaternary mosaic savannah-riparian forest ecosystem on the Aru Islands of Eastern Indonesia. Our phylogenetic analyses reveal that unsuspected dental homoplasy and the detrimental effects of missing data collectively obscure stem bandicoot relationships. Nevertheless, recalibrated molecular clocks and multiple ancestral area optimizations unanimously infer an early diversification of modern xeric-adapted forms. These probably originated during the late Palaeogene (30–40 Ma) alongside progenitors of other desert marsupials, and thus occupied seasonally dry heterogenous habitats long before the onset of late Neogene aridity. Bandicoots (Peramelemorphia) are a speciose order of Australasian marsupials that appeared early in the evolu- tionary history of Australidelphia1. Most are small to medium sized (up to 5 kg) terrestrial omnivores occupying a spectrum of rainforest to desert habitats2,3.
    [Show full text]
  • A New Family of Diprotodontian Marsupials from the Latest Oligocene of Australia and the Evolution of Wombats, Koalas, and Their Relatives (Vombatiformes) Robin M
    www.nature.com/scientificreports OPEN A new family of diprotodontian marsupials from the latest Oligocene of Australia and the evolution of wombats, koalas, and their relatives (Vombatiformes) Robin M. D. Beck1,2 ✉ , Julien Louys3, Philippa Brewer4, Michael Archer2, Karen H. Black2 & Richard H. Tedford5,6 We describe the partial cranium and skeleton of a new diprotodontian marsupial from the late Oligocene (~26–25 Ma) Namba Formation of South Australia. This is one of the oldest Australian marsupial fossils known from an associated skeleton and it reveals previously unsuspected morphological diversity within Vombatiformes, the clade that includes wombats (Vombatidae), koalas (Phascolarctidae) and several extinct families. Several aspects of the skull and teeth of the new taxon, which we refer to a new family, are intermediate between members of the fossil family Wynyardiidae and wombats. Its postcranial skeleton exhibits features associated with scratch-digging, but it is unlikely to have been a true burrower. Body mass estimates based on postcranial dimensions range between 143 and 171 kg, suggesting that it was ~5 times larger than living wombats. Phylogenetic analysis based on 79 craniodental and 20 postcranial characters places the new taxon as sister to vombatids, with which it forms the superfamily Vombatoidea as defned here. It suggests that the highly derived vombatids evolved from wynyardiid-like ancestors, and that scratch-digging adaptations evolved in vombatoids prior to the appearance of the ever-growing (hypselodont) molars that are a characteristic feature of all post-Miocene vombatids. Ancestral state reconstructions on our preferred phylogeny suggest that bunolophodont molars are plesiomorphic for vombatiforms, with full lophodonty (characteristic of diprotodontoids) evolving from a selenodont morphology that was retained by phascolarctids and ilariids, and wynyardiids and vombatoids retaining an intermediate selenolophodont condition.
    [Show full text]
  • The Oldest Fossil Record of Bandicoots (Marsupialia; Peramelemorphia) from the Late Oligocene of Australia
    Palaeontologia Electronica palaeo-electronica.org The oldest fossil record of bandicoots (Marsupialia; Peramelemorphia) from the late Oligocene of Australia K.J. Travouillon, R.M.D. Beck, S.J. Hand, and M. Archer ABSTRACT Two new late Oligocene representatives of the marsupial order Peramelemorphia (bandicoots and bilbies) from the Etadunna Formation of South Australia are described here. Bulungu muirheadae sp. nov., from Zone B (Ditjimanka Local Fauna [LF]), is rep- resented by several dentaries and isolated upper and lower molars. Bulungu campbelli sp. nov., from Zone C (Ngapakaldi LF), is represented by a single dentary and maxilla. Together, they represent the oldest fossil bandicoots described to date. Both are small (estimated body mass of <250 grams) in comparison to most living bandicoot species and were probably insectivorous based on their dental morphology. They appear to be congeneric with Bulungu palara from Miocene local faunas of the Riversleigh World Heritage Area (WHA), Queensland and the Kutjamarpu LF (Wipajiri Formation) of South Australia. However, the Zone B peramelemorphian appears to be more plesiom- orphic than B. palara in its retention of complete centrocristae on all upper molars. K. J. Travouillon. School of Earth Sciences, University of Queensland, St Lucia, Queensland 4072, Australia [email protected] and School of Biological, Earth and Environmental Sciences, University of New South Wales, New South Wales 2052, Australia R.M.D. Beck. School of Biological, Earth and Environmental Sciences, University of New South Wales, New South Wales 2052, Australia [email protected] S.J. Hand. School of Biological, Earth and Environmental Sciences, University of New South Wales, New South Wales 2052, Australia [email protected] M.
