Coastal Foredune Vegetation in Wellington Conservancy
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Classifications
Classifications rt.code.desc Classifications Code Classifications rt.code.base Akitio River Scheme - River Maintenance RC Direct Benefit AREA Akitio River Scheme - Contributor CN Contributor AREA Ashhurst Scheme - Flood Protection AC Flooding Urban CAPITAL Ashhurst Scheme - Flood Protection SUIP AN Annual Charge TARGET Ashhurst Scheme - Lower Stream Maintenance AL Channel Maintenance High AREA Ashhurst Scheme - Upper Stream Maintenance AU Channel Maintenance Low AREA Eastern Manawatu - Lower River Maintenance EL Channell Maintenane High AREA Eastern Manawatu - Upper River Maintenance EU Channell Maintenance low AREA Eastern Manawatu River Scheme - Contributor CN Contributor AREA Eastern Manawatu River Scheme - Indirect IN Indirect Benefit TARGET Forest Road Drainage Scheme A High Benefit AREA Forest Road Drainage Scheme B Medium Benefit AREA Forest Road Drainage Scheme C Moderate Benefit AREA Forest Road Drainage Scheme D Low Benefit AREA Forest Road Drainage Scheme E Minor Benefit AREA Forest Road Drainage Scheme F Indirect Benefit AREA Foxton East Drainage Scheme D1 High Benefit AREA Foxton East Drainage Scheme D2 Medium Benefit AREA Foxton East Drainage Scheme D3 Moderate Benefit AREA Foxton East Drainage Scheme D4 Minor Benefit AREA Foxton East Drainage Scheme D5 Low Benefit AREA Foxton East Drainage Scheme SUIP AC Annual Charge TARGET Foxton East Drainage Scheme Urban U1 Urban CAPITAL Haunui Drainage Scheme A Direct Benefit CAPITAL Himatangi Drainage Scheme A High Benefit AREA Himatangi Drainage Scheme B Medium Benefit AREA Himatangi -
Grass Genera in Townsville
Grass Genera in Townsville Nanette B. Hooker Photographs by Chris Gardiner SCHOOL OF MARINE and TROPICAL BIOLOGY JAMES COOK UNIVERSITY TOWNSVILLE QUEENSLAND James Cook University 2012 GRASSES OF THE TOWNSVILLE AREA Welcome to the grasses of the Townsville area. The genera covered in this treatment are those found in the lowland areas around Townsville as far north as Bluewater, south to Alligator Creek and west to the base of Hervey’s Range. Most of these genera will also be found in neighbouring areas although some genera not included may occur in specific habitats. The aim of this book is to provide a description of the grass genera as well as a list of species. The grasses belong to a very widespread and large family called the Poaceae. The original family name Gramineae is used in some publications, in Australia the preferred family name is Poaceae. It is one of the largest flowering plant families of the world, comprising more than 700 genera, and more than 10,000 species. In Australia there are over 1300 species including non-native grasses. In the Townsville area there are more than 220 grass species. The grasses have highly modified flowers arranged in a variety of ways. Because they are highly modified and specialized, there are also many new terms used to describe the various features. Hence there is a lot of terminology that chiefly applies to grasses, but some terms are used also in the sedge family. The basic unit of the grass inflorescence (The flowering part) is the spikelet. The spikelet consists of 1-2 basal glumes (bracts at the base) that subtend 1-many florets or flowers. -
Jervis Bay Territory Page 1 of 50 21-Jan-11 Species List for NRM Region (Blank), Jervis Bay Territory
Biodiversity Summary for NRM Regions Species List What is the summary for and where does it come from? This list has been produced by the Department of Sustainability, Environment, Water, Population and Communities (SEWPC) for the Natural Resource Management Spatial Information System. The list was produced using the AustralianAustralian Natural Natural Heritage Heritage Assessment Assessment Tool Tool (ANHAT), which analyses data from a range of plant and animal surveys and collections from across Australia to automatically generate a report for each NRM region. Data sources (Appendix 2) include national and state herbaria, museums, state governments, CSIRO, Birds Australia and a range of surveys conducted by or for DEWHA. For each family of plant and animal covered by ANHAT (Appendix 1), this document gives the