Journal of Threatened Taxa |
www.threatenedtaxa.org | 26 April 2022 | 14(4): 20848–20858
ISSN 0974-7907
(Online) | ISSN 0974-7893 (Print)
https://doi.org/10.11609/jott.7485.14.4.20848-20858
#7485 | Received 02
June 2021 | Final received 02 March 2022 | Finally accepted 07 March 2022
Distribution of the genus Pinguicula
(L., 1753) (Lentibulariaceae) in Gunma Prefecture,
Japan with new records
Hiro Shimai
1 & Takehiro
Ohmori 2
1 Tokyo Metropolitan Board of
Education, 2-8-1, Nishi-Shinjuku, Shinjuku-ku, Tokyo
163-8001, Japan.
2 Gunma Museum of Natural History,
1674-1, Kamikuroiwa, Tomioka, Gunma 370-2345, Japan.
1 shimaihiro@gmail.com
(corresponding author), 2 ohmori@gmnh.pref.gunma.jp
Editor: Anonymity
requested. Date of publication:
26 April 2022 (online & print)
Citation: Shimai,
H. & T. Ohmori (2022). Distribution of the genus Pinguicula
(L., 1753) (Lentibulariaceae) in Gunma Prefecture,
Japan with new records. Journal of Threatened
Taxa 14(4): 20848–20858. https://doi.org/10.11609/jott.7485.14.4.20848-20858
Copyright: © Shimai
& Ohmori 2022. Creative Commons Attribution
4.0 International License. JoTT allows unrestricted use, reproduction, and
distribution of this article in any medium by providing adequate credit to the
author(s) and the source of publication.
Funding: The authors
receive no fundings for this project.
Competing interests: The authors
declare no competing interests.
Author details: Hiro Shimai—Tokyo Metropolitan Board of Education (present); PhD from University of
Kent (2017); Chief curator at Takamori Botanical
Garden (2000–2010); MPhil from University of Nottingham (1988). Takehiro Ohmori—Herbarium Staff and Educator at Gunma Museum
of Natural History (present); Ph. D. from Graduate School of Science and
Engineering, Ibaraki University (2009). Department of Science, Chiba University
(1988).
Author contributions: Both authors equally contributed
to the field surveys, data collection, and the preparation of this manuscript.
Acknowledgements: The authors are grateful to
curators of herbaria for permission to study herbarium specimens. Thanks are
also due to Dr. Atsushi Ebihara
(National Museum of Nature and Science, Tsukuba, Japan) for providing the
digital image of the specimen presented in this paper.
Abstract: We studied the distribution of
two Pinguicula (Butterwort) species in Gunma Prefecture, Japan, based on
our herbarium specimen examinations and field observations. As a result,
several localities of Pinguicula macroceras,
such as Mt. Akagi-yama and the Tanigawa
Mountain Range, have been confirmed to exist . In addition, two new localities
of P. macroceras, Mts. Hotaka-yama
and Ojikazawa-no-kashira,
which had not been previously recorded, were found. However, only a single
locality of P. ramosa, a threatened species
(Endangered in the Red List of Gunma Prefecture and Vulnerable in the Red List
of the Ministry of the Environment of Japan), was confirmed to be present in
the prefecture. The two species have extremely narrow environmental preferences
and are restricted to specific environmental niches. The population size of
both species at each microhabitat is small and there is a potential risk of
disappearance of those localities in the future by the impacts of environmental
stress or human activities. This study documents the current situation of the
genus in Gunma Prefecture and suggests that urgent conservation is necessary to
protect both the two species and their habitats in the prefecture.
Keywords: Distribution of Pinguicula,
flora of Gunma, habitat, Lentibulariaceae, P. macroceras, P. ramose
Introduction
Species of the genus Pinguicula
L. (1753) (Lentibulariaceae) are relatively small
herbs basically forming basal rosettes with adhesive carnivorous leaves. Over
90 species are distributed in Eurasia, North and South America, the Caribbean
Islands, and Morocco (Casper 1966; Fleischmann & Roccia
2018), and approximately half of which are found in Mexico (Zamudio 2005). At
least two species, P. macroceras Link (1820)
and P. ramosa Miyoshi (1890), occur in Japan.
In general, those species are found in nutrient-poor wet soil where other plant
species are scarce.
Pinguicula macroceras was often treated as P.
vulgaris L. var. macroceras (Link) Herder
by Japanese botanists, but it is recognized as a distinct species in recent
years (after Casper 1962). P. macroceras is
widely distributed in the northern Pacific region, including Japan, the Kurils,
Sakhalin, the Aleutians, Alaska, and western Canada to northern California. The
holotype of the species, collected in Unalaska, Alaska and deposited in Botanic
Garden and Botanic Museum Berlin (B), was lost during WWII (Casper 1962); however,
the lectotype was recently designated by Domínguez et al. (2017).