    [Show full text]
  • Palaeoecology of Oligo-Miocene Local Faunas from Riversleigh
    Palaeoecology of Oligo-Miocene Local Faunas from Riversleigh Troy J. M. Myers 2002 i Table of Contents Chapter 1 Introduction............................................................................................ 1 Chapter 2 Marsupial body mass prediction ............................................................ 8 Chapter 3 A review of cenogram methodology and body-size distribution moment statistics in the determination of environmental parameters................ 38 Chapter 4 A discriminant function analysis of recent and fossil Australian faunas 69 Chapter 5 Classification and ordination analysis of selected Riversleigh Local Faunas ............................................................................................... 88 Chapter 6 The Nambaroo-Balbaroo palaeocommunity....................................... 110 Chapter 7 The Litokoala – Muribacinus palaeocommunity ................................. 129 Chapter 8 The Last Minute-Ringtail palaeocommunity ....................................... 146 Chapter 9 The independent Local Faunas ......................................................... 158 The Hiatus Local Fauna ........................................................................................159 The White Hunter Local Fauna.............................................................................162 The Cleft-Of-Ages Local Fauna............................................................................182 The Keith’s Chocky Block Local Fauna...............................................................187
    [Show full text]
  • A Tiny New Marsupial Lion (Marsupialia, Thylacoleonidae) from the Early Miocene of Australia
    Palaeontologia Electronica palaeo-electronica.org A tiny new marsupial lion (Marsupialia, Thylacoleonidae) from the early Miocene of Australia Anna K. Gillespie, Michael Archer, and Suzanne J. Hand ABSTRACT Microleo attenboroughi, a new genus and species of diminutive marsupial lion (Marsupialia: Thylacoleonidae), is described from early Miocene freshwater limestones in the Riversleigh World Heritage Area, northwestern Queensland, Australia. A broken palate that retains incomplete cheektooth rows demonstrates that this new, very small marsupial lion possessed the elongate, trenchant P3 and predominantly subtriangular upper molars characteristic of thylacoleonids, while other features of the premolar sup- port its placement in a new genus. Phylogenetic analysis suggests that Microleo atten- boroughi is the sister taxon to all other thylacoleonids, and that Thylacoleonidae may lie outside Vombatomorphia as the sister taxon of all other wombat-like marsupials including koalas. However, given limited data about the cranial morphology of M. atten- boroughi, Thylacoleonidae is concluded here, conservatively, to be part of the vom- batomorphian clade. This new thylacoleonid brings to three the number of marsupial lion species that have been recovered from early Miocene deposits at Riversleigh and indicates a level of diversity previously not seen for this group. It is likely that the differ- ent size and morphology of the three sympatric taxa reflects niche partitioning and hence reduced competition. Thylacoleonids may have been the dominant arboreal predators of Cenozoic Australia. Anna K. Gillespie*, Palaeontology, Geobiology and Earth Archives (PANGEA) Research Centre, School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney 2052, Australia; [email protected], *corresponding author Michael Archer, Palaeontology, Geobiology and Earth Archives (PANGEA) Research Centre, School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney 2052, Australia; [email protected] Suzanne J.
    [Show full text]
  • Diversity and Systematics of Marsupial Lions from the Riversleigh World Heritage Area and the Evolution of the Thylacoleonidae
    DIVERSITY AND SYSTEMATICS OF MARSUPIAL LIONS FROM THE RIVERSLEIGH WORLD HERITAGE AREA AND THE EVOLUTION OF THE THYLACOLEONIDAE ANNA K GILLESPIE Submitted in fulfilment of the requirements for the degree of Doctor of Philosophy in the School of Biological, Earth and Environmental Sciences, University of New South Wales 2007 i ABSTRACT The fossil record of marsupial lions (family Thylacoleonidae) from Australian Oligo- Miocene deposits is generally poor. Study of new material of this family collected from Oligo-Miocene limestone sediments of the Riversleigh World Heritage Area, northwestern Queensland adds significant new information about previously described species and also indicates a greater diversity of thylacoleonids during this period of geological time. Two new genera and five new species are described. Reassessment of the holotype of the type species of Priscileo, P. pitikantensis, indicates it shows stronger affinities to species of the genus Wakaleo than it does to Priscileo roskellyae. Priscileo is regarded here to be a junior synonym of Wakaleo. The cranium and lower dentition of Priscileo roskellyae show significant morphological differences from species of Wakaleo, and this species is referred to a new genus, Lekaneleo. Distinctive morphological differences are identified in the M3s of Wakaleo oldfieldi and W. vanderleueri, species previously distinguished only by relative size differences in their dentitions. Functional morphological assessment of postcranial remains of species of Wakaleo suggests that they were probably scansorial or arboreal, but does not support a previous hypothesis of a fossorial habit. Cladistic analyses of the interrelationships of marsupial lions support the referral of Priscileo pitikantensis to the genus Wakaleo. The monotypic genus Microleo is the sister-group to all remaining thylacoleonid taxa.
