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Propagating with Nature: Simpler Is Better by Mike Creel Written for July 21, 2005 Workshop at the 22Nd Annual Cullowhee Conference “Native Plants in the Landscape
Propagating WITH Nature: Simpler Is Better By Mike Creel Written for July 21, 2005 workshop at The 22nd Annual Cullowhee Conference “Native Plants in the Landscape CONTENTS Page ---- Topics 1 -- Why You Came Here - To Learn Simple Propagation What Is Different About Creel-Way Propagation? Low-Tech, Simple, Outdoors, Cheap A Few “Technical Terms Why Learn to Propagate Native Plants 2 -- How to Get Started in Creel-Way Propagation Principles of Creel-Way Propagation When Sticking Cuttings When Planting Seed Pots Identification Tags Woody Cutting Theory 3 -- Selecting & Mixing Your Media One All-Purpose Media Mix Shade Cloth Cools Cuttings Just Local Humus, No Rooting Hormones, Repotting Cuttings Varmint Caps for Seed Pots 4 -- Drilling Pots To Improve Drainage Drilling Thin-Walled Plastic Rescuing Pots In Peril Hold-Down Wires 5 -- Selection And Use Of Propagation Domes 6 -- Cuttings by the Calendar - Winter, Spring, Summer, Fall 7 -- Cutting Selection for Native Azaleas and Other Plants Unusual Cutting Types - InstantPlant, SuperPlant Unorthodox Propagation Pots - High-Rise, Collander, Dome-Pot Potpourri 8 -- Propagator’s Review Propagation With Motivation, Advantages of Creel-Way My Latest Experiments, Several Rules Nature Is My Greenhouse, Sharing Your Fruits 9 -- American Native Azalea Species in Bloom Order for Southeast Photos and Illustrations 10 -- Creel-Way Dome-Pot one gallon 11 -- Recommended Pots & Domes 12 - -Drilling & Filling Pots for Good Drainage 13-- Menagerie of Dome-Pots 14 -- Collander Dome-Pot 15 -- Dormant Cuttings Are Really Pruning Mike Creel 155 Cannon Trail Road Lexington, South Carolina 29073 [email protected] 1 -- Propagating WITH Nature: Simpler Is Better by Mike Creel Why You Came - You have probably come to this workshop wanting to learn new, simpler ways to propagate native plants on a small scale, and you will! I do not use rooting hormones other than what is contained in the plant cutting and in local soil bacteria. -
Mangrove Swamp (Caroni Wetland, Trinidad)
FIGURE 1.3 Swamps. (a) Floodplain swamp (Ottawa River, Canada). (b) Mangrove swamp (Caroni wetland, Trinidad). FIGURE 1.4 Marshes. (a) Riverine marsh (Ottawa River, Canada; courtesy B. Shipley). (b) Salt marsh (Petpeswick Inlet, Canada). FIGURE 1.5 Bogs. (a) Lowland continental bog (Algonquin Park, Canada). (b) Upland coastal bog (Cape Breton Island, Canada). FIGURE 1.6 Fens. (a) Patterned fen (northern Canada; courtesy C. Rubec). (b) Shoreline fen (Lake Ontario, Canada). FIGURE 1.7 Wet meadows. (a) Sand spit (Long Point, Lake Ontario, Canada; courtesy A. Reznicek). (b) Gravel lakeshore (Tusket River, Canada; courtesy A. Payne). FIGURE 1.8 Shallow water. (a) Bay (Lake Erie, Canada; courtesy A. Reznicek). (b) Pond (interdunal pools on Sable Island, Canada). FIGURE 2.1 Flooding is a natural process in landscapes. When humans build cities in or adjacent to wetlands, flooding can be expected. This example shows Cedar Rapids in the United States in 2008 (The Gazette), but incidences of flood damage to cities go far back in history to early cities such as Nineveh mentioned in The Epic of Gilgamesh (Sanders 1972). FIGURE 2.5 Many wetland organisms are dependent upon annual flood pulses. Animals discussed here include (a) white ibis (U.S. Fish and Wildlife Service), (b) Mississippi gopher frog (courtesy M. Redmer), (c) dragonfly (courtesy C. Rubec), and (d) tambaqui (courtesy M. Goulding). Plants discussed here include (e) furbish lousewort (bottom left; U.S. Fish and Wildlife Service) and ( f ) Plymouth gentian. -N- FIGURE 2.10 Spring floods produce the extensive bottomland forests that accompany many large rivers, such as those of the southeastern United States of America. -
Checklist of Common Native Plants the Diversity of Acadia National Park Is Refl Ected in Its Plant Life; More Than 1,100 Plant Species Are Found Here
