Tropical Forest Community Ecology
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Dynamics and Disturbance in an Old-Growth Forest Remnant In
DYNAMICS AND DISTURBANCE IN AN OLD-GROWTH FOREST REMNANT IN WESTERN OHIO Thesis Submitted to The College of Arts and Sciences of the UNIVERSITY OF DAYTON In Partial Fulfillment of the Requirements for The Degree of Master of Science in Biology By Sean Michael Goins UNIVERSITY OF DAYTON Dayton, Ohio August, 2012 DYNAMICS AND DISTURBANCE IN AN OLD-GROWTH FOREST REMNANT IN WESTERN OHIO Name: Goins, Sean Michael APPROVED BY: __________________________________________ Ryan W. McEwan, Ph.D. Committee Chair Assistant Professor __________________________________________ M. Eric Benbow, Ph.D. Committee Member Assistant Professor __________________________________________ Mark G. Nielsen, Ph.D. Committee Member Associate Professor ii ABSTRACT DYNAMICS AND DISTURBANCE IN AN OLD-GROWTH FOREST REMNANT IN WESTERN OHIO Name: Goins, Sean Michael University of Dayton Advisor: Dr. Ryan W. McEwan Forest communities are dynamic through time, reacting to shifts in disturbance and climate regimes. A widespread community shift has been witnessed in many forests of eastern North America wherein oak (Quercus spp.) populations are decreasing while maple (Acer spp.) populations are increasing. Altered fire regimes over the last century are thought to be the primary driver of oak-to-maple community shifts; however, the influence of other non-equilibrium processes on this community shift remains under- explored. Our study sought to determine the community structure and disturbance history of an old-growth forest remnant in an area of western Ohio where fires were historically uncommon. To determine community structure, abundance of woody species was measured within 32 plots at 4 canopy strata and dendrochronology was used to determine the relative age-structure of the forest. -
Tropical Deciduous Forests and Savannas
2/1/17 Tropical Coastal Communities Relationships to other tropical forest systems — specialized swamp forests: Tropical Coastal Forests Mangrove and beach forests § confined to tropical and & subtropical zones at the interface Tropical Deciduous Forests of terrestrial and saltwater Mangrove Forests Mangrove Forests § confined to tropical and subtropical § stilt roots - support ocean tidal zones § water temperature must exceed 75° F or 24° C in warmest month § unique adaptations to harsh Queensland, Australia environment - convergent Rhizophora mangle - red mangrove Moluccas Venezuela 1 2/1/17 Mangrove Forests Mangrove Forests § stilt roots - support § stilt roots - support § pneumatophores - erect roots for § pneumatophores - erect roots for O2 exchange O2 exchange § salt glands - excretion § salt glands - excretion § viviparous seedlings Rhizophora mangle - red mangrove Rhizophora mangle - red mangrove Xylocarpus (Meliaceae) & Rhizophora Mangrove Forests Mangrove Forests § 80 species in 30 genera (20 § 80 species in 30 genera (20 families) families) § 60 species OW& 20 NW § 60 species OW& 20 NW (Rhizophoraceae - red mangrove - Avicennia - black mangrove; inner Avicennia nitida (black mangrove, most common in Neotropics) boundary of red mangrove, better Acanthaceae) drained Rhizophora mangle - red mangrove Xylocarpus (Meliaceae) & Rhizophora 2 2/1/17 Mangrove Forests § 80 species in 30 genera (20 families) § 60 species OW& 20 NW Four mangrove families in one Neotropical mangrove community Avicennia - Rhizophora - Acanthanceae Rhizophoraceae -
Tropical Vegetation Response to Heinrich Event 1 As Simulated with the Uvic ESCM Title Page and CCSM3 Abstract Introduction Conclusions References D
Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Clim. Past Discuss., 8, 5359–5387, 2012 www.clim-past-discuss.net/8/5359/2012/ Climate doi:10.5194/cpd-8-5359-2012 of the Past CPD © Author(s) 2012. CC Attribution 3.0 License. Discussions 8, 5359–5387, 2012 This discussion paper is/has been under review for the journal Climate of the Past (CP). Tropical vegetation Please refer to the corresponding final paper in CP if available. response to Heinrich Event 1 D. Handiani et al. Tropical vegetation response to Heinrich Event 1 as simulated with the UVic ESCM Title Page and CCSM3 Abstract Introduction Conclusions References D. Handiani1, A. Paul1,2, X. Zhang1, M. Prange1,2, U. Merkel1,2, and L. Dupont2 Tables Figures 1Department of Geosciences, University of Bremen, Bremen, Germany 2 MARUM – Center for Marine Environmental Sciences, University of Bremen, J I Bremen, Germany J I Received: 12 October 2012 – Accepted: 31 October 2012 – Published: 5 November 2012 Correspondence to: D. Handiani ([email protected]) Back Close Published by Copernicus Publications on behalf of the European Geosciences Union. Full Screen / Esc Printer-friendly Version Interactive Discussion 5359 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract CPD We investigated changes in tropical climate and vegetation cover associated with abrupt climate change during Heinrich Event 1 (HE1) using two different global cli- 8, 5359–5387, 2012 mate models: the University of Victoria Earth System-Climate Model (UVic ESCM) and 5 the Community Climate System Model version 3 (CCSM3). Tropical South American Tropical vegetation and African pollen records suggest that the cooling of the North Atlantic Ocean during response to Heinrich HE1 influenced the tropics through a southward shift of the rainbelt. -
Old-Growth Forests
Pacific Northwest Research Station NEW FINDINGS ABOUT OLD-GROWTH FORESTS I N S U M M A R Y ot all forests with old trees are scientifically defined for many centuries. Today’s old-growth forests developed as old growth. Among those that are, the variations along multiple pathways with many low-severity and some Nare so striking that multiple definitions of old-growth high-severity disturbances along the way. And, scientists forests are needed, even when the discussion is restricted to are learning, the journey matters—old-growth ecosystems Pacific coast old-growth forests from southwestern Oregon contribute to ecological diversity through every stage of to southwestern British Columbia. forest development. Heterogeneity in the pathways to old- growth forests accounts for many of the differences among Scientists understand the basic structural features of old- old-growth forests. growth forests and have learned much about habitat use of forests by spotted owls and other species. Less known, Complexity does not mean chaos or a lack of pattern. Sci- however, are the character and development of the live and entists from the Pacific Northwest (PNW) Research Station, dead trees and other plants. We are learning much about along with scientists and students from universities, see the structural complexity of these forests and how it leads to some common elements and themes in the many pathways. ecological complexity—which makes possible their famous The new findings suggest we may need to change our strat- biodiversity. For example, we are gaining new insights into egies for conserving and restoring old-growth ecosystems. canopy complexity in old-growth forests. -
Sass Forestecomgt 2018.Pdf
Forest Ecology and Management 419–420 (2018) 31–41 Contents lists available at ScienceDirect Forest Ecology and Management journal homepage: www.elsevier.com/locate/foreco Lasting legacies of historical clearcutting, wind, and salvage logging on old- T growth Tsuga canadensis-Pinus strobus forests ⁎ Emma M. Sassa, , Anthony W. D'Amatoa, David R. Fosterb a Rubenstein School of Environment and Natural Resources, University of Vermont, Burlington, VT 05405, USA b Harvard Forest, Harvard University, 324 N Main St, Petersham, MA 01366, USA ARTICLE INFO ABSTRACT Keywords: Disturbance events affect forest composition and structure across a range of spatial and temporal scales, and Coarse woody debris subsequent forest development may differ after natural, anthropogenic, or compound disturbances. Following Compound disturbance large, natural disturbances, salvage logging is a common and often controversial management practice in many Forest structure regions of the globe. Yet, while the short-term impacts of salvage logging have been studied in many systems, the Large, infrequent natural disturbance long-term effects remain unclear. We capitalized on over eighty years of data following an old-growth Tsuga Pine-hemlock forests canadensis-Pinus strobus forest in southwestern New Hampshire, USA after the 1938 hurricane, which