number of species in the country and how many of them are found in the region. It also identifies species listed as Vulnerable, Critically Endangered, Endangered or Conservation Dependent under the EPBC Act. A biodiversity summary for this region is also available. For more information please see: www.environment.gov.au/heritage/anhat/index.html Limitations • ANHAT currently contains information on the distribution of over 30,000 Australian taxa. This includes all mammals, birds, reptiles, frogs and fish, 137 families of vascular plants (over 15,000 species) and a range of invertebrate groups. Groups notnot yet yet covered covered in inANHAT ANHAT are notnot included included in in the the list. list. • The data used come from authoritative sources, but they are not perfect. All species names have been confirmed as valid species names, but it is not possible to confirm all species locations. -
02 Whole.Pdf (9.122Mb)
Copyright is owned by the Author of the thesis. Pennission is given for a copy to be downloaded by an individual for the purpose of research and private study only. The thesis may not be reproduced elsewhere without the pennission of the Author. PALEOENVIRONMENTAL ANALYSIS OF QUATERNARY STRATA IN THE LEVIN AREA A thesis presented in partial fulfilment of the requirements for the degree of Master of Science in Quaternary Science at Massey University ALAN HENRY SEWELL 1991 ·-~-. - - ,.-.··,_·.:·.-· Frontispiece: Pencil sketch looking north from the Tararua foothills, south-east of Potts Hill, across the Tokomaru Marine Terrace and Manawatu River flood plain beyond. ABSTRACT Marine transgression during the Last Interglacial resulted in widespread inundation of the southern Manawa tu area. The Otaki Formation constitutes the relatively thick blanket of predominantly marine sand deposited at the height of the transgression and is now exposed in a partially dissected marine terrace abutting the Tararua Range. Sedimentation was controlled by basement block faulting related to a regional strike-slip tectonic regime on the south eastern margin of the South Wanganui Basin. Wave-induced longshore currents from the north-west supplied abundant sediment to the coast. North-east of Levin the Kairanga Trough, occupying a north-east-trending structural depression between uplifted basement blocks, formed the centre of an embayment during the transgression. Tide-dominated depositional processes predominated around the margins of the embayment. In the Forest Lakes area, the absence of seaward barriers resulted in an open wave-dominated coastline. Between Ohau and Shannon mixed wave/tide processes predominated. Stabilisation of sea level resulted in shoreline progradation which was especially marked south of Levin where a dune belt formed, mantling the coastal cliff and later migrating inland. -
Ecology, Habitat and Growth
Technical Article No. 7.1 - ecology, habitat and growth INTRODUCTION Spinifex (Spinifex sericeus R.Br.) is the major Spinifex often occurs with other indigenous sand indigenous sand dune grass that occurs on binding species on the foredune including pingao foredunes throughout most of the North Island (Ficinia spiralis), nihinihi (sand convolvulus, and the upper part of the South Island. Sometimes Calystegia soldanella), and hinarepe (sand referred to as silvery sand grass, or kowhangatara, tussock, Poa billardierei). it is the dominant sand binding plant on the seaward face of the foredune where its long trailing runners and vigorous growth make it an ideal sand dune stabiliser. In many North Island dunes, spinifex forms a near continuous colony for long stretches of sandy coastline. Technical Handbook Section 7: Native vegetation on foredunes Technical habitat and growth 7.1 Spinifex - ecoloogy, Article No. 7.1 - Spinifex - ecology, habitat and growth PLANT DESCRIPTION Spinifex is a stout perennial grass with strong on both surfaces (McDonald, 1983). At intervals of creeping runners or stolons. Leaves are usually 10-15 cm, new nodes are formed from which roots 5-10 mm wide and up to 38 cm long (Craig, 1984). emerge, take root and eventually a discrete plant The stolons can be up to 20 m long with internodes will form where there is sufficient space that is up to 38 cm long. Each node produces adventitious independent of the original stolon (Hesp, 1982). roots and upright, silvery green leaves that are hairy Vigorous spinifex on a foredune showing the upright silvery green leaves and long creeping runners or stolons that spread rapidly to occupy bare sand. -
