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Pollen-Based Temperature and Precipitation Records of the Past
University of Wollongong Research Online Faculty of Science, Medicine and Health - Papers Faculty of Science, Medicine and Health 2017 Pollen-based temperature and precipitation records of the past 14,600 years in northern New Zealand (37°S) and their linkages with the Southern Hemisphere atmospheric circulation Ignacio Jara Victoria University of Wellington Rewi Newnham Victoria University of Wellington Brent V. Alloway University of Wollongong Janet M. Wilmshurst Landcare Research NZ Andrew Rees Victoria University of Wellington Publication Details Jara, I. A., Newnham, R. M., Alloway, B. V., Wilmshurst, J. M. & Rees, A. B.H. (2017). Pollen-based temperature and precipitation records of the past 14,600 years in northern New Zealand (37°S) and their linkages with the Southern Hemisphere atmospheric circulation. The oH locene: a major interdisciplinary journal focusing on recent environmental change, 27 (11), 1756-1768. Research Online is the open access institutional repository for the University of Wollongong. For further information contact the UOW Library: [email protected] Pollen-based temperature and precipitation records of the past 14,600 years in northern New Zealand (37°S) and their linkages with the Southern Hemisphere atmospheric circulation Abstract Regional vegetation, climate history, and local water table fluctuations for the past 14,600 years are reconstructed from pollen and charcoal records of an ombrogenous peatbog in northern New Zealand (38°S). A long-term warming trend between 14,600 and 10,000 cal. yr BP is punctuated by two brief plateaux between 14,200-13,800 and 13,500-12,000 cal. yr BP. Periods of relatively drier conditions are inferred between 14,000-13,400 and 12,000-10,000 cal. -
Chromosome Numbers in Gymnosperms - an Update
Rastogi and Ohri . Silvae Genetica (2020) 69, 13 - 19 13 Chromosome Numbers in Gymnosperms - An Update Shubhi Rastogi and Deepak Ohri Amity Institute of Biotechnology, Research Cell, Amity University Uttar Pradesh, Lucknow Campus, Malhaur (Near Railway Station), P.O. Chinhat, Luc know-226028 (U.P.) * Corresponding author: Deepak Ohri, E mail: [email protected], [email protected] Abstract still some controversy with regard to a monophyletic or para- phyletic origin of the gymnosperms (Hill 2005). Recently they The present report is based on a cytological data base on 614 have been classified into four subclasses Cycadidae, Ginkgoi- (56.0 %) of the total 1104 recognized species and 82 (90.0 %) of dae, Gnetidae and Pinidae under the class Equisetopsida the 88 recognized genera of gymnosperms. Family Cycada- (Chase and Reveal 2009) comprising 12 families and 83 genera ceae and many genera of Zamiaceae show intrageneric unifor- (Christenhusz et al. 2011) and 88 genera with 1104 recognized mity of somatic numbers, the genus Zamia is represented by a species according to the Plant List (www.theplantlist.org). The range of number from 2n=16-28. Ginkgo, Welwitschia and Gen- validity of accepted name of each taxa and the total number of tum show 2n=24, 2n=42, and 2n=44 respectively. Ephedra species in each genus has been checked from the Plant List shows a range of polyploidy from 2x-8x based on n=7. The (www.theplantlist.org). The chromosome numbers of 688 taxa family Pinaceae as a whole shows 2n=24except for Pseudolarix arranged according to the recent classification (Christenhusz and Pseudotsuga with 2n=44 and 2n=26 respectively. -
Palaeo Leaf Economics Reveal a Shift in Ecosystem Function Associated with the End-Triassic Mass Extinction Event