National Park Service Acadia U.S. Department of the Interior Acadia National Park Checklist of Common Native Plants The diversity of Acadia National Park is refl ected in its plant life; more than 1,100 plant species are found here. This checklist groups the park’s most common plants into the communities where they are typically found. The plant’s growth form is indicated by “t” for trees and “s” for shrubs. To identify unfamiliar plants, consult a fi eld guide or visit the Wild Gardens of Acadia at Sieur de Monts Spring, where more than 400 plants are labeled and displayed in their habitats. All plants within Acadia National Park are protected. Please help protect the park’s fragile beauty by leaving plants in the condition that you fi nd them. Deciduous Woods ash, white t Fraxinus americana maple, mountain t Acer spicatum aspen, big-toothed t Populus grandidentata maple, red t Acer rubrum aspen, trembling t Populus tremuloides maple, striped t Acer pensylvanicum aster, large-leaved Aster macrophyllus maple, sugar t Acer saccharum beech, American t Fagus grandifolia mayfl ower, Canada Maianthemum canadense birch, paper t Betula papyrifera oak, red t Quercus rubra birch, yellow t Betula alleghaniesis pine, white t Pinus strobus blueberry, low sweet s Vaccinium angustifolium pyrola, round-leaved Pyrola americana bunchberry Cornus canadensis sarsaparilla, wild Aralia nudicaulis bush-honeysuckle s Diervilla lonicera saxifrage, early Saxifraga virginiensis cherry, pin t Prunus pensylvanica shadbush or serviceberry s,t Amelanchier spp. cherry, choke t Prunus virginiana Solomon’s seal, false Maianthemum racemosum elder, red-berried or s Sambucus racemosa ssp. -
This Article Appeared in a Journal Published by Elsevier. the Attached
This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Quaternary Research 75 (2011) 531–540 Contents lists available at ScienceDirect Quaternary Research journal homepage: www.elsevier.com/locate/yqres Response of a warm temperate peatland to Holocene climate change in northeastern Pennsylvania Shanshan Cai, Zicheng Yu ⁎ Department of Earth and Environmental Sciences, Lehigh University, 1 West Packer Avenue, Bethlehem, PA 18015, USA article info abstract Article history: Studying boreal-type peatlands near the edge of their southern limit can provide insight into responses of Received 11 September 2010 boreal and sub-arctic peatlands to warmer climates. In this study, we investigated peatland history using Available online 18 February 2011 multi-proxy records of sediment composition, plant macrofossil, pollen, and diatom analysis from a 14C-dated sediment core at Tannersville Bog in northeastern Pennsylvania, USA. Our results indicate that peat Keywords: accumulation began with lake infilling of a glacial lake at ~9 ka as a rich fen dominated by brown mosses. -
Managing Iowa Habitats
Managing Iowa Habitats Fen Wetlands Introduction Why should I be concerned? Fens are the rarest of Iowa’s wetland commu- Fens are an important and unique wetland nities and of great scientific interest. While type. Not only are the fens themselves rare, but their geology varies, they all are the products they shelter over 200 plant species, 20 of which of the seepage of groundwater to the surface. are Iowa endangered and threatened species. Because the water is rich in calcium and other Many of the plant species have been in these minerals, only a select group of plants is able to areas for thousands of years. The fen’s vegeta- grow there. As a result, fens contain many tion, in turn, shelters wildlife by providing plant species considered endangered or valuable habitat. threatened in Iowa. Fens are valuable to humans as well. They are A few of the oldest fens contain plant remains important as sites of groundwater discharge — that date back 10,000 years, though most Iowa good indicators of shallow aquifers. Vegetation fens are less than 5,000 years old. A few of in all wetlands plays an important role in these “younger” fens may have existed 10,000 recycling nutrients, trapping eroding soil, and years ago, but because of dramatic climate filtering out polluting chemicals such as changes, they may have dried up and lost the nitrates. However, the rarity of fens and their plant remains (by burning or erosion) that relatively small size makes it important could prove their age. When the climate grew to protect them from overloading by wetter again about 5,000 years ago, these fens these materials. -