    [Show full text]
  • Forum Comment Doi:10.1130/G32600C.1
    Forum Comment doi:10.1130/G32600C.1 Early to middle Miocene monsoon climate in Australia K.J. Travouillon, M. Archer, and S.J. Hand gests they had not yet evolved in Australia, and that the biota documented School of Biological, Earth and Environmental Sciences, University of in the Riversleigh deposits of this age may well be representative of much New South Wales, New South Wales 2052, Australia of northern Australia. Extensive species overlaps (Travouillon et al., 2006) with the early Miocene Kutjamarpu LF from the Wipijiri Formation in Herold et al. (2011) present a monsoon climate model for the early the Lake Eyre Basin suggests that similar species-rich forest communities to middle Miocene of Australia, which suggests that widespread rainfor- extended into central Australia at this time. est vegetation could not be supported in northern Australia at that time With respect to the suggestion (Herold et al., 2011) that their mod- without a major increase in atmospheric CO2 concentration. They note eling indicates that grasslands may have been present in central and/or that this appears to be at odds with the results of Archer et al. (1994) and northern Australia at this time, Martin (2006), having reviewed all paly- Travouillon et al. (2009) who argue that early and middle Miocene faunas nological evidence from Australia, concluded that there is no evidence for of, for example, Riversleigh in north-western Queensland are indicative of grasslands prior to the Pliocene. at least regional rainforest paleohabitats. We suggest that some aspect of the modeling that led Herold et al. The data used as quantitative climate proxies to calibrate Herold et to conclude that the early to middle Miocene communities of Riversleigh al.’s models require comment.
    [Show full text]
  • 2011Byrneetaljbiog.Pdf
    Journal of Biogeography (J. Biogeogr.) (2011) 38, 1635–1656 SYNTHESIS Decline of a biome: evolution, contraction, fragmentation, extinction and invasion of the Australian mesic zone biota Margaret Byrne1*, Dorothy A. Steane2, Leo Joseph3, David K. Yeates4, Greg J. Jordan2, Darren Crayn5, Ken Aplin3, David J. Cantrill6, Lyn G. Cook7, Michael D. Crisp8, J. Scott Keogh8, Jane Melville9, Craig Moritz10, Nicholas Porch11, J. M. Kale Sniderman12, Paul Sunnucks13 and Peter H. Weston14 1Science Division, Department of Environment ABSTRACT and Conservation, Locked Bag 104, Bentley Aim The mesic biome, encompassing both rain forest and open sclerophyllous Delivery Centre, Perth, WA 6983, Australia, 2School of Plant Sciences and CRC Forestry, forests, is central to understanding the evolution of Australia’s terrestrial biota University of Tasmania, Private Bag 55, and has long been considered the ancestral biome of the continent. Our aims are Hobart, Tas. 7001, Australia, 3Australian to review and refine key hypotheses derived from palaeoclimatic data and the National Wildlife Collection, CSIRO Ecosystem fossil record that are critical to understanding the evolution of the Australian Sciences, GPO Box 284, Canberra, ACT 2601, mesic biota. We examine predictions arising from these hypotheses using Australia, 4Australian National Insect available molecular phylogenetic and phylogeographical data. In doing so, we Collection, CSIRO Ecosystem Sciences, PO Box increase understanding of the mesic biota and highlight data deficiencies and 1700, Canberra, ACT 2601, Australia, fruitful areas for future research. 5Australian Tropical Herbarium, James Cook Location The mesic biome of Australia, along the eastern coast of Australia, and University Cairns Campus, PO Box 4811, in the south-east and south-west, including its rain forest and sclerophyllous, Cairns, Qld 4870, Australia, 6National often eucalypt-dominated, habitats.
    [Show full text]
  • 283049006-Oa
    The pre-Pleistocene fossil thylacinids (Dasyuromorphia: Thylacinidae) and the evolutionary context of the modern thylacine Douglass S. Rovinsky1, Alistair R. Evans2,3 and Justin W. Adams1 1 Department of Anatomy and Developmental Biology, Monash University, Clayton, VIC, Australia 2 School of Biological Sciences, Monash University, Clayton, VIC, Australia 3 Geosciences, Museums Victoria, Melbourne, VIC, Australia ABSTRACT The thylacine is popularly used as a classic example of convergent evolution between placental and marsupial mammals. Despite having a fossil history spanning over 20 million years and known since the 1960s, the thylacine is often presented in both scientific literature and popular culture as an evolutionary singleton unique in its morphological and ecological adaptations within the Australian ecosystem. Here, we synthesise and critically evaluate the current state of published knowledge regarding the known fossil record of Thylacinidae prior to the appearance of the modern species. We also present phylogenetic analyses and body mass estimates of the thylacinids to reveal trends in the evolution of hypercarnivory and ecological shifts within the family. We find support that Mutpuracinus archibaldi occupies an uncertain position outside of Thylacinidae, and consider Nimbacinus richi to likely be synonymous with N. dicksoni. The Thylacinidae were small-bodied (< ~8 kg) unspecialised faunivores until after the ~15–14 Ma middle Miocene climatic transition (MMCT). After the MMCT they dramatically increase in size and develop adaptations to a hypercarnivorous diet, potentially in response to the aridification of Submitted 27 March 2019 the Australian environment and the concomitant radiation of dasyurids. This fossil Accepted 10 July 2019 history of the thylacinids provides a foundation for understanding the ecology of the Published 2 September 2019 modern thylacine.