The southernmost distribution of P.
macroceras known in Japan is a limestone cliff at
Mt. Ishidate-yama on the border of Kochi and
Tokushima Prefectures, Shikoku Island (Yamanaka 1953; Komiya & Shibata
1998). In literature, the Botanical Society of Japan (1888) reported that R. Yatabe and some other botanists observed Pinguicula
sp. (most likely P. macroceras) on Mt. Ishizuchi-san in Ehime Prefecture, which could be the
westernmost distribution of the species; however, no specimens from the
mountain have been found so far. Many
localities are known particularly in the Chubu region (central Japan,
particularly in Nagano Prefecture) and farther north. Pinguicula macroceras in the country are mostly restricted to
occurring in higher mountains or deep gorges (Komiya & Shibata 1998). The
species exceptionally occurs at low altitudes of 140–200 m along rivers in Gosen, Niigata Prefecture (Katagiri
1980; Komiya & Shibata 1998). The species is often found on limestone or
serpentine rocks in the Chubu region and farther south while it is also found
in peat or silt in northern Japan. The species is a relic species in the
postglacial era (Komiya & Shibata 1998).
Pinguicula ramosa, described by Manabu Miyoshi, is
endemic to Japan, specifically in Gunma and Tochigi Prefectures. It is confined
to altitudes of 1,400–2,300 m in only a few mountains around Nikko City. The
authority is often treated as P. ramosa
‘Miyoshi ex Yatabe’ since Casper’s (1966) taxonomic
monograph of the genus; however, it is correctly P. ramosa
‘Miyoshi’ (Shimai 2016). The voucher specimen stamped
as ‘TYPUS’ in Koishikawa Botanical Garden, University
of Tokyo (TI) was designated as the lectotype by Domínguez et al. (2017). The
species is restricted to specific mountains in Gunma and Tochigi Prefectures,
and the threatened status is Vulnerable (Ministry of the Environment of Japan
2020) and Endangered in Gunma Prefecture (Gunma Prefecture 2018). It is often
found on vertical or overhanging cliffs formed by weathered tuff breccia. The
habitat in Mt. Koshin-zan in Tochigi Prefecture,
where the species were first discovered, is strictly protected as a special
rank of the Natural Monument. Regarding the taxonomic rank, Tamura (1953) treated
that it was an infraspecific taxon of P. villosa
L. (1973), i.e., P. villosa L. var. ramosa (Miyoshi) Tamura (1953). However, P. ramosa is a distinct species morphologically (Komiya
and Shibata 1998), cytologically (Casper and Stimper
2009), and phylogenetically (Shimai et al. 2021).
Gunma Prefecture (area of 6,362
km2) is in the northern part of the Kanto region. The prefecture
roughly has the Kanto Plain in the south and mountain ranges in the north. It
is an inland prefecture without coastlines but there are many sources of the
Tone-gawa River System. The climate of the prefecture
is affected by both the Pacific Ocean side and the Sea of Japan side. Although
the number of localities of P. macroceras in
Gunma is fewer than that in neighboring Nagano or
Niigata Prefecture, Gunma is biogeographically important because it borders the
two prefectures, which geologically divide Western and Eastern Japan. Gunma and
Tochigi are the only prefectures where the two Pinguicula species
certainly occur. In Tochigi, P. macroceras is
recorded from only two mountains, Mt. Nikko-Shirane-san
and Mt. Nantai-san. Although more localities of P.
macroceras are known in Gunma than Tochigi, the
population size at each locality in Gunma is small and there is a risk of
habitat reduction. Many high mountains and deep gorges prevent the thorough
investigation of flora in Gunma, resulting in insufficient research in such
inaccessible areas. In this study, we document the distribution of Pinguicula
including both earlier records as well as newly found ones in Gunma Prefecture
by our recent investigations to prevent the disappearance of the species.
Materials
and Methods
Herbarium specimens housed in
museums and botanical gardens in the world were studied (mainly 2013-–2020) and
specimen data on the labels such as localities, collected years, and collectors
were gathered. The localities in Gunma are summarized in Table 1, but detailed
locations or coordinates are omitted to protect the habitats. After 1900, it
was divided every 10 years, and collection records, if any, at each locality
were presented in the table. The elevation and coordinate of each mountain are
obtained from the database of the Geospatial Information Authority of Japan
(https://www.gsi.go.jp/top.html), and those are of a representative peak of
each mountain but do not necessarily indicate the exact location where the
species can be found. A distribution map was produced based on the specimen
records using GeoCat, Geospatial Conservation
Assessment Tool (Royal Botanic Gardens, Kew; http://geocat.kew.org/), and the
extent of occurrence (EOO) and the area of occupancy (AOO) were calculated by
the program. The AOO was calculated by the default parameter of 2 km × 2 km (=
4 km2). Two or more microhabitats close to each other (e.g., within
100 m) or two or more collection records from the same area were treated as a
single locality. The coordinate datasets on GeoCat
were then transferred to QGIS 3.14 to produce a distribution map (Figure 1).
Even if other localities were found on literature or internet source, those
were not recognized in this study unless specimens from there were found.
Results
Specimens of Pinguicula
collected in Gunma Prefecture were mostly found at herbaria in Japan, such as
GMNHJ, KYO, TI, and TNS. Localities recognized are summarized in Table 1 and
are individually discussed below.
Pinguicula macroceras Link
1. Mt. Akagi-yama
(1,828 m, 36.560278, 139.193333) (Image
1A, B)
Mt. Akagi-yama
(or also called Akagi-san), located ca. 20 km north-east of Maebashi, the
prefectural capital of Gunma, is one of the symbolic mountains of the
prefecture. It is a complex volcano although no volcanic activities have been
recorded for ca. 30,000 years (Kobayashi & Nakamura 2001). The somma consists of several peaks including Kurobi-san (1,828 m; the highest peak of the mountain), Komagatake (1,685 m), and Jizo-dake
(1,674 m). There are a few lakes and ponds, e.g., Lakes Ono (or Onuma) and Kono (or Konuma), in the caldera.
