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Is Glyphis Cicatricosa an Indicator for 'Global Warming' Or an 'Urban Heat

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Is Glyphis Cicatricosa an Indicator for 'Global Warming' Or an 'Urban Heat The Lichenologist 49(3): 291–296 (2017) © British Lichen Society, 2017 doi:10.1017/S0024282917000111 Is Glyphis cicatricosa an indicator for ‘global warming’ or an ‘urban heat island’ effect in Japan? During the course of floristic studies of Japa- which are 6–12-locular with lenticular cells, nese lichens, Glyphis cicatricosa Ach. (Graphi- 30–55 × 7–12 μm; and absence of specific daceae, Ascomycota), a pantropical species chemical substances (Nakanishi 1966; (Galloway 2007), was found on the bark of Archer 2009). The specimen collected from Phellodendron amurense Rupr. in a suburban Tsukuba-city agrees with the morphological area of Tsukuba-city (36°06'03''N, 140° and chemical features mentioned above, with 06'43''E). This is on the Pacificsideofeastern spore sizes ((min.–) mean ± 1SD (–max.)) as Honshu, with a warm-temperate climate and follows: (31·7–)35·1 ± 3·8(–45·1) × (6·7–) is the northernmost locality of G. cicatricosa in 7·8 ± 0·7(–9·2) μm(n = 10). Japan. The sapling tree was planted in the Glyphis cicatricosa is widely distributed Tsukuba Botanical Garden (c. 14 ha, 20 m in tropical to warm-temperate regions such elev.) in 1984 when the mean annual as south-eastern USA, Central and South temperature was 12 °C, but this has gradually America, South, South-East and East Asia, increased since then to almost 15 °C in 2015 Australia, New Zealand and the Pacific (e.g. when G. cicatricosa was discovered (Fig. 1). Archer 2009; Moon et al. 2015). In Japan, it Does an increase in annual temperature at this is reported from warm-temperate and sub- site plausibly explain the unexpected phyto- tropical regions in the south and the Bonin geographical distribution of this lichen in Islands (Nakanishi 1966; Kurokawa 1969). terms of ‘global warming’, or is it the result of The record from Tsukuba-city is the most an ‘urban heat island’ effect, or indeed is it northern locality within Japan (Fig. 2). Here related to one or more other factors? the tree on which it occurs is isolated in a relatively open setting (Fig. 3). The tree on A voucher specimen of G. cicatricosa collected during a which G. cicatricosa is found was originally field survey in 2015, now housed in the National transplanted from a montane area of central Museum of Nature and Science (TNS), was compared with other specimens of the species in TNS listed Japan (Yamanashi Prefecture) where this below. Morphological observations were made using a lichen is absent and has almost certainly dissecting microscope (Olympus SZX16) and a differ- become established after the tree was ential interference contrast microscope (Olympus collected. On the tree trunk c. 10 thalli (each BX51). Anatomical examination was undertaken using 1–3 cm in diam.) grow, 30 to 150 cm above hand-cut sections mounted in GAW (glycerine: ethanol: water, 1:1:1). the ground, mainly in association with Meteorological and air pollution data were obtained Graphis handelii Zahlbr. and scattered thalli from the Japan Meteorological Agency and the National of Lecanora pulverulenta Müll. Arg. and Institute for Environmental Studies respectively; it Pertusaria pertusa (L.) Tuck. should be noted that the distances between the Botanical Garden and the meteorological and air pollution The distinctive phytogeographical dis- monitoring stations are 5·5 and 8·1 km, respectively. tribution pattern of pantropical species in Japan is delimited south of the 15 °C annual Glyphis cicatricosa is characterized by its isothermal line (with a mean annual mini- greyish white or brownish thallus with crow- mum of −3·5 °C), known as the ‘Crinum ded lirellae formed in rounded to elliptical Line’; this is based on the distribution pseudostromata; lirellae with open discs that of Crinum asiaticum L. var. japonicum are covered with brownish pruina; clear Baker, a vascular plant belonging to the hymenium; 8-spored asci with hyaline spores Amaryllidaceae (Koshimizu 1938). Many This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http:// creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. Downloaded from https://www.cambridge.org/core. IP address: 170.106.33.19, on 26 Sep 2021 at 04:35:28, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S0024282917000111 292 THE LICHENOLOGIST Vol. 49 17 16 15 14 13 12 Annual mean temperature (°C) 11 10 1980 1985 1990 1995 2000 2005 2010 2015 Year FIG. 1. Mean annual temperature in Tsukuba-city, 1984 to 2015, at the monitoring station located 5·5 km S of the Botanical Garden (Japan Meteorological Agency; http://www.jma.go.jp/). Dashed line represents the threshold 15 °C isotherm, the ‘Crinum Line’, which correlates approximately with the distribution of Glyphis cicatricosa. organisms have similar distribution patterns been many studies