The Role of Remote Sensing for the Assessment and Monitoring of Forest Health: a Systematic Evidence Synthesis
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Conservation Issues: California Chaparral
Author's personal copy Conservation Issues: California Chaparral RW Halsey, California Chaparral Institute, Escondido, CA, United States JE Keeley, U.S. Geological Survey, Three Rivers, CA, United States ã 2016 Elsevier Inc. All rights reserved. What Is Chaparral? 1 California Chaparral Biodiversity 1 Chaparral Community Types 1 Measuring Chaparral Biodiversity 4 Diversity Within Individual Plant Taxa 5 Faunal Diversity 5 Influence of Geology 7 Influence of Climate 7 Influence of Fire 8 Impact of Climate Change 10 Preserving Chaparral Biodiversity 10 References 10 What Is Chaparral? Chaparral is a diverse, sclerophyllous shrub-dominated plant community shaped by a Mediterranean-type climate (hot, dry summers and mild, wet winters), a complex mixture of relatively young soils (Specht and Moll, 1983), and large, infrequent, high-intensity fires (30–150 year fire return interval) (Keeley and Zedler, 2009; Keeley et al., 2004; Lombardo et al., 2009). Large expanses of dense chaparral vegetation cover coastal mesas, canyons, foothills, and mountain slopes throughout the California Floristic Province (Figure 1), southward into Baja California, and extending north into the Rogue River Valley of southwest Oregon. Disjunct patches of chaparral can also be found in central and southeastern Arizona and northern Mexico (Keeley, 2000). Along with the four other Mediterranean-type climate regions of the world with similar shrubland vegetation (Central Chile, Mediterranean Basin, South Africa, and southwestern Australia) (Table 1), California has been designated a biodiversity hot spot (Myers et al., 2000). Twenty-five designated locations in all, these hot spots have exceptional concentrations of endemic species that are undergoing exceptional loss of habitat (Myers et al., 2000; Rundel, 2004). -
Woodlands of the Savanna Lands No
Tropical Topics An interpretive newsletter for the tourism industry Woodlands of the savanna lands No. 71 December 2001 Conserving moisture Notes from the Life is tough for plants living in the seasonally dry tropics. Soils arepoorandforhalftheyearthelandisparchedandproneto Editor fireswhilefortheotherhalfitisinundatedwithwater.Only Millions of years ago, much of the plantswhichhavebeenabletoadapttothispunishingregime Australian continent was covered cangrowhere,havingdevelopedcertaincharacteristicsto with rainforest. However, as the makethispossible. climate changed and the continent became more arid, a new type of While trees in the rainforest tend to It seems that these vegetation evolved consisting of have spreading surface roots to make trees are simply using plants which adapted themselves the most of nutrients available on the different survival to the new harsh conditions – forest floor, those in savanna lands strategies. It is as if they notably eucalypts, acacias, generally have deep root systems, to make the choice between melaleucas, grevilleas and reach deep reserves of water. Some investing energy into producing a banksias. trees concentrate their resources in the strong, long-lasting product or early stages of growth on developing numerous poor-quality disposable These types of trees now occupy a deep and massive tap root. ones. Studies have shown that the much of the savanna lands. This ‘construction costs’ to a tree for Tropical Topics cannot, of course, Once obtained, water must be used production of deciduous leaves are describe them all but looks at economically. The thick bark on many lower than the costs of producing strategies for living in an tropical woodland trees, apart from evergreen leaves. inhospitable environment, giving protection from fire, can help to characteristics of the main groups conserve moisture. -
The Chaparral Vegetation in Mexico Under Nonmediterranean Climate: the Convergence and Madrean-Tethyan Hypotheses Reconsidered1