In the mountain, the specimens of
P. macroceras were collected mainly from Kurobi-san and Jizo-dake Peaks,
but the former has no collection records after the 1930s. The specimens have
been collected repeatedly from the latter peak and the species is present near
the summit; however, the population size is declining rapidly since the soil
there is getting dry. It was commonly seen at Jizo-dake
Peak in the early 2000s but was only ca. 50 individuals in 2019. At Jizo-dake Peak, the species is found only in eroded wet
black soil. The habitat is above the forest line with good sunlight which may
result in dry soil and the consequent decline of population size. There are
several herbarium specimens that say only ‘Mt. Akagi-yama’
on the labels (i.e., not specified exact peaks or locations).
Although no specimens have been
found so far, Hattori (1908) wrote that numerous plants of P. macroceras were seen at Komagatake
and Choshichiro-dake Peaks in the mountain. In July,
the summit of Kurobi-san was purple in color by the flower of the species (Hattori 1909). Pictures
in the book of Hattori (1908) showed that the summit of Kurobi-san
was an open grassland at that time while the summit is mostly surrounded by
trees, today. No plants were found at these peaks in our recent surveys.
2. Mt. Nikko-Shirane-san
(2,578 m, 36.798611, 139.375833 ) (Image 1C, D)
Mt. Nikko-Shirane-san,
a stratovolcano, is located on the border of Gunma and Tochigi Prefectures. It
is the highest mountain in the Kanto region and northern Japan. The mountain is
officially Shirane-san, but there are some other
mountains that have the same name, so it is often called Nikko-Shirane-san to specify. The mountain, characteristically
dome-shaped, is located in the western part of Nikko National Park (114,908
ha).
Due to ancient volcanic
activities, a few lakes and ponds have been formed. Relatively large numbers of
P. macroceras are seen on the Tochigi side of
the mountain. There was a record of the species from the Gunma side in
literature, but it was thought to be extinct (Moriya 1976). However, we confirmed
in 2019 that the species was still present there although less than 30
individuals. It grows among grasses so it may be difficult to find them unless
they are in flower. Concerning its small population size, they may disappear
from there in the future.
3. Oze
National Park
Oze, highland wetlands on the Gunma,
Niigata, and Fukushima prefectural borders, was formed by volcanic activities
of Mt. Hiuchigatake (2,356 m) ca. 10,000 years before
present. It roughly consists of Ozegahara (peatland),
Oze-numa Pond, and a few mountains including Mts. Hiuchigatake and Shibutsu-san.
Wetlands and ponds in a plateau provide characteristic vegetation with many
rare and endemic plant species. Oze and its
surroundings have been designated as Oze National
Park (37,200 ha). It is an area that symbolizes the conservation of nature in
Japan. At least two localities of P. macroceras,
Ayame-daira and Mt. Shibutsu-san,
are known in Oze.
(a ) Ayame-daira
(1,969 m, 36.900556, 139.244722)
Ayame-daira,
with a gentle peak and mountain peatlands, is located in the southern part of
the national park. Too many visitors caused erosions and it subsequently became
bare ground at the top of Ayame-daira in the 1950s.
Since the 1960s, a vegetation recovery program has been attempted by a few
organizations and is yet on the way; therefore, the wetland is strictly
protected. Some literature occasionally recorded that P. macroceras
occurred there but only a single herbarium specimen from there has been found
so far. We have confirmed in July 2020 that a small population of the species
is present there. There is a specimen from Ozegahara,
which might be collected at Ayame-daira (probably mislabeled), because the species is not present in Ozegahara.
(b) Mt. Shibutsu-san
(2,228 m, 36.903611, 139.173333)
Mt. Shibustu-san,
located at the westernmost of the national park, is composed of serpentines (Kawase et al. 2009). Some rare plant species (e.g., Japonolirion osense
Nakai and Arenaria
katoana Makino) are seen in the mountain (Tomimatsu et al. 2004; Kawase
& Yumoto 2006; Kawase
et al. 2009). There are many P. macroceras
specimens previously collected at the mountain. Some location names on the northeastern slope of the mountain are specified on the
specimen labels, but those could be within the same area. There is a specimen
from the northwestern slope, but the area is
designated as an environmental protection area by Gunma Prefecture and is
restricted to access there. There were many specimens that say only ‘Mt. Shibutsu-san’ on the labels.
4. Naramata-gawa
River watershed
Naramata-gawa River, which is upstream of
Tone-gawa River, is originated in the Echigo Mountains. The area belongs to Minakami
township in Gunma. P. macroceras was collected
at one of the branch streams of Naramata-gawa River
in 2003. There is another collection record from somewhere along Naramata-gawa River in 1955, but it is unclear if this
location is identical with the former. No recent information is available.
5. Mt. Hotaka-yama
(2,158 m, 36.805278, 139.132500 ) [New record] (Image 2A)
Mt. Hotaka-yama
is often called Joshu-Hotaka-yama to distinguish it
from Mt. Hotaka-dake (3,190 m; the third highest
mountain in Japan) on the prefectural border of Gifu and Nagano. Mt. Hotaka-yama, an old volcanic mountain, is an independent
peak located at the south of Mt. Shibutsu-san.