Flora of Stockton/Port Hunter Sandy Foreshores
Flora of the Stockton and Port Hunter sandy foreshores with comments on fifteen notable introduced species. Petrus C. Heyligers CSIRO Sustainable Ecosystems, Queensland Biosciences Precinct, 306 Carmody Road, St. Lucia, Queensland 4067, AUSTRALIA. [email protected] Abstract: Between 1993 and 2005 I investigated the introduced plant species on the Newcastle foreshores at Stockton and Macquaries Pier (lat 32º 56’ S, long 151º 47’ E). At North Stockton in a rehabilitated area, cleared of *Chrysanthemoides monilifera subsp. rotundata, and planted with *Ammophila arenaria interspersed with native shrubs, mainly Acacia longifolia subsp. sophorae and Leptospermum laevigatum, is a rich lora of introduced species of which *Panicum racemosum and *Cyperus conglomeratus have gradually become dominant in the groundcover. Notwithstanding continuing maintenance, *Chrysanthemoides monilifera subsp. rotundata has re-established among the native shrubs, and together with Acacia longifolia subsp. sophorae, is important in sand stabilisation along the seaward edge of the dune terrace. The foredune of Little Park Beach, just inside the Northern Breakwater, is dominated by Spinifex sericeus and backed by Acacia longifolia subsp. sophorae-*Chrysanthemoides monilifera subsp. rotundata shrubbery. In places the shrubbery has given way to introduced species such as *Oenothera drummondii, *Tetragonia decumbens and especially *Heterotheca grandilora. At Macquaries Pier *Chrysanthemoides monilifera subsp. rotundata forms an almost continuous fringe between the rocks that protect the pier against heavy southerlies. However, its presence on adjacent Nobbys Beach is localised and the general aspect of this beach is no different from any other along the coast as it is dominated by Spinifex sericeus. Many foreign plant species occur around the sandy foreshores at Port Hunter. -
Co-Extinction of Mutualistic Species – an Analysis of Ornithophilous Angiosperms in New Zealand
DEPARTMENT OF BIOLOGICAL AND ENVIRONMENTAL SCIENCES CO-EXTINCTION OF MUTUALISTIC SPECIES An analysis of ornithophilous angiosperms in New Zealand Sandra Palmqvist Degree project for Master of Science (120 hec) with a major in Environmental Science ES2500 Examination Course in Environmental Science, 30 hec Second cycle Semester/year: Spring 2021 Supervisor: Søren Faurby - Department of Biological & Environmental Sciences Examiner: Johan Uddling - Department of Biological & Environmental Sciences “Tui. Adult feeding on flax nectar, showing pollen rubbing onto forehead. Dunedin, December 2008. Image © Craig McKenzie by Craig McKenzie.” http://nzbirdsonline.org.nz/sites/all/files/1200543Tui2.jpg Table of Contents Abstract: Co-extinction of mutualistic species – An analysis of ornithophilous angiosperms in New Zealand ..................................................................................................... 1 Populärvetenskaplig sammanfattning: Samutrotning av mutualistiska arter – En analys av fågelpollinerade angiospermer i New Zealand ................................................................... 3 1. Introduction ............................................................................................................................... 5 2. Material and methods ............................................................................................................... 7 2.1 List of plant species, flower colours and conservation status ....................................... 7 2.1.1 Flower Colours ............................................................................................................. -
3619-Northern Ohariu Fault: Earthquake Hazard Assessment of A