American Journal of Botany 85(10): 1398±1408. 1998. THE CHAPARRAL VEGETATION IN MEXICO UNDER NONMEDITERRANEAN CLIMATE: THE CONVERGENCE AND MADREAN-TETHYAN HYPOTHESES RECONSIDERED1 ALFONSO VALIENTE-BANUET,2,4 NOEÂ FLORES-HERNAÂ NDEZ,2 MIGUEL VERDUÂ ,3 AND PATRICIA DAÂ VILA3 2Instituto de EcologõÂa, Universidad Nacional AutoÂnoma de MeÂxico, Apartado Postal 70±275, UNAM, 04510 MeÂxico, D.F.; and 3UBIPRO, ENEP-Iztacala, Universidad Nacional AutoÂnoma de MeÂxico, Apartado Postal 314, MeÂxico, 54090, Tlalnepantla, MeÂxico A comparative study between an unburned evergreen sclerophyllous vegetation located in south-central Mexico under a wet-summer climate, with mediterranean regions was conducted in order to re-analyze vegetation and plant characters claimed to converge under mediterranean climates. The comparison considered ¯oristic composition, plant-community struc- ture, and plant characters as adaptations to mediterranean climates and analyzed them by means of a correspondence analysis, considering a tropical spiny shrubland as the external group. We made a species register of the number of species that resprouted after a ®re occurred in 1995 and a distribution map of the evergreen sclerophyllous vegetation in Mexico (mexical) under nonmediterranean climates. The TehuacaÂn mexical does not differ from the evergreen sclerophyllous areas of Chile, California, Australia, and the Mediterranean Basin, according to a correspondence analysis, which ordinated the TehuacaÂn mexical closer to the mediter- ranean areas than to the external group. All the vegetation and ¯oristic characteristics of the mexical, as well as its distribution along the rain-shadowed mountain parts of Mexico, support its origin in the Madrean-Tethyan hypothesis of Axelrod. Therefore, these results allow to expand the convergence paradigm of the chaparral under an integrative view, in which a general trend to aridity might explain ¯oristic and adaptive patterns detected in these environments. -
Season of Burn Effects in Southern California Chaparral
Paper presented at 2nd Interface Between Ecology and Land Development in California conference, 18-19 April 1997, Occidental College, Los Angeles, CA; Jon E. Keeley, coordinator. Season of Burn Effects in Southern California Chaparral Jan L. Beyers and Carla D. Wakeman Pacific Southwest Research Station, USDA Forest Service, Riverside, CA 92507 Tel. (909) 680-1527; Fax (909) 680-1501 E-mail: [email protected] Abstract. Prescribed burning for fuel reduction is most safely implemented during the wet season or early summer in southern California chaparral. Previous studies suggest that wet season burns result in poor germination of fire-dependent species and that growing season burns may reduce sprouting vigor of shrubs. We examined vegetation recovery after March, June, and November prescribed fires at different sites, and after spring and fall wildfires in a single area. At all sites, good germination of obligate-seeding Ceanothus was observed, and herbaceous species with both heat- and charate-stimulated germination were found. Shrub sprouting percentage tended to be lower after the late spring burn than the fall burns. Fire intensity and postfire weather patterns may also affect chaparral regeneration response. Keywords: Adenostoma fasciculatum, Ceanothus, chamise, fire effects, fire-followers, fire intensity, prescribed fire Introduction Chaparral is the fire-prone, shrub-dominated vegetation type abundant in the foothills adjacent to many southern California cities. Shrubs are typically 1 to 4 m (3 to 12 ft) tall with evergreen, sclerophyllous leaves (Cooper 1922, Keeley and Keeley 1988). California’s Mediterranean-type climate is characterized by mild, wet winters and hot, dry summers (Barbour and Major 1988). -
Assessing Water Stress of Desert Tamarugo Trees Using in Situ Data and Very High Spatial Resolution Remote Sensing
Remote Sens. 2013, 5, 5064-5088; doi:10.3390/rs5105064 OPEN ACCESS Remote Sensing ISSN 2072-4292 www.mdpi.com/journal/remotesensing Article Assessing Water Stress of Desert Tamarugo Trees Using in situ Data and Very High Spatial Resolution Remote Sensing Roberto O. Chávez 1,*, Jan G. P. W. Clevers 1, Martin Herold 1, Edmundo Acevedo 2 and Mauricio Ortiz 2,3 1 Laboratory of Geo-Information Science and Remote Sensing, Wageningen University, P.O. Box 47, 6700 AA Wageningen, The Netherlands; E-Mails: [email protected] (J.G.P.W.C.); [email protected] (M.H.) 2 Laboratorio de Relación Suelo-Agua-Planta, Facultad de Ciencias Agronómicas, Universidad de Chile, Casilla 1004, Santiago, Chile; E-Mail: [email protected] (E.A.); [email protected] (M.O.) 3 Centro de Estudios Avanzados en Fruticultura (CEAF), Conicyt-Regional R08I1001, Av. Salamanca s/n, Rengo, Chile * Author to whom correspondence should be addressed; E-Mails: [email protected] or [email protected]; Tel.: +31-317-481-552; Fax: +31-317-419-000. Received: 24 July 2013; in revised form: 12 September 2013 / Accepted: 9 October 2013 / Published: 15 October 2013 Abstract: The hyper-arid Atacama Desert is one of the most extreme environments for life and only few species have evolved to survive its aridness. One such species is the tree Prosopis tamarugo Phil. Because Tamarugo completely depends on groundwater, it is being threatened by the high water demand from the Chilean mining industry and the human consumption. In this paper, we identified the most important biophysical variables to assess the water status of Tamarugo trees and tested the potential of WorldView2 satellite images to retrieve these variables. -