Northern Fen Communitynorthern Abstract Fen, Page 1
Northern Fen CommunityNorthern Abstract Fen, Page 1 Community Range Prevalent or likely prevalent Infrequent or likely infrequent Absent or likely absent Photo by Joshua G. Cohen Overview: Northern fen is a sedge- and rush-dominated 8,000 years. Expansion of peatlands likely occurred wetland occurring on neutral to moderately alkaline following climatic cooling, approximately 5,000 years saturated peat and/or marl influenced by groundwater ago (Heinselman 1970, Boelter and Verry 1977, Riley rich in calcium and magnesium carbonates. The 1989). community occurs north of the climatic tension zone and is found primarily where calcareous bedrock Several other natural peatland communities also underlies a thin mantle of glacial drift on flat areas or occur in Michigan and can be distinguished from shallow depressions of glacial outwash and glacial minerotrophic (nutrient-rich) northern fens, based on lakeplains and also in kettle depressions on pitted comparisons of nutrient levels, flora, canopy closure, outwash and moraines. distribution, landscape context, and groundwater influence (Kost et al. 2007). Northern fen is dominated Global and State Rank: G3G5/S3 by sedges, rushes, and grasses (Mitsch and Gosselink 2000). Additional open wetlands occurring on organic Range: Northern fen is a peatland type of glaciated soils include coastal fen, poor fen, prairie fen, bog, landscapes of the northern Great Lakes region, ranging intermittent wetland, and northern wet meadow. Bogs, from Michigan west to Minnesota and northward peat-covered wetlands raised above the surrounding into central Canada (Ontario, Manitoba, and Quebec) groundwater by an accumulation of peat, receive inputs (Gignac et al. 2000, Faber-Langendoen 2001, Amon of nutrients and water primarily from precipitation et al. -
Western Samoa
A Directory of Wetlands in Oceania In: Scott, D.A. (ed.) 1993. A Directory of Wetlands in Oceania. IWRB, Slimbridge, U.K. and AWB, Kuala Lumpur, Malaysia. A Directory of Wetlands in Oceania WESTERN SAMOA INTRODUCTION by Cedric Schuster Department of Lands and Environment Area: 2,935 sq.km. Population: 170,000. Western Samoa is an independent state in the South Pacific situated between latitudes 13° and 14°30' South and longitudes 171° and 173° West, approximately 1,000 km northeast of Fiji. The state comprises two main inhabited islands, Savai'i (1,820 sq.km) and Upolu (1,105 sq.km), and seven islets, two of which are inhabited. Western Samoa is an oceanic volcanic archipelago that originated in the Pliocene. The islands were formed in a westerly direction with the oldest eruption, the Fagaloa volcanics, on the eastern side. The islands are still volcanically active, with the last two eruptions being in 1760 and 1905-11 respectively. Much of the country is mountainous, with Mount Silisili (1,858 m) on Savai'i being the highest point. Western Samoa has a wet tropical climate with temperatures ranging between 17°C and 34°C and an average temperature of 26.5°C. The temperature difference between the rainy season (November to March) and the dry season (May to October) is only 2°C. Rainfall is heavy, with a minimum of 2,000 mm in all places. The islands are strongly influenced by the trade winds, with the Southeast Trades blowing 82% of the time from April to October and 54% of the time from May to November. -
Apn80: Northern Spruce
ACID PEATLAND SYSTEM APn80 Northern Floristic Region Northern Spruce Bog Black spruce–dominated peatlands on deep peat. Canopy is often sparse, with stunted trees. Understory is dominated by ericaceous shrubs and fine- leaved graminoids on high Sphagnum hummocks. Vegetation Structure & Composition Description is based on summary of vascular plant data from 84 plots (relevés) and bryophyte data from 17 plots. l Moss layer consists of a carpet of Sphag- num with moderately high hummocks, usually surrounding tree bases, and weakly developed hollows. S. magellanicum dominates hum- mocks, with S. angustifolium present in hollows. High hummocks of