wp?:4·i .2. 444"'ll,Im6%fi.j - , le..Ibd*di.I 5*fe NORTHERN OHARIU FAULT: 4 /2 ** 4 :ty Earthquake Hazird Assessment of a Newly I . 46. .;1/*if. Discovered Actlve Strike-Slip Fault in Horowhenua 4,2 83 Alan Palmerl & Russ¥an Dissen* 1Soil and Earth Sciences Group, Instii of Natural' 1€sour, Massey University, Private Bag 11-222, Palmerston NorthW a. [email protected] Institute of Geological & Nuclear Sciences, PO Box 30-368 Lower Hutt, NZ 1&6./AL'Ime [email protected] A#jPlibll+A '\ R Prepared for a EQC Research Foundation Project 97/263 April, 2002 1.0 TECHNICAL ABSTRACT The Ohariu fault, discovered about 100 years ago, extends northeastward from o ffshore o f the Wellington south coast near Tongue Point through Porirua towards Paraparaumu. It has long been thought that the Ohariu fault "dies out" to the north in the Waikanae/Otaki area as a series of splays. However, in 1996 we discovered that the pronounced, 60 km long, NNE- to NE-trending topographic lineation that runs just inland of, and parallel to, the western flank of the northern portion of the Tararua Range between Otaki and Palmerston North is an active, right-lateral strike-slip fault. We name this newly discovered fault the Northern Ohariu fault because it appears to be the northern, along-strike, continuation of the Ohariu fault. Collectively the Ohariu and Northern Ohariu faults define a major active strike-slip fault that has a total length in excess of 130 km. Offset geomorphic features such as alluvial terrace risers and valley margins, and estimated ages based on soil and loess stratigraphy are used to constrain the timing, amount, and rate of movement on the fault. -
Three Public Bus Services in the Horowhenua District?
Palmerston North Himatangi Did you know Rangiotu Longburn Foxton Beach Horizons Regional Bainesse Tiakiahuna Council provides Foxton Waitarere three public bus Shannon services in the Levin Manakau Horowhenua Otaki District? Waikanae SURVEY INSIDE Have you taken a trip on any of these bus services? Fill out the survey inside Yes and tell us about your experience Fill out the survey inside and tell us what No would make it easier for you to do so Find out more about the Plus services and try them out For more information visit www.horizons.govt.nz or freephone Horizons on 0508 800 800 CURRENT TIMETABLES LEVIN TO WAIKANAE BUS SERVICE* * A minor timetable change has taken place as of 15 July 2018 Greater Wellington has made a slight adjustment to their train timetable and as result we have adjusted the bus departure times. (i.e Depart Levin changed from 9.30am to 9.20am) This operational change ensures passengers still have the opportunity to connect to the train travelling south. DEPARTS LEVIN Tuesday/Thursday Morning Time as of 15 July 2018 Location Depart Levin 9.20 am Te Takeretanga o Kura-hau-pō, Bath Street, Levin Depart Manakau 9.38 am Honi Taipua Street (opposite Manakau Bowling & Sports Club) Depart Otaki 9.51am Intercity Bus Shelter, Main Highway Otaki Arrive Waikanae 10.05am Train Station, Waikanae DEPARTS WAIKANAE Depart Waikanae 2.45 pm Train Station, Waikanae Depart Otaki 3.11 pm Intercity Bus Shelter, Main Highway Otaki Depart Manakau 3.24 pm Honi Taipua Street (opposite Manakau Bowling & Sports Club) Arrive Levin 3.38 pm -
Seed Production and Processing of the Indigenous Coastal Sand-Binding Plant Spinifex Sericeus 99
Seed Production and Processing of the Indigenous Coastal Sand-Binding Plant Spinifex sericeus 99 Seed Production and Processing of the Indigenous Coastal Sand-Binding Plant Spinifex sericeus © Robert Southward Institute of Natural Resources, Massey University, Private Bag 11-222, Palmerston North Email: [email protected] Spinifex sericeus R.Br is an important indigenous sand-binding grass growing on coastal foredunes throughout the North Island and northern South Island of New Zealand. Utilising seed rather than vegetative propagation techniques has typically been more successful in establishing plants for sand dune sta- bilisation in New Zealand. Since 1998, caryopses (naked “seeds”) have been mechanically extracted at Massey University from 43 collections (or sub-col- lections) sent by interested parties from 16 North Island beaches. Although most collections received were from five beaches of the south western coast of the North Island (25), especially Hokio beach near Levin, a number were also received from a further five west coast and six east coast beaches. Weights of extracted whole seeds ranged from as little as 2.9 g (approximately 210 seeds) to 142 g (approximately 11,270 seeds) per “packed” fertiliser bag of spinifex seedheads (ave. 51.1 g, about 3790 seeds). The ten highest yields obtained were collections from Hokio (8), Foxton (1), and Himatangi (1) beaches. Low yields were more typical of east coast beaches, although the lowest yields recorded were from the west coast beach of Oakura, near New Plymouth. Fungal smut or rodents were identified as causes of low seed yield in some cases. Thousand seed weight varied from 11.7 g (Patea) to 15.6 g (Muriwai). -