(Prosopis, Section Algarobia) in the Atacama Desert of Northern Chile
RESEARCH ARTICLE The pre-Columbian introduction and dispersal of Algarrobo (Prosopis, Section Algarobia) in the Atacama Desert of northern Chile Virginia B. McRostie1,2,3*, Eugenia M. Gayo4,5, Calogero M. Santoro6, Ricardo De Pol- Holz5,7, Claudio Latorre2,3 1 Departamento de AntropologÂõa, Facultad de Ciencias Sociales, Pontificia Universidad CatoÂlica de Chile, Santiago, Chile, 2 EcologõÂa & Centro UC Desierto de Atacama, Facultad de Ciencias BioloÂgicas, Pontificia Universidad CatoÂlica de Chile, Santiago, Chile, 3 Instituto de EcologõÂa y Biodiversidad, Santiago, Chile, a1111111111 4 Departamento de OceanografõÂa, Universidad de ConcepcioÂn, ConcepcioÂn, Chile, 5 Center for Climate and a1111111111 Resilience Research (CR)2, Santiago, Chile, 6 Instituto de Alta InvestigacioÂn, Laboratorio de ArqueologÂõa y a1111111111 Paleoambiente, Universidad de TarapacaÂ, Arica, Chile, 7 GAIA-Antartica, Universidad de Magallanes, Punta a1111111111 Arenas, Chile a1111111111 * [email protected] Abstract OPEN ACCESS Archaeological and palaeoecological studies throughout the Americas have documented Citation: McRostie VB, Gayo EM, Santoro CM, De Pol-Holz R, Latorre C (2017) The pre-Columbian widespread landscape and environmental transformation during the pre-Columbian era. The introduction and dispersal of Algarrobo (Prosopis, highly dynamic Formative (or Neolithic) period in northern Chile (ca. 3700±1550 yr BP) Section Algarobia) in the Atacama Desert of brought about the local establishment of agriculture, introduction of new crops (maize, qui- northern Chile. PLoS ONE 12(7): e0181759. https://doi.org/10.1371/journal.pone.0181759 noa, manioc, beans, etc.) along with a major population increase, new emergent villages and technological innovations. Even trees such as the Algarrobos (Prosopis section Algarobia) Editor: William J. Etges, University of Arkansas, UNITED STATES may have been part of this transformation. -
The Three Mediterranean Climates
Middle States Geographer, 2005, 38:52-60 THREE CONFLATED DEFINITIONS OF MEDITERRANEAN CLIMATES Mark A. Blumler Department of Geography SUNY Binghamton Binghamton, NY 13902-6000 ABSTRACT: "Mediterranean climate" has in effect three different definitions: 1) climate of the Mediterranean Sea and bordering land areas; 2) climate that favors broad-leaved, evergreen, sclerophyllous shrubs and trees; 3) winter-wet, summer-dry climate. These three definitions frequently are conflated, giving rise to considerable confusion and misstatement in the literature on biomes, vegetation-environment relationships, and climate change. Portions of the Mediterranean region do not have winter-wet, summer-dry climate, while parts that do, may not have evergreen sclerophylls. Places away from the Mediterranean Sea, such as the Zagros foothills, have more mediterranean climate than anywhere around the Sea under the third definition. Broad-leaved evergreen sclerophylls dominate some regions with non-mediterranean climates, typically with summer precipitation maximum as well as winter rain, and short droughts in spring and fall. Thus, such plants may be said to characteristize subtropical semi-arid regions. On the other hand, where summer drought is most severe, i.e., the most mediterranean climate under definition 3, broad-leaved evergreen sclerophylls are rare to absent. Rather than correlating with sclerophyll dominance, regions of extreme winter-wet, summer-dry climate characteristically support a predominance of annuals, the life form best adapted to seasonal rainfall regimes. Given the importance of useful forecasting of vegetation and climate change under greenhouse warming, it is imperative that biome maps begin to reflect the complexities of vegetation-climate relationships. INTRODUCTION literature also is replete with inaccurate statements about mediterranean regions. -
A Multi-Scale, Multi- Proxy Assessment of the Resilience of Cool Temperate Rainforest to Fire in Victoria’S Central Highlands