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/318473239 Palaeo leaf economics reveal a shift in ecosystem function associated with the end-Triassic mass extinction event Article in Nature Plants · July 2017 DOI: 10.1038/nplants.2017.104 CITATIONS READS 7 428 7 authors, including: Wuu Kuang Soh Karen Bacon University College Dublin University of Leeds 14 PUBLICATIONS 79 CITATIONS 15 PUBLICATIONS 167 CITATIONS SEE PROFILE SEE PROFILE Margret Steinthorsdottir Andrew C Parnell Swedish Museum of Natural History Maynooth University 30 PUBLICATIONS 408 CITATIONS 103 PUBLICATIONS 5,129 CITATIONS SEE PROFILE SEE PROFILE Some of the authors of this publication are also working on these related projects: Mid-Cretaceous south polar forests View project Response of pan-Arctic permafrost peatlands to rapid climate warming View project All content following this page was uploaded by Wuu Kuang Soh on 24 March 2019. The user has requested enhancement of the downloaded file. ARTICLES PUBLISHED: XX XX 2017 | VOLUME: 3 | ARTICLE NUMBER: 17104 Palaeo leaf economics reveal a shift in ecosystem function associated with the end-Triassic mass extinction event W. K. Soh1*,I.J.Wright2,K.L.Bacon3, T. I. Lenz2, M. Steinthorsdottir4,5,A.C.Parnell6 and J. C. McElwain1 Climate change is likely to have altered the ecological functioning of past ecosystems, and is likely to alter functioning in the future; however, the magnitude and direction of such changes are difficult to predict. Here we use a deep-time case study to evaluate the impact of a well-constrained CO2-induced global warming event on the ecological functioning of dominant plant communities. -
Species-Specific Basic Stem-Wood Densities for Twelve Indigenous Forest and Shrubland Species of Known Age, New Zealand
Marden et al. New Zealand Journal of Forestry Science (2021) 51:1 https://doi.org/10.33494/nzjfs512021x121x E-ISSN: 1179-5395 published on-line: 15/02/2021 Research Article Open Access New Zealand Journal of Forestry Science Species-specific basic stem-wood densities for twelve indigenous forest and shrubland species of known age, New Zealand Michael Marden1,*, Suzanne Lambie2 and Larry Burrows3 1 31 Haronga Road, Gisborne 4010, New Zealand 2 Manaaki Whenua – Landcare Research, Private Bag 3127, Hamilton 3240, New Zealand 3 Manaaki Whenua – Landcare Research, PO Box 69041, Lincoln 7640, New Zealand *Corresponding author: [email protected] (Received for publication 19 July 2019; accepted in revised form 26 January 2021) Abstract Background: Tree carbon estimates for New Zealand indigenous tree and shrub species are largely based on mean of sites throughout New Zealand. Yet stem-wood density values feed directly into New Zealand’s international and nationalbasic stem-wood greenhouse densities gas accounting. derived from We a limitedaugment number existing of publishedtrees, often basic of unspecified stem-wood age density and from data a limited with new number age- old, across 21 widely-distributed sites between latitudes 35° tospecific estimate values carbon for 12stocks. indigenous forest and shrubland species, including rarely obtained values for trees <6-years and 46° S, and explore relationships commonly used Methods: The volume of 478 whole stem-wood discs collected at breast height (BH) was determined by water displacement, oven dried, and weighed. Regression analyses were used to determine possible relationships between basic stem-wood density, and tree height, root collar diameter (RCD), and diameter at breast height (DBH). -
Vietnamese Conifers and Some Problems of Their Sustainable Utilization Ke Loc Et Al
Vietnamese conifers and some problems of their sustainable utilization Ke Loc et al. Vietnamese conifers and some problems of their sustainable utilization Phan Ke Loc 1, 2, Nguyen Tien Hiep 2, Nguyen Duc To Luu 3, Philip Ian Thomas 4, Aljos Farjon 5, L.V. Averyanov 6, J.C. Regalado, Jr. 7, Nguyen Sinh Khang 2, Georgina Magin 8, Paul Mathew 8, Sara Oldfield 9, Sheelagh O’Reilly 8, Thomas Osborn 10, Steven Swan 8 and To Van Thao 2 1 University of Natural Science, Vietnam National University, Hanoi; 2 Institute of Ecology and Biological Resources; 3 Vietnam Central Forest Seed Company; 4 Royal Botanic Garden Edinburgh; 5 Royal Botanic Gardens, Kew; 6 Komarov Botanical Institute; 7 Missouri Botanical Garden; 8 Fauna & Flora International; 9 Global Trees Campaign; 10 Independent Consultant Introduction Vietnam is now recognized as one of the top ten global conifer conservation ‘hotspots’, as defined by the Conifer Specialist Group of the World Conservation Union (IUCN). Vietnam’s conifer flora has approximately 34 species that are indigenous to the country, making up about 5% of conifers known worldwide. Although conifers represent only less than 0.3% of the