severely Pit and mound structures damaged forests across much of New England. To our knowledge, this study provides the longest evaluation of salvage logging impacts, and it highlights developmental trajectories for Tsuga canadensis-Pinus strobus forests under a variety of disturbance histories. Specifically, we examined development from an old-growth condition in 1930 through 2016 across three different disturbance histories: (1) clearcut logging prior to the 1938 hurricane with some subsequent damage by the hurricane (“logged”), (2) severe damage from the 1938 hurricane (“hurricane”), and (3) severe damage from the hurricane followed by salvage logging (“salvaged”). -
The Impacts of Increasing Drought on Forest Dynamics, Structure, and Biodiversity in the United States
Global Change Biology (2016) 22, 2329–2352, doi: 10.1111/gcb.13160 SPECIAL FEATURE The impacts of increasing drought on forest dynamics, structure, and biodiversity in the United States JAMES S. CLARK1 , LOUIS IVERSON2 , CHRISTOPHER W. WOODALL3 ,CRAIGD.ALLEN4 , DAVID M. BELL5 , DON C. BRAGG6 , ANTHONY W. D’AMATO7 ,FRANKW.DAVIS8 , MICHELLE H. HERSH9 , INES IBANEZ10, STEPHEN T. JACKSON11, STEPHEN MATTHEWS12, NEIL PEDERSON13, MATTHEW PETERS14,MARKW.SCHWARTZ15, KRISTEN M. WARING16 andNIKLAUS E. ZIMMERMANN17 1Nicholas School of the Environment, Duke University, Durham, NC 27708, USA, 2Forest Service, Northern Research Station 359 Main Road, Delaware, OH 43015, USA, 3Forest Service 1992 Folwell Avenue,Saint Paul, MN 55108, USA, 4U.S. Geological Survey, Fort Collins Science Center Jemez Mountains Field Station, Los Alamos, NM 87544, USA, 5Forest Service, Pacific Northwest Research Station, Corvallis, OR 97331, USA, 6Forest Service, Southern Research Station, Monticello, AR 71656, USA, 7Rubenstein School of Environment and Natural Resources, University of Vermont, 04E Aiken Center, 81 Carrigan Dr., Burlington, VT 05405, USA, 8Bren School of Environmental Science and Management, University of California, Santa Barbara, CA 93106, USA, 9Department of Biology, Sarah Lawrence College, New York, NY 10708, USA, 10School of Natural Resources and Environment, University of Michigan, 2546 Dana Building, Ann Arbor, MI 48109, USA, 11U.S. Geological Survey, Southwest Climate Science Center and Department of Geosciences, University of Arizona, 1064 E. Lowell -
Neotropical Rainforest Restoration: Comparing Passive, Plantation and Nucleation Approaches
UC Riverside UC Riverside Previously Published Works Title Neotropical rainforest restoration: comparing passive, plantation and nucleation approaches Permalink https://escholarship.org/uc/item/4hf3v06s Journal BIODIVERSITY AND CONSERVATION, 25(11) ISSN 0960-3115 Authors Bechara, Fernando C Dickens, Sara Jo Farrer, Emily C et al. Publication Date 2016-10-01 DOI 10.1007/s10531-016-1186-7 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Biodivers Conserv DOI 10.1007/s10531-016-1186-7 REVIEW PAPER Neotropical rainforest restoration: comparing passive, plantation and nucleation approaches 1,2 2 2 Fernando C. Bechara • Sara Jo Dickens • Emily C. Farrer • 2,3 2 2,4 Loralee Larios • Erica N. Spotswood • Pierre Mariotte • Katharine N. Suding2,5 Received: 17 April 2016 / Revised: 5 June 2016 / Accepted: 25 July 2016 Ó Springer Science+Business Media Dordrecht 2016 Abstract Neotropical rainforests are global biodiversity hotspots and are challenging to restore. A core part of this challenge is the very long recovery trajectory of the system: recovery of structure can take 20–190 years, species composition 60–500 years, and reestablishment of rare/endemic species thousands of years. Passive recovery may be fraught with instances of arrested succession, disclimax or emergence of novel ecosystems. In these cases, active restoration methods are essential to speed recovery and set a desired restoration trajectory. Tree plantation is the most common active approach to reestablish a high density of native tree species and facilitate understory regeneration. While this approach may speed the successional trajectory, it may not achieve, and possibly inhibit, a long-term restoration trajectory towards the high species diversity characteristic of these forests. -
Ecological Insights from Long-Term Research Plots in Tropical and Temperate Forests