S. fuscum may be present, although they are less frequent than in open bogs and poor fens. Pleurozium schre- beri is often very abundant and forms large mats covering drier mounds in shaded sites. Dicranum species are commonly interspersed within the Pleurozium mats. l Forb cover is minimal, and may include three-leaved false Solomon’s seal (Smilacina trifolia) and round-leaved sundew (Drosera rotundifolia). l Graminoid cover is 5-25%. Fine-leaved graminoids are most important and include three-fruited bog sedge (Carex trisperma) and tussock cottongrass (Eriophorum vagi- natum). l Low-shrub layer is prominent and dominated by ericaceous shrubs, particularly Lab- rador tea (Ledum groenlandicum), which often has >25% cover. Other ericads include bog laurel (Kalmia polifolia), small cranberry (Vaccinium oxycoccos), and leatherleaf (Chamaedaphne calyculata). Understory trees are limited to scattered black spruce. l Canopy is dominated by black spruce. Trees are usually stunted (<30ft [10m] tall) with 25-75% cover . Some sites have scattered tamaracks in addition to black spruce. -
PLTA-0103 Nature Conservancy 3/19/04 4:00 PM Page 1
PLTA-0103 Nature Conservancy 3/19/04 4:00 PM Page 1 ............................................................. Pennsylvania’s Land Trusts The Nature Conservancy About Land Trusts Conservation Options Conserving our Commonwealth Pennsylvania Chapter Land trusts are charitable organizations that conserve land Land trusts and landowners as well as government can by purchasing or accepting donations of land and conservation access a variety of voluntary tools for conserving special ................................................................ easements. Land trust work is based on voluntary agreements places. The basic tools are described below. The privilege of possessing Produced by the the earth entails the Pennsylvania Land Trust Association with landowners and creating projects with win-win A land trust can acquire land. The land trust then responsibility of passing it on, working in partnership with outcomes for communities. takes care of the property as a wildlife preserve, the better for our use, Pennsylvania’s land trusts Nearly a hundred land trusts work to protect important public recreation area or other conservation purpose. not only to immediate posterity, but to the unknown future, with financial support from the lands across Pennsylvania. Governed by unpaid A landowner and land trust may create an the nature of which is not William Penn Foundation, Have You Been to the Bog? boards of directors, they range from all-volunteer agreement known as a conservation easement. given us to know. an anonymous donor and the groups working in a single municipality The easement limits certain uses on all or a ~ Aldo Leopold Pennsylvania Department of Conservation n spring days, the Tannersville Cranberry Bog This kind of wonder saved the bog for today and for to large multi-county organizations with portion of a property for conservation and Natural Resources belongs to fourth-graders. -
Lowland Raised Bog (UK BAP Priority Habitat Description)
UK Biodiversity Action Plan Priority Habitat Descriptions Lowland Raised Bog From: UK Biodiversity Action Plan; Priority Habitat Descriptions. BRIG (ed. Ant Maddock) 2008. This document is available from: http://jncc.defra.gov.uk/page-5706 For more information about the UK Biodiversity Action Plan (UK BAP) visit http://www.jncc.defra.gov.uk/page-5155 Please note: this document was uploaded in November 2016, and replaces an earlier version, in order to correct a broken web-link. No other changes have been made. The earlier version can be viewed and downloaded from The National Archives: http://webarchive.nationalarchives.gov.uk/20150302161254/http://jncc.defra.gov.uk/page- 5706 Lowland Raised Bog The definition of this habitat remains unchanged from the pre-existing Habitat Action Plan (https://webarchive.nationalarchives.gov.uk/20110303150026/http://www.ukbap.org.uk/UKPl ans.aspx?ID=20, a summary of which appears below. Lowland raised bogs are peatland ecosystems which develop primarily, but not exclusively, in lowland areas such as the head of estuaries, along river flood-plains and in topographic depressions. In such locations drainage may be impeded by a high groundwater table, or by low permeability substrata such as estuarine, glacial or lacustrine clays. The resultant waterlogging provides anaerobic conditions which slow down the decomposition of plant material which in turn leads to an accumulation of peat. Continued accrual of peat elevates the bog surface above regional groundwater levels to form a gently-curving dome from which the term ‘raised’ bog is derived. The thickness of the peat mantle varies considerably but can exceed 12m. -