18 Fire on the mountain: A multi-scale, multi- proxy assessment of the resilience of cool temperate rainforest to fire in Victoria’s Central Highlands Patrick J. Baker School of Biological Sciences, Monash University, Clayton, Victoria [email protected] Rohan Simkin Monash University, Clayton, Victoria Nina Pappas Monash University, Clayton, Victoria Alex McLeod Monash University, Clayton, Victoria Merna McKenzie Monash University, Clayton, Victoria Introduction A common feature of many Australian landscapes is the interdigitation of eucalypt- dominated sclerophyll forest with rainforest. In most instances, the eucalypt forests dominate the landscape, with rainforest restricted to relatively small fragments and strips that are often (but not always) associated with topographic features such as riparian zones or southeastern- facing slopes. However, these patterns reflect the current state of a dynamic system. Over several terra australis 34 376 Patrick J. Baker et al. hundreds of thousands of years, the relative dominance of the rainforests and eucalypt forests has waxed and waned across these landscapes in near synchrony (Kershaw et al. 2002; Sniderman et al. 2009). During periods of relatively warm, dry conditions, the eucalypt- dominated vegetation has expanded and the rainforest contracted across the landscape. When the climate has been relatively cool and moist, the rainforests have expanded and the eucalypt forest contracted. This is, in part, thought to be a direct consequence of the ambient environmental conditions and their impact on regeneration success. However, the indirect influence of climate, in particular as a driver of fire regimes, may be as important, if not more important, in defining the structure, composition and relative abundance of rainforest and eucalypt taxa at the landscape scale. -
Classification and Description of World Formation Types
United States Department of Agriculture Classification and Description of World Formation Types Don Faber-Langendoen, Todd Keeler-Wolf, Del Meidinger, Carmen Josse, Alan Weakley, David Tart, Gonzalo Navarro, Bruce Hoagland, Serguei Ponomarenko, Gene Fults, Eileen Helmer Forest Rocky Mountain General Technical Service Research Station Report RMRS-GTR-346 August 2016 Faber-Langendoen, D.; Keeler-Wolf, T.; Meidinger, D.; Josse, C.; Weakley, A.; Tart, D.; Navarro, G.; Hoagland, B.; Ponomarenko, S.; Fults, G.; Helmer, E. 2016. Classification and description of world formation types. Gen. Tech. Rep. RMRS-GTR-346. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station. 222 p. Abstract An ecological vegetation classification approach has been developed in which a combi- nation of vegetation attributes (physiognomy, structure, and floristics) and their response to ecological and biogeographic factors are used as the basis for classifying vegetation types. This approach can help support international, national, and subnational classifica- tion efforts. The classification structure was largely developed by the Hierarchy Revisions Working Group (HRWG), which contained members from across the Americas. The HRWG was authorized by the U.S. Federal Geographic Data Committee (FGDC) to devel- op a revised global vegetation classification to replace the earlier versions of the structure that guided the U.S. National Vegetation Classification and International Vegetation Classification, which formerly relied on the UNESCO (1973) global classification (see FGDC 1997; Grossman and others 1998). This document summarizes the develop- ment of the upper formation levels. We first describe the history of the Hierarchy Revisions Working Group and discuss the three main parameters that guide the clas- sification—it focuses on vegetated parts of the globe, on existing vegetation, and includes (but distinguishes) both cultural and natural vegetation for which parallel hierarchies are provided. -
Eucalypt Open Forest
NVIS Fact sheet MVG 3 – Eucalypt open forest Australia’s native vegetation is a rich and fundamental Overview element of our natural heritage. It binds and nourishes our ancient soils; shelters and sustains wildlife, protects Typically, vegetation areas classified under streams, wetlands, estuaries, and coastlines; and absorbs MVG 3 – Eucalypt open forest: carbon dioxide while emitting oxygen. The National • correspond well with ‘dry sclerophyll forests’, but may Vegetation Information System (NVIS) has been developed include some wet sclerophyll forests (mostly classified and maintained by all Australian governments to provide within MVG 2) that do not exceed 30 m in height a national picture that captures and explains the broad • are distributed widely in monsoonal, tropical, diversity of our native vegetation. subtropical and temperate latitudes on soils of low to This is part of a series of fact sheets