Ecological Insights from Long-term Research Plots in Tropical and Temperate Forests Organized Oral Session 40 was co-organized by Amy Wolf, Stuart Davies, and Richard Condit, and held on 6 August 2009 during the 94th ES A Annual Meeting in Albuquerque, New Mexico. An International Network of Forest Research Sites This session was devoted to findings from an international network of long-term forest dynamics plots, providing some of the first comparisons between the tropical and temperate study areas. Whereas most ecologists recognize the importance of long-term research (Callahan 1984, Likens 1989, Magnuson 1990, Hobbie et al. 2003, and others), large-scale projects like this one are rare. The global network of forest dynamics plots has expanded since its origin in the early 1980s, yet research at the plots has remained integrated due to a combination of individual scientists' efforts and institutional commitments from the Center for Tropical Forest Science (CTFS, <www.ctfs.si.edu> of the Smithsonian Tropical Research Institute and the Arnold Arboretum of Harvard University (Hubbell and Foster 1983, Condit 1995). Today, 26 large plots have been established in tropical or subtropical forests of Central and South America, Africa, Asia, and Oceania, along with 8 recently added temperate forest plots. A standard protocol (Condit 1998) is followed at all sites, including the marking, mapping, and measuring of all trees and shrubs with stem diameters >1 cm. Reports October 2009 519 Reports An underlying objective of the ESA session was to illustrate how an understanding of forest dynamics can contribute to long-term strategies of sustainable forest management in a changing global environment. -
Silvicultural Activities: Description and Terminology 1
WHITE PAPER F14-SO-WP-SILV-34 Silvicultural Activities: Description and Terminology 1 David C. Powell; Forest Silviculturist Supervisor’s Office; Pendleton, OR Initial Version: JUNE 1992 Most Recent Revision: FEBRUARY 2018 Introduction ........................................................................................................................ 2 Silvicultural systems ............................................................................................................ 2 Age-based silvicultural systems .................................................................................... 2 Even-aged management ............................................................................................... 3 Figure 1 – Three common stand structures ........................................................................... 4 Figure 2 – Clearcutting ............................................................................................................ 5 Figure 3 – Seed-tree and shelterwood cutting ....................................................................... 6 Figure 4 – Windthrow in spruce-fir forest in the northern Blue Mountains .......................... 8 Figure 5 – Examples of overstory removal and understory removal cutting ......................... 9 Uneven-aged management ........................................................................................ 10 Figure 6 – Examples of individual-tree selection cutting in ponderosa pine ....................... 12 Figure 7 – Examples of group selection -
Forest--Savanna Transition Zones
Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Biogeosciences Discuss., 11, 4591–4636, 2014 Open Access www.biogeosciences-discuss.net/11/4591/2014/ Biogeosciences BGD doi:10.5194/bgd-11-4591-2014 Discussions © Author(s) 2014. CC Attribution 3.0 License. 