The Role of Currents in the Dispersal of Introduced Seashore Plants Around Australia
The role of currents in the dispersal of introduced seashore plants around Australia Petrus C. Heyligers CSIRO Sustainable Ecosystems, Queensland Biosciences Precinct, University of Queensland, 306 Carmody Road, St. Lucia Qld 4067. Email: [email protected] Abstract: The aim of this study was to assess the role of currents in the dispersal of seashore species with buoyant propagules. Four introduced species which have now attained a wide distribution in southern and eastern Australia were used as indicators: Cakile edentula, Cakile maritima (Brassicaceae), Euphorbia paralias (Euphorbiaceae) and Arctotheca populifolia (Asteraceae). None arrived in Australia unaided, as all early collection localities are near ports and early long-distance dispersal within Australia was often due to shipping. Buoyancy and viability of propagules were tested to assess dispersal and colonisation potential. Propagule spread was analysed using information from herbarium specimens and fieldwork. A progression of herbarium specimen collection dates could often be explained by regional current regimes, as revealed by stranding locations of drift bottles and drift cards. The eastward spread of Euphorbia paralias from King George Sound, Western Australia, correlated well with stranding patterns of drift bottles released south of the Sound. The colonisation by Arctotheca populifolia of the southern extremity of the Eyre Peninsula and the south-east of South Australia was achieved through fruits carried from Western Australia by the Leeuwin Current. These and other congruencies between patterns of spread and the results of drifter releases are analysed and discussed. Cunninghamia (2007) 10(2): 167–188 We know remarkably little about long-distance transport of the propagules in water, although there are reports of strandline plants having travelled great distances (Guppy 1906; Ridley 1930). -
Host Range Testing of Tetramesa Romana and Rhizaspidiotus Donacis
The host ranges of Tetramesa romana and Rhizaspidiotus donacis, potential control agents for giant reed, Arundo donax. Introduction Arundo donax, or giant reed, is a tall, woody grass that has been proposed as a target for biological control in New Zealand. It originates from Eurasia, but has become a serious environmental weed in many southern hemisphere countries and in North America. A global account of its distribution, impact and management can be found here: http://www.issg.org/database/species/ecology.asp?si=112 . Although still of limited distribution in New Zealand, it is consider to be a serious future threat to wetlands, riparian areas and other habitats. More information about its potential impact in New Zealand can be found in the application, or can be accessed here: http://www.landcareresearch.co.nz/science/plants-animals- fungi/plants/weeds/biocontrol/approvals/current-applications . Two control agents have been selected for introduction to New Zealand 1. Arundo wasp, Tetramesa romana Walker (Hymenoptera: Eurytomidae) 2. Arundo scale, Rhizaspidiotus donacis (Leonardi) (Hemiptera: Diaspididae) Arundo wasp lays its eggs into the shoots of giant reed, inducing a gall. Larvae feed within the shoot gall. Growth can be severely stunted and with sufficient attack stems can die. Like pest scales of pot plants and fruit trees, arundo scale extracts the products of photosynthesis from the phloem of giant reed rhizomes, reducing the productivity and growth rate of plants. The New Zealand initiative can draw heavily on a biological control programme against giant reed that has been underway in USA and Mexico for over ten years.