total number of higher vascular plant species of Vietnam, they are of great ecological, cultural and economic importance. Most conifer wood is prized for its high value in house construction, furniture making, etc. The decline of conifer populations in Vietnam has caused serious concern among scientists. Threats to conifer species are substantial and varied, ranging from logging (both commercial and subsistence), land clearing for agriculture, and forest fire. Over the past twelve years (1995-2006), Vietnam Botanical Conservation Program (VBCP), a scientific cooperation between the Missouri Botanical Garden in Saint Louis and the Institute of Ecology and Biological Resources in Hanoi, has conducted various studies on this important group of plants in order to gather baseline information necessary to make sound recommendations for their conservation and sustainable use. -
Fossil Pollen Records Indicate That Patagonian Desertification Was Not Solely a Consequence of Andean Uplift
ARTICLE Received 25 Oct 2013 | Accepted 4 Mar 2014 | Published 28 Mar 2014 DOI: 10.1038/ncomms4558 Fossil pollen records indicate that Patagonian desertification was not solely a consequence of Andean uplift L. Palazzesi1,2, V.D. Barreda1, J.I. Cuitin˜o3, M.V. Guler4, M.C. Tellerı´a5 & R. Ventura Santos6 The Patagonian steppe—a massive rain-shadow on the lee side of the southern Andes—is assumed to have evolved B15–12 Myr as a consequence of the southern Andean uplift. However, fossil evidence supporting this assumption is limited. Here we quantitatively estimate climatic conditions and plant richness for the interval B10–6 Myr based on the study and bioclimatic analysis of terrestrially derived spore–pollen assemblages preserved in well-constrained Patagonian marine deposits. Our analyses indicate a mesothermal climate, with mean temperatures of the coldest quarter between 11.4 °C and 16.9 °C (presently B3.5 °C) and annual precipitation rarely below 661 mm (presently B200 mm). Rarefied richness reveals a significantly more diverse flora during the late Miocene than today at the same latitude but comparable with that approximately 2,000 km further northeast at mid-latitudes on the Brazilian coast. We infer that the Patagonian desertification was not solely a consequence of the Andean uplift as previously insinuated. 1 Museo Argentino de Ciencias Naturales ‘Bernardino Rivadavia’, Angel Gallardo 470 (C1405DJR), Buenos Aires, Argentina. 2 Jodrell Laboratory, Royal Botanic Gardens, Kew, Richmond, Surrey TW9 3DS, UK. 3 Universidad de Buenos Aires, Departamento de Ciencias Geolo´gicas, Facultad de Ciencias Exactas y Naturales. Intendente Gu¨iraldes 2160 (C1428EHA), Buenos Aires, Argentina. -
2. DACRYCARPUS (Endlicher) De Laubenfels, J. Arnold Arbor. 50: 315
Flora of China 4: 79. 1999. 2. DACRYCARPUS (Endlicher) de Laubenfels, J. Arnold Arbor. 50: 315. 1969. 鸡毛松属 ji mao song shu Podocarpus L’Héritier ex Persoon sect. Dacrycarpus Endlicher, Syn. Conif. 221. 1847; Bracteocarpus A. V. Bobrov & Melikyan. Trees or shrubs evergreen, dioecious (very rarely monoecious); trunk straight; main branches spreading or drooping; branchlets drooping or ascending, dense. Leaves dimorphic: juvenile leaves 2-ranked and forming an oblong-ovate branchlet outline, linear, not scalelike; adult leaves needlelike or scalelike, falcate, bilaterally or bifacially flattened, or not flattened, 0.8–1.5 mm. Pollen cones lateral (rarely terminal), solitary or few together; microsporophylls numerous, imbricate; microsporangia 2, abaxial. Seed-bearing structures terminal and often borne on short, lateral branchlets, pedunculate, with appressed or spreading, bractlike leaves at base of peduncle; apical 1 or 2 bracts fertile; basal bracts fused to form a succulent, warty receptacle; ovule inverted. Epimatium wholly enveloping seed, united with fertile bract(s) and together bearing a short, free apex forming an asymmetrically projecting crest on immature seed-bearing structure. Seed large. Nine species: from China and Myanmar to Fiji Islands and New Zealand; one species in China. 1. Dacrycarpus imbricatus (Blume) de Laubenfels var. patulus de Laubenfels, J. Arnold Arbor. 50: 320. 1969. 鸡毛松 ji mao song Bracteocarpus kawaii (Hayata) A. V. Bobrov & Meli- kyan; Podocarpus kawaii Hayata. Trees to 40 m tall; trunk to 2 m d.b.h.; bark superficially dark brown or blackish, weathering gray, red-brown and granular fibrous within, flaking in thin strips; crown spreading; branchlets stiff, erect. Juvenile leaves borne at 60–75° to branchlet axis, 0.2– 0.7 mm apart (branchlets 3–4 × 1.2–1.6 cm in outline), sessile, green or ± glaucous, linear, falcate to “S”- shaped, 6–10(–17) × 0.9–1.2 mm, stomata arranged in 2 whitish rows on abaxial surface, base decurrent, margin entire, apex obliquely incurved-apiculate, apiculus 0.2–0.3 mm. -