11, 4591–4636, 2014 This discussion paper is/has been under review for the journal Biogeosciences (BG). Forest–savanna Please refer to the corresponding final paper in BG if available. transition zones Structural, physiognomic and E. M. Veenendaal et al. aboveground biomass variation in Title Page savanna-forest transition zones on three Abstract Introduction continents. How different are Conclusions References co-occurring savanna and forest Tables Figures formations? J I E. M. Veenendaal1, M. Torello-Raventos2, T. R. Feldpausch3, T. F. Domingues4, J I 5 3 2,25 3,6 7 8 F. Gerard , F. Schrodt , G. Saiz , C. A. Quesada , G. Djagbletey , A. Ford , Back Close J. Kemp9, B. S. Marimon10, B. H. Marimon-Junior10, E. Lenza10, J. A. Ratter11, L. Maracahipes10, D. Sasaki12, B. Sonké13, L. Zapfack13, D. Villarroel14, Full Screen / Esc M. Schwarz15, F. Yoko Ishida6,16, M. Gilpin3, G. B. Nardoto17, K. Affum-Baffoe18, L. Arroyo14, K. Bloomfield3, G. Ceca1, H. Compaore19, K. Davies2, A. Diallo20, Printer-friendly Version N. M. Fyllas3, J. Gignoux21, F. Hien20, M. Johnson3, E. Mougin22, P. Hiernaux22, Interactive Discussion T. Killeen14,23, D. Metcalfe8, H. S. Miranda17, M. Steininger24, K. Sykora1, M. I. Bird2, J. Grace4, S. Lewis3,26, O. L. Phillips3, and J. Lloyd16,27 4591 -
Decelerating Growth in Tropical Forest Trees
Ecology Letters, (2007) 10: 461–469 doi: 10.1111/j.1461-0248.2007.01033.x LETTER Decelerating growth in tropical forest trees Abstract Kenneth J. Feeley,1* S. Joseph The impacts of global change on tropical forests remain poorly understood. We Wright,2 M. N. Nur Supardi,3 examined changes in tree growth rates over the past two decades for all species occurring Abd Rahman Kassim3 and Stuart in large (50-ha) forest dynamics plots in Panama and Malaysia. Stem growth rates 2,4 J. Davies declined significantly at both forests regardless of initial size or organizational level 1 Center for Tropical Forest (species, community or stand). Decreasing growth rates were widespread, occurring in Science, Arnold Arboretum Asia 24–71% of species at Barro Colorado Island, Panama (BCI) and in 58–95% of species at Program, Harvard University, 22 Pasoh, Malaysia (depending on the sizes of stems included). Changes in growth were not Divinity Avenue, Cambridge, consistently associated with initial growth rate, adult stature, or wood density. Changes in MA 02138, USA 2Smithsonian Tropical Research growth were significantly associated with regional climate changes: at both sites growth Institute, Panama City, Panama was negatively correlated with annual mean daily minimum temperatures, and at BCI 3Forest Environment Division, growth was positively correlated with annual precipitation and number of rainfree days Forest Research Institute (a measure of relative insolation). While the underlying cause(s) of decelerating growth is Malaysia, Kuala Lumpur, still unresolved, these patterns strongly contradict the hypothesized pantropical increase Malaysia 52109 in tree growth rates caused by carbon fertilization. Decelerating tree growth will have 4Center for Tropical Forest important economic and environmental implications. -
Changes in Global Terrestrial Live Biomass Over the 21St Century
advances.sciencemag.org/cgi/content/full/7/27/eabe9829/DC1 Supplementary Materials for Changes in global terrestrial live biomass over the 21st century Liang Xu, Sassan S. Saatchi*, Yan Yang, Yifan Yu, Julia Pongratz, A. Anthony Bloom, Kevin Bowman, John Worden, Junjie Liu, Yi Yin, Grant Domke, Ronald E. McRoberts, Christopher Woodall, Gert-Jan Nabuurs, Sergio de-Miguel, Michael Keller, Nancy Harris, Sean Maxwell, David Schimel *Corresponding author. Email: [email protected] Published 2 July 2021, Sci. Adv. 7, eabe9829 (2021) DOI: 10.1126/sciadv.abe9829 This PDF file includes: Figs. S1 to S10 Tables S1 to S7 Supplementary Materials Supplementary Figures & Tables Fig. S1. Flow chart of procedures estimating global live biomass carbon stocks. It includes the organizations of input data forming training samples for regional and spatio-temporal models, spatially continuous annual remote sensing data sets as predictor layers, the models used, and the final output products at 10km resolution. Fig. S2. Ecoregion maps used in this study. (A) Regional land cover types by separating the biomes based on continents; (B) Combined land cover types aggregated to a total of 5 vegetation classes globally. Maps were derived from the MODIS IGBP (International Geosphere-Biosphere Programme) land cover product. We selected the data in 2001 as the base map for the inclusion of forest clearing and fire events in their original classes. Detailed description of each class can be found in Table S1. Fig. S3. Regional carbon stock series from 2000 to 2019. The land cover classes were derived from MODIS LC product (Fig. S2) and divided continentally to show regional effects.