The specimen of P. macroceras was recently collected at the south-facing
slope of Mt. Hotaka-yama on 16 August 2016 by T. Ohmori
and H. Yoshii which is deposited in Gunma Museum of Natural History (GMNHJ). It is too dangerous to go off the mountain
trails and the activities of researchers are restricted as there are many
cliffs along streams and above the subalpine zone. Furthermore, there are many
areas and mountains nearby, such as Oze, the Tanigawa Mountain Range, and Mt. Nikko-Shirane-san,
which are more important in the field of botany, resulting in less exploration
by botanists in Mt. Hotaka-yama. Those might be
reasons why the species had not been discovered in the mountain until
2016.
6. Tanigawa
Mountain Range
Strictly speaking, the Tanigawa Mountain Range is a part of the Mikuni Mountain
Range. The Tanigawa Mountain Range, with several
mountains, is on the prefectural border of Gunma and Niigata (sometimes called
‘jo-etsu kokkyo’), and it
depends on literature which mountains are included in the mountain range. In
this study, it is defined that the range is from Mts. Asahi-dake
and Kasagatake in the east to Mt. Tairappyo-yama
in the west. Those mountains are connected by the Gunma ridge trail.
(a) Mt. Asahi-dake
(1,945 m, 36.880556, 138.97250 )
Mt. Asahi-dake
is located in the eastern part of the mountain range. The specimen of P. macroceras was collected at the mountain in 1976 and
1981, but the specimen label did not show any exact location. No recent
specimens have been found; however, the species is present according to
information from climbers who visited the mountain. The species also occurs on
Shimizu-toge Pass, on the Niigata side, ca. 2 km
north-west of the summit of Mt. Asahi-dake.
(b) Mt. Kasagatake
(1,852 m, 36.869444, 138.962778)
Mt. Kasagatake
(or Mt. Okura-yama) is located ca. 1.5 km south-west
of Mt. Asahi-dake. The specimen of P. macroceras was collected in 1965, and it is the only
specimen found so far. The specimen label specifies as ‘between Okura and Kasagatake’, which is probably somewhere on a trail between
Okura-one Ridge and the summit of Mt. Kasagatake (the
trail is disused today). It is not confirmed whether the species is still
present there.
(c) Mt. Tanigawa-dake
(1,977 m, 36.837222, 138.930000 (Image
1E, F)
Mt. Tanigawa-dake,
a serpentinous mountain, is located on the
prefectural border of Gunma and Niigata. The mountain possesses two
characteristic peaks, which are Oki-no-mimi (1,977 m)
and Toma-no-mimi (1,963 m).
A few localities of P. macroceras can be found
around the peaks. Those microhabitats are covered by grasses; therefore, it is
somewhat difficult to find the species unless they are in flower. There are not
many individuals, often <50, within each microhabitat. There is a potential
risk that they may disappear from there in the future due to ecological
succession. Some other populations can be seen on a vertical cliff on the
northeast side of the mountain, but it is impossible to approach there without
climbing equipment.
(d) Ojikazawa-no-kashira (1,840 m, 36.829167, 138.912500) [New record]
(Images 1G, H, 2B)
Ojikazawa-no-kashira
is located between Mts. Tanigawa-dake and Mantaro-san (ca. 1.5 km west of the former). The north side
of the mountain trail belongs to Niigata Prefecture. P. macroceras
had not been collected before, but only a few plants were newly discovered in a
grassland near the summit of the Gunma side on 07 July 2019, which the specimen
collected by H. Shimai has been deposited in the
National Museum of Nature and Science (TNS). There is a risk that the species
could potentially disappear from there in the future since the locality is
densely covered by grasses which is unfavorable for P.
macroceras.
(e) Mt. Mantaro-san
(1,954 m, 36.824167, 138.879167)
Mt. Mantaro-san,
ca. 5 km west of Mt. Tanigawa-dake, is located on the
Gunma ridge trail to Mt. Tairappyo-yama. Because of
the relatively long trail, botanists rarely access the area. Approximately 100
plants were found on the ridge below the peak on 07 July 2019. This locality is
about on the prefectural border of Gunma and Niigata. The microhabitat is also
covered by grasses due to ecological succession , and the population may
disappear in the future. It is unclear whether it is identical to the location
below.
There was an earlier collection
record of the species in the back of Kawafuru-onsen
Spa. Although the exact location is unknown, it is assumed that it may be
between a headwater stream of Akaya-gawa River and
the ridge on the prefectural border, or near the ridge. The area is on the
south slope of Mt. Mantaro-san, but the trail between
the spa and the ridge is very long and rugged, requiring crossing streams;
therefore, botanists usually do not enter such a tough route.
(f) Mt. Tairappyo-yama
(1,984 m, 36.817500, 138.821667)
Mt. Tairappyo-yama,
at the western edge of the Tanigawa Mountain Range,
stands on the prefectural border of Gunma and Niigata, and it has peatlands
near the summit (Sasaki & Kariya 2000). P. macroceras was collected from two locations on the
Gunma side, but our surveys in 2018 and 2019 failed to find the species along
the mountain trail. It may be possible that the species is still present away
from the trail. Although we have not accessed the specimens, the species was also
collected on the Niigata side of the mountain (Katagiri
1980).