Mosses: Weber and Wittmann, Electronic Version 11-Mar-00
Catalog of the Colorado Flora: a Biodiversity Baseline Mosses: Weber and Wittmann, electronic version 11-Mar-00 Amblystegiaceae Amblystegium Bruch & Schimper, 1853 Amblystegium serpens (Hedwig) Bruch & Schimper var. juratzkanum (Schimper) Rau & Hervey WEBER73B. Amblystegium juratzkanum Schimper. Calliergon (Sullivant) Kindberg, 1894 Calliergon cordifolium (Hedwig) Kindberg WEBER73B; HERMA76. Calliergon giganteum (Schimper) Kindberg Larimer Co.: Pingree Park, 2960 msm, 25 Sept. 1980, [Rolston 80114), !Hermann. Calliergon megalophyllum Mikutowicz COLO specimen so reported is C. richardsonii, fide Crum. Calliergon richardsonii (Mitten) Kindberg WEBER73B. Campyliadelphus (Lindberg) Chopra, 1975 KANDA75 Campyliadelphus chrysophyllus (Bridel) Kanda HEDEN97. Campylium chrysophyllum (Bridel) J. Lange. WEBER63; WEBER73B; HEDEN97. Hypnum chrysophyllum Bridel. HEDEN97. Campyliadelphus stellatus (Hedwig) Kanda KANDA75. Campylium stellatum (Hedwig) C. Jensen. WEBER73B. Hypnum stellatum Hedwig. HEDEN97. Campylophyllum Fleischer, 1914 HEDEN97 Campylophyllum halleri (Hedwig) Fleischer HEDEN97. Nova Guinea 12, Bot. 2:123.1914. Campylium halleri (Hedwig) Lindberg. WEBER73B; HERMA76. Hypnum halleri Hedwig. HEDEN97. Campylophyllum hispidulum (Bridel) Hedenäs HEDEN97. Campylium hispidulum (Bridel) Mitten. WEBER63,73B; HEDEN97. Hypnum hispidulum Bridel. HEDEN97. Cratoneuron (Sullivant) Spruce, 1867 OCHYR89 Cratoneuron filicinum (Hedwig) Spruce WEBER73B. Drepanocladus (C. Müller) Roth, 1899 HEDEN97 Nomen conserv. Drepanocladus aduncus (Hedwig) Warnstorf WEBER73B. -
Rhodora (Rhododendron Canadense) Global Rank: G5 State Rank: SNR Climate Change Vulnerability Index: Highly Vulnerable Confidence: Low
Species: Rhodora (Rhododendron canadense) Global Rank: G5 State Rank: SNR Climate Change Vulnerability Index: Highly Vulnerable Confidence: Low Habitat: Rhodora is often locally abundant in bogs, peaty wetlands, and barrens in northeast Pennsylvania (Rhoads and Block 2007; Rhoads and Klein 1993). The range of rhodora extends from Newfoundland and Quebec west to Ontario and south to northeastern Pennsylvania and northern New Jersey (NatureServe 2011). Threats: Rhodora is likely to be sensitive to changes in temperature or hydrology at the sites it inhabits. Rhodora is mostly shade intolerant so tree species establishment and subsequent canopy development likely reduces populations of this shrub species. Main Factors Contributing to Vulnerability Rank: Distribution relative to natural barriers: Rhodora is limited to the northeastern corner of Pennsylvania where it represents the southern edge of its range. Dispersal and movement: Rhodora seeds are wind and water dispersed (Campbell et al. 2003) and mostly limited to short distance dispersal within the site where established. Predicted micro sensitivity to changes in temperature: Rhodora occur in microsites/microhabitats towards the cooler end of the spectrum. In Pennsylvania, rhodora is confined to the cooler, northeastern portion of the state. Predicted macro sensitivity to changes in precipitation, hydrology, or moisture regime: Within the species range in Pennsylvania, the species has experienced a less than average precipitation variation in the past 50 years. Predicted micro sensitivity to changes in precipitation, hydrology, or moisture regime: Rhodora is somewhat to moderately dependent on a moisture regime that is highly vulnerable to loss or reduction with climate change and the expected direction of moisture change is likely to reduce the species’ distribution, abundance, or habitat quality.