Beetles in a Suburban Environment: a New Zealand Case Study. The
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26 AvailableNew on-lineZealand at: Journal http://www.newzealandecology.org/nzje/ of Ecology, Vol. 38, No. 1, 2014 Simulating long-term vegetation dynamics using a forest landscape model: the post-Taupo succession on Mt Hauhungatahi, North Island, New Zealand Timothy Thrippleton1*, Klara Dolos1, George L. W. Perry2,3, Jürgen Groeneveld3,4 and Björn Reineking1 1Biogeographical Modelling, BayCEER, University of Bayreuth, Universitätsstr. 30, 95447 Bayreuth, Germany 2School of Biological Sciences, The University of Auckland, Private Bag 92019, Auckland 1142, New Zealand 3School of Environment, The University of Auckland, Private Bag 92019, Auckland 1142, New Zealand 4Department of Ecological Modelling, Helmholtz Centre for Environmental Research – UFZ, Permoserstr. 15, 04318 Leipzig, Germany *Corresponding author (Email: [email protected]) Published online: 1 November 2013 Abstract: Forest dynamics in New Zealand are shaped by catastrophic, landscape-level disturbances (e.g. volcanic eruptions, windstorms and fires). The long return-intervals of these disturbances, combined with the longevity of many of New Zealand’s tree species, restrict empirical investigations of forest dynamics. In combination with empirical data (e.g. palaeoecological reconstructions), simulation modelling provides a way to address these limitations and to unravel complex ecological interactions. Here we adapt the forest landscape model LandClim to simulate dynamics across the large spatio-temporal scales relevant for New Zealand’s forests. Using the western slope of Mt Hauhungatahi in the central North Island as a case study, we examine forest succession following the Taupo eruption (c. 1700 cal. years BP), and the subsequent emergence of elevational species zonation. Focusing on maximum growth rate and shade tolerance we used a pattern-oriented parameterisation approach to derive a set of life-history parameters that agree with those described in the ecological literature. -
Fossil Ants (Hymenoptera: Formicidae): Ancient Diversity and the Rise of Modern Lineages
Myrmecological News 24 1-30 Vienna, March 2017 Fossil ants (Hymenoptera: Formicidae): ancient diversity and the rise of modern lineages Phillip BARDEN Abstract The ant fossil record is summarized with special reference to the earliest ants, first occurrences of modern lineages, and the utility of paleontological data in reconstructing evolutionary history. During the Cretaceous, from approximately 100 to 78 million years ago, only two species are definitively assignable to extant subfamilies – all putative crown group ants from this period are discussed. Among the earliest ants known are unexpectedly diverse and highly social stem- group lineages, however these stem ants do not persist into the Cenozoic. Following the Cretaceous-Paleogene boun- dary, all well preserved ants are assignable to crown Formicidae; the appearance of crown ants in the fossil record is summarized at the subfamilial and generic level. Generally, the taxonomic composition of Cenozoic ant fossil communi- ties mirrors Recent ecosystems with the "big four" subfamilies Dolichoderinae, Formicinae, Myrmicinae, and Ponerinae comprising most faunal abundance. As reviewed by other authors, ants increase in abundance dramatically from the Eocene through the Miocene. Proximate drivers relating to the "rise of the ants" are discussed, as the majority of this increase is due to a handful of highly dominant species. In addition, instances of congruence and conflict with molecular- based divergence estimates are noted, and distinct "ghost" lineages are interpreted. The ant fossil record is a valuable resource comparable to other groups with extensive fossil species: There are approximately as many described fossil ant species as there are fossil dinosaurs. The incorporation of paleontological data into neontological inquiries can only seek to improve the accuracy and scale of generated hypotheses. -