7. Mt. Arafune-yama
(1,423 m, 36.203889, 138.637222)
Mt. Arafune-yama,
with a massive vertical rock cliff, is in the western part of Gunma (on the
prefectural border of Gunma and Nagano). The existence of P. macroceras, collected on the Gunma side only once in
1960, was confirmed by the specimen only. No detailed location was mentioned on
the specimen label except the name of the mountain. It is unclear whether the
species is still present there; however, it is almost impossible to search for
plants on the inaccessible massive rock cliff. The locality is not only the
westernmost but also the southernmost for the species in Gunma.
Pinguicula ramosa Miyoshi
8. Mt. Kesamaru-yama
(1,961 m, 36.649444, 139.327222) (Image 1I, J)
Mt. Kesamaru-yama,
a volcanic mountain on the prefectural border of Gunma and Tochigi, is located
at the westernmost of the Ashio Massif. Mt. Kesamaru-yama consists of a few peaks. The highest peak is
a point at 1,961 m (no name for the peak), north of Ato-Kesamaru
Peak (1,908 m). The species occurs on both Gunma and Tochigi sides of the
mountain.
Ato-Kesamaru Peak is the only place where P.
ramosa occurs in Gunma. Only four specimens from
the Gunma side were confirmed to exist. Although there were a few other
specimens saying only ‘Mt. Kesamaru-yama’ on the
specimen label, no prefecture was specified. The species can be seen only on a
vertical cliff of weathered tuff breccia on the mountain as also seen on Mts. Koshin-zan and Nantai-san in
Tochigi. The species basically occurs below the tree line, but the habitat on
the Gunma side has good sunlight compared with localities in Tochigi. The
habitat receives direct sunlight in the morning, which may cause dry out the
soil of the microhabitat. Minor collapses of the cliff seem to be relatively
common, which may affect the habitat of the species. No P. macroceras has been found on Mt. Kesamaru-yama.
Distribution areas of Pinguicula
in Gunma
In P. macroceras
in Gunma, the EOO calculated by GeoCat was 2,458 km2
and the AOO was 64.0 km2, both of which suggested Endangered
although the species is not listed in the Red List of Gunma Prefecture. The
area of Gunma Prefecture is ca. 6,362 km2; therefore, the EOO covers
one-third of the prefecture. Although the GeoCat
instruction suggests that it is possible to evaluate the threatened category at
a regional level, it needs further studies whether this method can be
applicable for such a widespread species. On the other hand, P. ramosa occurs only in a single locality in Gunma
Prefecture, which is unable to calculate the EOO by GeoCat
since the program requires at least three locations to evaluate the status.
However, it is apparent that P. ramosa is an
endangered species in Gunma.
Discussion
The localities of Pinguicula macroceras within Gunma Prefecture are mostly
restricted to above the subalpine zone, 1,500 m or higher, in the north (Figure
1). If some other localities outside of Gunma (e.g., Mts. Asama-yama and Iwasuge-yama in Nagano
and Mt. Nantai-san in Tochigi) are included, those
surround the northern half of Gunma Prefecture. The species is often found in
alkaline soil (e.g., limestone or serpentine outcrops) in the Chubu region or
farther south. However, the environmental preference of P. macroceras in Gunma is similar to that in the Tohoku
region (e.g., in Mts. Akita-Komagatake, Nyuto-zan, and Hachimantai). P.
macroceras in Gunma Prefecture tends to be found
in acid peaty soil near snow patches or stream banks rather than alkaline soil,
where the species is more often seen in the Chubu region and farther south
(particularly at lower altitudes). It is highly possible that the species grows
in extreme environments to avoid survival competitions with other plant
species, but it may not strictly depend on the soil pH level. It is also
probable that increasing pioneering plants, such as grasses, sasa bamboos, and tall herbaceous plants (i.e., ecological
succession) in the habitats, or erosions along mountain trails would be more
serious causes for declining populations of P. macroceras.
Furthermore, natural disasters, including heavy rains or furious typhoons,
which tend to be increasing in recent years, may cause the distraction of the
locality due to landslides.
Kurobi-san, one of the peaks at Mt.
Akagi-yama, used to be famous for P. macroceras; however, the species has totally
disappeared from there already. There is no recent information whether the
species is still present in some localities (e.g., Mt. Arafune-yama)
due to remote areas or inaccessible cliffs. Most of the localities of P. macroceras are within national parks, which are
protected by law. Even within the protected areas, the microhabitats are
covered by grasses (e.g., Mt. Tanigawa-dake), which
are unfavorable for the species. In the current
study, we report two new localities, but many localities in Gunma Prefecture
have a small number of the species.
Regarding Pinguicula ramosa, large colonies were seen on both the Gunma and
Tochigi sides of Mt. Kesamaru-yama before; however,
those rapidly shrank in the last 50 years (Hiroshi Masuda pers. comm. vi.2019).
On the Gunma side, we recently observed only a small number of P. ramosa plants on a vertical rock face. It is unclear
how many plants are present there, but it is no doubt that the population size
is very small. Dry soil and corruption of the rock face may cause the
extinction of species on the Gunma side.
In addition, the localities of P.
macroceras in other prefectures near the Gunma
border are Mts. Asama-yama and Iwasuge-yama
in Nagano, Nakatsu-gawa River in Saitama, Mts. Nantai-san and Nikko-Shirane-san
in Tochigi. The localities of P. ramosa
outside of Gunma are Mts. Kesamaru-yama, Nokogiri-yama, Koshin-zan, Nyoho-san, and Nantai-san in
Tochigi.