    [Show full text]
  • Palaeoecology of Oligo-Miocene Macropodoids Determined from Craniodental and Calcaneal Data
    Janis, C. , Damuth, J., Travouillon, K., Figueirido, B., Archer, M., & Hand, S. (2016). Palaeoecology of Oligo-Miocene macropodoids determined from craniodental and calcaneal data. Memoirs of Museum Victoria, 74, 209-232. https://museumvictoria.com.au/about/books-and- journals/journals/memoirs-of-museum-victoria/2010-2019/2016-vol- 74-special-issue-in-honour-of-dr-thomas-h-rich/janis-damuth- travouillon-figueirido-hand-and-archer/ Publisher's PDF, also known as Version of record Link to publication record in Explore Bristol Research PDF-document This is the final published version of the article (version of record). It first appeared online via Museum Victoria at https://museumvictoria.com.au/about/books-and-journals/journals/memoirs-of-museum-victoria/2010-2019/2016- vol-74-special-issue-in-honour-of-dr-thomas-h-rich/janis-damuth-travouillon-figueirido-hand-and-archer/. Please refer to any applicable terms of use of the publisher. University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ Memoirs of Museum Victoria 74: 209–232 (2016) Published 2016 ISSN 1447-2546 (Print) 1447-2554 (On-line) http://museumvictoria.com.au/about/books-and-journals/journals/memoirs-of-museum-victoria/ Palaeoecology of Oligo-Miocene macropodoids determined from craniodental and calcaneal data CHRISTINE M. JANIS1,2,*, JOHN DAMUTH3, KENNY J. TRAVOUILLON4,5, BORJA FIGUEIRIDO6, SUZANNE J. HAND7, AND MICHAEL ARCHER7 1 Department of Ecology and Evolutionary Biology, Brown University, Providence, RI 02912, USA (christine_janis@ Brown.edu) 2 School of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK 3 Department of Ecology, Evolution and Marine Biology, University of California Santa Barbara, Santa Barbara, CA 93106, USA ([email protected]) 4 School of Earth Sciences, University of Queensland, St.
    [Show full text]
  • Marsupialia; Diprotodontia) from Northern and Central Australia
    Palaeontologia Electronica palaeo-electronica.org Miminipossum notioplanetes, a Miocene forest-dwelling phalangeridan (Marsupialia; Diprotodontia) from northern and central Australia Michael Archer, Pippa Binfield, Suzanne J. Hand, Karen H. Black, Phillip Creaser, Troy J. Myers, Anna K. Gillespie, Derrick A. Arena, John Scanlon, Neville Pledge, and Jenni Thurmer ABSTRACT Miminipossum notioplanetes represents a new Early/Middle Miocene family (Miminipossumidae) of phalangeridan possums recovered from the Two Trees Local Fauna from the Riversleigh World Heritage area in northwestern Queensland and the Kutjamarpu Local Fauna of the Tirari Desert in northern South Australia. Because of widespread convergence in key features of P3 and M1 among phalangeridan families, the interfamilial relationships of Miminipossumidae are uncertain. The age of the Kutja- marpu Local Fauna has been in doubt with estimates ranging from Late Oligocene to Middle Miocene. The new taxon raises to 15 the number of taxa in the Kutjamarpu Local Fauna that are shared with both Riversleigh’s Faunal Zone B (Early Miocene) and Riversleigh’s Faunal Zone C (Middle Miocene) assemblages. Although there is rel- atively little biocorrelative support for the estimate of a Late Oligocene age, doubt remains about whether the age is more likely to be Early or Middle Miocene. In terms of palaeoenvironmental implications, because both Riversleigh’s Early and Middle Mio- cene assemblages have been concluded to have accumulated in temperate, wet, spe- cies-rich lowland forests, the same or similar Early/Middle Miocene palaeoenvironments may well have extended into central Australia at the time when the Kutjamarpu assemblage was accumulating. Michael Archer. Palaeontology, Geobiology and Earth Archives Research Centre (PANGEA), School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney 2052, Australia; [email protected] Pippa Binfield.
    [Show full text]