which the Australian moderate fertility Government developed based on NVIS Version 4.2 data to • dominant trees vary from 10 to 30 m tall and with provide detailed descriptions of the major vegetation groups crown cover 50 – 80 per cent (foliage projective cover of (MVGs) and other MVG types. The series is comprised of 30 – 70 per cent) depending on soil characteristics, local a fact sheet for each of the 25 MVGs to inform their use by moisture and rainfall planners and policy makers. An additional eight MVGs are • are dominated by a variety of eucalypts from the available outlining other MVG types. genera Corymbia, Angophora and Eucalyptus subgenus Eucalyptus, occasionally with Eucalyptus species from For more information on these fact sheets, including other subgenera, notably Symphyomyrtus its limitations and caveats related to its use, please see: ‘Introduction to the Major Vegetation Group • comprise understoreys typically dominated by shrubs, (MVG) fact sheets’. -
The Conservation of Biodiversity in Chile
Revista Chilena de Historia Natural 66:383-402, 1993 REVIEW The conservation of biodiversity in Chile La conservaci6n de la biodiversidad en Chile CESARS.ORMAZABAL School of Forestry and Environmental Studies Yale University, New Haven, Connecticut 06511, USA Current Address: Rodas 124, Las Condes, Santiago, Chile ABSTRACT I analyze Chile's biological diversity in terrestrial and marine environments, including information on the magnitude of biodiversity at three levels (ecosystem, species, and genetic). I identify the main values, and the importance of conserving such heritage, making comments about past and current activities of some national institutions interested in biodiversity conservation. I emphasize actions related to increasing and improving knowledge on biodiversity, legislation, some economic and social values, and protection of biodiversity in the field. I identify the main threats to Chile's biodiversity and give recommendations for maintaining and enhancing its conservation. Chile has developed many efforts to avoid biodiversity losses. It has enacted legislation, maintained institutions, and taken actions that favor biological diversity. However, some of the policies, legislation, and actions have been too specific, disperse, and uncoordinated. A system of inter-institutional coordination is urgently required. An efficient approach, through symposia, to identify the most threatened woody plant and terrestrial vertebrate species, was developed. Now, is time to define conservation status for species not included in previous symposia, identify the most threatened species, and begin programs to increase their population size. It is essential to initiate actions concerning the protection of amphibians, reptiles, cacti, and non-woody terrestrial plants. Also, it is urgent to start conservation activities for aquatic environments. -
Prosopis Pallida Complex: a Monograph
DFID DFID Natural Resources Systems Programme The Prosopis juliflora - Prosopis pallida Complex: A Monograph NM Pasiecznik With contributions from P Felker, PJC Harris, LN Harsh, G Cruz JC Tewari, K Cadoret and LJ Maldonado HDRA - the organic organisation The Prosopis juliflora - Prosopis pallida Complex: A Monograph NM Pasiecznik With contributions from P Felker, PJC Harris, LN Harsh, G Cruz JC Tewari, K Cadoret and LJ Maldonado HDRA Coventry UK 2001 organic organisation i The Prosopis juliflora - Prosopis pallida Complex: A Monograph Correct citation Pasiecznik, N.M., Felker, P., Harris, P.J.C., Harsh, L.N., Cruz, G., Tewari, J.C., Cadoret, K. and Maldonado, L.J. (2001) The Prosopis juliflora - Prosopis pallida Complex: A Monograph. HDRA, Coventry, UK. pp.172. ISBN: 0 905343 30 1 Associated publications Cadoret, K., Pasiecznik, N.M. and Harris, P.J.C. (2000) The Genus Prosopis: A Reference Database (Version 1.0): CD ROM. HDRA, Coventry, UK. ISBN 0 905343 28 X. Tewari, J.C., Harris, P.J.C, Harsh, L.N., Cadoret, K. and Pasiecznik, N.M. (2000) Managing Prosopis juliflora (Vilayati babul): A Technical Manual. CAZRI, Jodhpur, India and HDRA, Coventry, UK. 96p. ISBN 0 905343 27 1. This publication is an output from a research project funded by the United Kingdom Department for International Development (DFID) for the benefit of developing countries. The views expressed are not necessarily those of DFID. (R7295) Forestry Research Programme. Copies of this, and associated publications are available free to people and organisations in countries eligible for UK aid, and at cost price to others. Copyright restrictions exist on the reproduction of all or part of the monograph.