which have suggested in Japan including pantropical lichens which, that an increase in mean temperature, for according to Sato (1959), are generally dis- example through ‘global warming’, will influ- tributed in the warmer areas to the south of ence lichen distribution (e.g. van Herk the 15 °C annual isothermal line. Glyphis et al. 2002; Seaward 2004; Ellis et al. 2007, cicatricosa in Japan (Fig. 2) is clearly pan- 2015; Aptroot 2009; Hauck 2009; Bengtsson tropical, with a mainly tropical and sub- & Paltto 2013; Davydov et al. 2013; tropical distribution and only sporadic Semenova et al. 2015). Northward shifts in records from adjacent warm-temperate distribution in Japan, as seen in G. cicatricosa, regions (see Kurokawa 2006). Other pan- have already been reported in various plants tropical lichen species in Japan are repre- and animals (Kitahara et al. 2001; Murakami sented by, for example, Dictyonema sericeum et al. 2007; Japan Weather Association 2013). (Sw.) Berk., D. moorei (Nyl.) Henssen, Therefore, the relatively recent occurrence of Lecanora leprosa Feé, Sticta gracilis (Müll. G. cicatricosa,aswellasL. leprosa, in Tsukuba- Arg.) Zahlbr. and S. duplolimbata (Hue) city could be explained in terms of ‘global Vain. (Sato 1959; Kurokawa 2006). Of these warming’, exacerbated by an ‘urban heat pantropical species, only L. leprosa and island’ effect. However, the documented dis- G. cicatricosa have been found in Tsukuba- tribution shifts for lichens that can be linked to city (Ohmura 2016). global warming effects are still rather scanty, The higher air temperature created in urban and corroborative reports for a few species, as areas, the ‘urban heat island effect’, is well above, have some severe limitations in the known (e.g. McCarthy et al. 2010; Kusaka degree to which they can be generalized. Due et al. 2012) but it has not been widely recog- to dramatic reductions in air pollution in nized as contributing directly to lichen dis- many cities worldwide, as exemplified by tribution (Coppins 1973), mainly due to the Tsukuba-city (Fig. 4) and other cities in Japan overriding impact of air pollution. In arid or (Ohmura et al. 2008, 2012, 2014), lichen dis- sub-arid climates, both air pollution and tribution patterns no longer demonstrate a drought can affect lichen distribution, as clear relationship with sulphur dioxide. This demonstrated by Nimis (1985). There have leads to a multivariate process involving urban Downloaded from https://www.cambridge.org/core. IP address: 170.106.33.19, on 26 Sep 2021 at 04:35:28, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S0024282917000111 2017 Short Communications 293 °C 24 22 20 18 16 14 FIG.2.DistributionmapofGlyphis cicatricosa in Japan, with records from Tsukuba-city (★) and other localities (●); mean annual temperature from 1981 to 2010 delineated (Japan Meteorological Agency; http://www.jma.go.jp/). heat islands which potentially represent higher Amakubo, Tsukuba-city (36°06'03''N, 140°06'43''E), latitude refugia for the colonization of species on bark of Phellodendron amurense, 20 m elev., 2015, that are shifting their distributions as a con- Y. Ohmura 11001 (TNS). Prov. Izu (Pref. Shizuoka): Mishima, 1928, Y. Asahina 196 (TNS). Prov. Tohtomi sequence of global warming. Investigating this (Pref. Shizuoka): Saruwatari, Aigusa-mura, Ogasa-gun, phenomenon is facilitated by declining levels 7 vii 1932, G. Hashimoto s. n. (TNS). Prov. Izumi (Pref. of pollution in urban areas where lichen reco- Osaka): Kami-Kyoshi, Kyoshi-mura, Semnan-gun, lonization is of particular interest to 1954, M. Togashi 549056 (TNS). Kyushu, Prov. Buzen (Pref. Fukuoka): Nakatsumiya, Ohshima, Munakata- biogeographers. gun, on tree bark, 20 m elev., 8 viii 1960, W. Yoshitake s. n. (TNS). Prov. Bungo (Pref. Ôita): Nishi-Arita-mura, Representative specimens examined. Japan: Honshu, Hita-gun, 21 ii 1922, Nakayama s. n. (TNS). Prov. Prov. Hitachi (Pref. Ibaraki): Tsukuba Botanical Garden, Hyuga (Pref. Miyazaki): Nakaura, Nishi-Benbun, Downloaded from https://www.cambridge.org/core. IP address: 170.106.33.19, on 26 Sep 2021 at 04:35:28, subject to the Cambridge Core terms of use, available at https://www.cambridge.org/core/terms. https://doi.org/10.1017/S0024282917000111 294 THE LICHENOLOGIST Vol. 49 A B C FIG.3.Glyphis cicatricosa, Tsukuba Botanical Garden. A, habitat; B, location on Phellodendron amurense indicated by arrow, associated mainly with Graphis handelii; C, thallus. Scale: C = 2 mm. Nichinan, 1955, S. Kurokawa 550087 (TNS); (TNS); Sakamine, Kikai-jima, on bark of Casuarina Uto Shrine, Minami-Naka-gun, 1955, S. Kurokawa equisetifolia, 1988, H. Kashiwadani 35650 (TNS). 550117 (TNS). Izu Islands (Tokyo Metropolis): Specimens noted in references but not examined. Japan: Tairo-pond, Miyake Island, 1976, H. Kashiwadani Prov. Hizen (Pref. Nagasaki): Arikawa, Arikawa-cho, 120 m 13710 (TNS). Bonin Islands (Tokyo Metropolis): elev., [undated], M.
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