Concerning the EOO in P. macroceras, it covers one-third of the area of Gunma
Prefecture, but the status of the species including P. ramosa
is not optimistic. Further studies of both species and their urgent
conservation act in Gunma Prefecture are necessary. The current situation of
the two species is recorded above, but there may be unknown localities in high
mountains or deep gorges.
Specimens examined
Pinguicula macroceras Link, Jahrb.
Gewächsk. 1: 54 (1820).
JAPAN. Gunma: Mt. Akagi-yama, 20.vii.1952, Okuyama 10148
(TNS; as P. vulgaris); 04.vi.1961, Komiya s.n.
(TNS); 01.viii.1962, Tanaka s.n. (GMNHJ; as P.
vulgaris var. macroceras); 29.vi.1999,
Shibata s.n. (TNS); 18.vi.2000, Komiya & Shibata s.n. (TNS). Mt. Akagi-yama, Jizo-dake, 26.vii.1948, Tanaka s.n.
(GMNHJ; as P. vulgaris var. macroceras);
30.vii.1950, Komiya s.n. (TNS); vi.1951, Komiya s.n. (TNS); vi.1952, Komiya s.n.
(TNS); 13.vi.1954, Higuchi s.n. (GMNHJ; as P.
vulgaris var. macroceras); 1,400 m,
19.vi.1965, Fukuoka & Naruhashi 20 (KANA, KYO; as
P. vulgaris var. macroceras); ca. 1,650
m, 08.vi.2001, Shimai s.n.
(Nippon Dental Univ.); 1,640 m, 05.vi.2004, Yoshii s.n.
(GMNHJ; as P. vulgaris var. macroceras);
1,660 m, 17.vii.2018, Shimai s.n.
(TNS). Mt. Akagi-yama, Kurobi-san,
25.vii.1903, Hayata s.n.
(SAPS, TI; as P. vulgaris); 09.viii.1927, Kojima s.n.
(GMNHJ; as P. vulgaris var. macroceras);
12.vii.1928, Hara s.n. (TI; as P. vulgaris);
25.vii.1930, Shiobara s.n.
(GMNHJ; as P. vulgaris var. macroceras);
15.vi.1934, Saito s.n. (GMNHJ; as P. vulgaris
var. macroceras); 16.vi.1934, Fukushima s.n. (GMNHJ; as P. vulgaris var. macroceras).
Mt. Akagi-yama, between Onuma
Lake and Jizo-dake, 1,400–1,700 m, 15.vi.1969, Konta 7707 (TNS; as P. vulgaris). Mt. Arafune-yama, 20.ix.1960, Satomi s.n.
(TNS; as P. vulgaris). Mt. Asahi-dake,
24.vii.1976, Yoshizawa 761 (TNS; as P. vulgaris); 14.vii.1981, Haginiwa JH033382 (TNS; as P. vulgaris var. macroceras). Mt. Hotaka-yama,
16.viii.2016, Ohmori and Yoshii 12056 (GMNHJ; as P.
vulgaris var. macroceras). Mt. Mantaro-san, 07.vii.2019, Shimai s.n. (TNS). Minakami, Upper
stream of Kawafuru-onsen Spa; vi.1976, Miyamae s.n. (GMNHJ; as P. vulgaris var. macroceras).
Minakami, branch of Naramata-gawa
River, 1,290 m, 25.viii.2003, Ohmori et al. 3540
(GMNHJ; as P. vulgaris var. macroceras).
Naramata-gawa River, upper stream of Tone-gawa River, 20.vi.1955, Matsuda s.n.
(TI). Mt. Nikko-Shirane-san, 21.vii.2019, Shimai s.n. (TNS). near Ojikazawa-no-kashira Peak,
07.vii.2019, Shimai s.n.
(TNS). between Okura and Mt. Kasagatake, 29.vii.1965,
Miyamae s.n. (GMNHJ; as P. vulgaris var. macroceras). Oze, Ayamedaira, 23.vii.1947, Tanaka s.n.
(GMNHJ; as P. vulgaris var. macroceras).
Ozegahara, 23.vii.1951, Ikoshi
s.n. (TNS; as P. vulgaris). Mt. Shibutsu-san, 15.vii.1924, Takeda & Tatewaki
s.n. (SAPS); 16.vi.1929, Hara s.n.
(TI; as P. vulgaris); 13.viii.1931, Hoshi s.n.
(KYO); 09.viii.1935, Ohwi & Tagawa 301 (KYO);
04.vii.1941, Hurusawa s.n.
(TI; as P. vulgaris); 20.vii.1942, Satomi s.n.
(KANA; as P. vulgaris); 19.vii.1946, Nakai
2694 (KYO; as P. vulgaris); 2,100 m, 05.viii.1949, Kawasaki 4363 (TNS;
as P. vulgaris); 20.vii.1950, Tobe s.n. (GMNHJ; as P. vulgaris var. macroceras);
27.vii.1951, Komiya s.n. (TNS); 30.vii.1952, Tamura s.n. (KYO); vi.1954, Komiya s.n.
(TNS); 20.vii.1954, Asai s.n.