Republic of Fiji: the State of the World's Forest Genetic Resources
REPUBLIC OF FIJI This country report is prepared as a contribution to the FAO publication, The Report on the State of the World’s Forest Genetic Resources. The content and the structure are in accordance with the recommendations and guidelines given by FAO in the document Guidelines for Preparation of Country Reports for the State of the World’s Forest Genetic Resources (2010). These guidelines set out recommendations for the objective, scope and structure of the country reports. Countries were requested to consider the current state of knowledge of forest genetic diversity, including: Between and within species diversity List of priority species; their roles and values and importance List of threatened/endangered species Threats, opportunities and challenges for the conservation, use and development of forest genetic resources These reports were submitted to FAO as official government documents. The report is presented on www. fao.org/documents as supportive and contextual information to be used in conjunction with other documentation on world forest genetic resources. The content and the views expressed in this report are the responsibility of the entity submitting the report to FAO. FAO may not be held responsible for the use which may be made of the information contained in this report. STATE OF THE FOREST GENETIC RESOURCES IN FIJI Department of Forests Ministry of Fisheries and Forests for The Republic of Fiji Islands and the Secreatriat of Pacific Communities (SPC) State of the Forest Genetic Resources in Fiji _____________________________________________________________________________________________________________________ Table of Contents Executve Summary ………………………………………………………………………………………………………………………..…….. 5 Introduction ………………………………………………………………………………………………………………………………..…….. 6 Chapter 1: The Current State of the Forest Genetic Resources in Fiji ………………………………………………………………….……. -
Descriptions of Some Mature Kauri Forests of New Zealand, By
DESCRIPTIONS OF SOME MATURE KAURI FORESTS OF NEW ZEALAND by Moinuddin Ahmed and John Ogden Department of Botany, University of Auckland, Private Bag 92019, Auckland ABSTRACT A quantitative sampling of 25 mature kauri stands, throughout the species natural limits, was carried out. Each kauri stand is described in terms of its phytosociological attributes (frequency, density and basal area) for kauri and associated canopy and subcanopy species. A species list of plants under 10cm dbh is also given with their relative frequencies in each stand. In all stands kauri comprises most of the basal area. It is associated with 10 different co-dominant species. However, most of the forests have a similar species composition. It is suggested that all these kauri forest samples belong to one overall association. INTRODUCTION The vegetation of various kauri forests has been described by Adam (1889), Cockayne (1908, 1928), Cranwell and Moore (1936), Sexton (1941), Anon (1949) and more recently Barton (1972), Anon (1980) and Ecroyd (1982). A quantitative description of some kauri forests was given by Palmer (1982), Ogden (1983) and Wardle (1984). However, due to extensive past disturbance and milling, most of the above accounts do not describe the natural forest state. Observations on the population dynamics of mature kauri forests were presented by Ahmed and Ogden (1987) and Ogden et al. (1987) while multivariate analyses were performed by Ahmed (1988). However, no comprehensive attempt has yet been made to analyse mature undisturbed kauri forest stands in relation to their species composition. Kauri forests have a restricted distribution in the North Island. Among these remnants, there are few, if any, truly untouched sites.