(TI; as P. vulgaris var. macroceras);
22.vii.1954, Oda s.n. (Tochigi Pref. Museum; as P.
vulgaris var. macroceras); viii.1954, Sugaya s.n. (TUS; as P.
vulgaris); 02.viii.1969, Miyamae s.n. (GMNHJ; as P.
vulgaris var. macroceras); 29.viii.1969, Oze Conservation Center of Gunma
Pref. s.n. (GMNHJ; as P. vulgaris var. macroceras). Northeastern
slope of Mt. Shibutsu-san, ca. 2,000 m, 17.vii.1950,
Mizushima s.n. (TI; as P. vulgaris var. macroceras); 30.viii.1950, Komiya s.n. (TNS); 1,900–2,000 m, 04.vii.2003, Shimai
s.n. (Nippon Dental Univ.). Northwestern
slope of Mt. Shibutsu-san, 1,600 m, 05.viii.2001, Ohmori & Yoshii 1797 (GMNHJ; as P. vulgaris var.
macroceras). Mt. Tairappyo-yama,
East side, 1,900 m, 21.vi.1959, Hara s.n. (TI). Mt. Tairappyo-yama, between Tairappyo-goya
Hut and summit, 12.vii.1957, Okuyama et al. 13691
(TNS). Mt. Tanigawa-dake, 1,900 m, 14.vii.1928, Hara
9602 (TI; as P. vulgaris var. macroceras);
06.vii.1948, Yamazaki & Ono 2913 (S, TI; as P. vulgaris);
08.viii.1949, Komiya s.n. (TNS); 08.vii.1951, Higuchi
s.n. (GMNHJ; as P. vulgaris var. macroceras); 24.vii.1951, Tobe
s.n. (GMNHJ; as P. vulgaris var. macroceras); 02.vii.1953, Kimura & Matsuda s.n. (TI; as P. vulgaris var. macroceras);
03.vii.1953, Komiya s.n. (TNS); 14.vii.1953, Kanai
382 (TI; as P. vulgaris var. macrocarpa);
vii.1966, Yamazaki s.n. (TI); 01.viii.1961, Suto s.n. (GMNHJ; as P.
vulgaris var. macroceras); 15.vii.1965,
Komiya s.n. (TNS); 20.vii.1999, Komiya & Shibata s.n. (TNS); ca. 1,950 m, 23.viii.2004, Shimai
s.n. (Nippon Dental Univ.); 03.viii.2018, Shimai s.n. (TNS); 07.vii.2019, Shimai s.n. (TNS). between Mt. Tanigawa-dake and Mt. Asahi-dake,
01.vii.1956, Harazawa s.n.
(KANA).
Pinguicula ramosa Miyoshi, Bot. Mag. (Tokyo) 4: 315
(1890).
JAPAN. Gunma: Midori, Mt. Kesamaru-yama, 14.vi.1974, Suto s.n. (GMNHJ); 29.vi.2003, Shibata s.n.
(Nippon Dental Univ.); 28.vi.2009, Yoshii et al. s.n.
(GMNHJ); 06.vi.2019, Shimai s.n.
(TNS).
Herbarium code: GMNHJ = Gunma
Museum of Natural History | KANA = Kanazawa University | KYO =
Kyoto University | S = Swedish Museum of Natural History | SAPS =
Hokkaido University Museum | TI = University of Tokyo | TNS =
National Museum of Nature and Science | TUS = Tohoku University.
All specimens in Nippon Dental
University have been transferred to TNS.
Table 1. Observed specimens of Pinguicula
in Gunma Prefecture. MAC = P. macroceras. RAM
= P. ramosa. Localities are listed in
alphabetical order. Numbers correspond with those in the text and Figure 1.
[New] = new record reported in this study. X = specimen collected during the
period. Voucher specimens are listed in the specimens examined section.
Species |
Locality in Gunma |
No. |
Specimen record |
|||||||||||
MAC |
Akagi-yama,
Mt. (Jizo-dake) |
1 |
|
|
|
|
X |
X |
X |
|
|
|
X |
X |
MAC |
Akagi-yama,
Mt. (Kurobi-san) |
1 |
X |
|
X |
X |
|
|
|
|
|
|
|
|
MAC |
Akagi-yama,
Mt. (w/o location) |
1 |
|
|
|
|
|
X |
X |
|
|
X |
X |
|
MAC |
Arafune-yama, Mt. |
7 |
|
|
|
|
|
|
X |
|
|
|
|
|
MAC |
Asahi-dake,
Mt. |
6 (1) |
|
|
|
|
|
|
|
X |
X |
|
|
|
MAC |
Ayame-daira |
3 (1) |
|
|
|
|
X |
X? |
|
|
|
|
|
|
MAC |
Hotaka-yama, Mt. [New] |
5 |
|
|
|
|
|
|
|
|
|
|
|
X |
MAC |
Kasagatake, Mt. |
6 (2) |
|
|
|
|
|
|
|
|
|
|
|
|
RAM |
Kesamaru-yama, Mt. |
8 |
|
|
|
|
|
|
|
X |
|
|
X |
X |
MAC |
Mantaro-san, Mt. |
6 (5) |
|
|
|
|
|
|
X |
|
|
|
|
X |
MAC |
Naramata-gawa River |
4 |
|
|
|
|
|
X |
|
|
|
|
X |
|
MAC |
Nikko-Shirane-san,
Mt. |
2 |
|
|
|
|
|
|
|
|
|
|
|
X |
MAC |
Ojikazawa-no-kashira, Mt. [New] |
6 (4) |
|
|
|
|
|
|
|
|
|
|
|
X |
MAC |
Shibutsu-san, Mt. (NE
slope) |
3 (2) |
|
|
|
|
|
X |
|
|
|
|
X |
|
MAC |
Shibutsu-san, Mt. (NW
slope) |
3 (2) |
|
|
|
|
|
|
|
|
|
|
X |
|
MAC |
Shibutsu-san, Mt. (w/o
location) |
3 (2) |
|
|
X |
X |
X |
X |
X |
|
|
|
|
|
MAC |
Tairappyo-yama, Mt. |
6 (6) |
|
|
|
|
|
X |
|
|
|
|
|
|
MAC |
Tanigawa-dake, Mt. |
6 (3) |
|
|
|
|
|
|
|
|
|
|
X |
X |
MAC |
Tanigawa-dake, Mt. (w/o
location) |
6 (3) |
|
|
X |
|
X |
X |
X |
|
|
X |
|
|
|
|
|
1900-1909 |
1910-1919 |
1920-1929 |
1930-1939 |
1940-1949 |
1950-1959 |
1960-1969 |
1970-1979 |
1980-1989 |
1990-1999 |
2000-2009 |
2010-2019 |
For figure &
images - - click here
References
Botanical
Society of Japan (1888). Notes: Botanical field expedition to the Shikoku region. Botanical
Magazine, Tokyo 2: 202–204.
Casper, S.J.
(1962). On Pinguicula
macroceras Link in North America. Rhodora 64: 212–221.
Casper, S.J.
(1966). Monographie der gattung Pinguicula
L. Bibliotheca Botanica. 127/128.
Casper, S.J.
and R. Stimper (2009). Chromosome numbers in Pinguicula
(Lentibulariaceae): survey atlas, and taxonomic
conclusions. Plant Systematics and Evolution 277: 21–60.
Domínguez, Y., C.M.P. Valdés
& V.F.O. Miranda (2017). Typification of name in the genus Pinguicula
L. (Lentibulariaceae). Phytotaxa
312: 179–198.
Fleischmann,
A. & A. Roccia (2018). Systematics and evolution of Lentibulariaceae: I. Pinguicula. pp. 70–80. In:
Ellison A.M. & L. Adamec (eds.), Carnivorous
Plants: Physiology, Ecology, and Evolution. Oxford University Press.
Oxford.
Gunma
Prefecture (2018). Red List, Plants. revised in 2012 and partially revised in 2018.
https://www.pref.gunma.jp/contents/100071278.pdf
Downloaded on 01 December 2020.
Hattori, T. (1908). The
Carnivorous Plants. Ogawashoeido, Tokyo, 252pp.
Hattori, T. (1909). Carnivorous
Plants of Japan. Rokumeikan, Tokyo, 109pp.
Katagiri, Y. (1980). Pinguicula vulgaris L.
var. macroceras Herder, pp. 119–121. In:
Ishizawa S. (ed.), Distribution Maps of Plants of Niigata Prefecture, Vol.
1. No. 35. Niigata Jinenjyo-kai, Ojiya.
Kawase, D. & T. Yumoto
(2006). Clonal
structure and genetic differentiation in the serpentine plant Japonolirion osense
(Petrosaviaceae) using AFLP markers. Acta Phytotaxonomica et Geobotanica
57: 183–190.
Kawase, D., T. Yumoto
& K. Sato (2009). Phylogeography of a rare serpentine plant, Arenaria katoana
Makino (Caryophyllaceae). Acta Phytotaxonomica
et Geobotanica 60: 19–25.
Kobayashi, K.
& E. Nakamura (2001). Geochemical Evolution of Akagi Volcano, NE Japan: Implications for
interaction between island-arc magma and lower crust, and generation of
isotopically various magmas. Journal of Petrology 42: 2303–2331. https://doi.org/10.1093/petrology/42.12.2303
Komiya, S.
& C. Shibata (1998). Japanese Pinguicula (Lentibulariaceae).
Bulletin of Nippon Dental University, General Education 28: 117–146.
Ministry of
the Environment (2020). Red List 2020. http://www.env.go.jp/press/107905.html Accessed on 28 December 2020.
Miyoshi, M.
(1890). Notes on Pinguicula
ramosa sp. nov. Botanical
Magazine, Tokyo 4: 314–319.
Moriya, A.
(1976). Plants of
Tochigi, Shimotsuke-bunko 2, Gekkan-Satsuki-Kenkyusha,
Kanuma.
Sasaki, A.
& Y. Kariya (2000). Initiation age of a peaty soil
layer in the subalpine zone of Mount Tairappyo, the
Mikuni Mountains, Central Japan. Quarterly Journal of Geography 52:
283–294.
Shimai, H. (2016). Pinguicula ramosa
Miyoshi–a
botanical review. Carnivorous Plant Newsletter 45: 51–68. https://cpn.carnivorousplants.org/articles/CPNv45n2p51_68.pdf
Shimai H, H. Setoguchi,
D.L. Roberts & M. Sun (2021). Biogeographical patterns and speciation of the genus Pinguicula
(Lentibulariaceae) inferred by phylogenetic analyses.
PLoS ONE 16: e0252581. https://doi.org/10.1371/journal.pone.0252581
Tamura, M.
(1953). Key to the
insectivorous plants of Japan. Acta Phytotaxonomica
et Geobotanica 15: 31–32.
Tomimatsu, H., A. Hoya, H. Takahashi &
M. Ohara (2004). Genetic
diversity and multilocus genetic structure in the relictual endemic herb Japonolirion
osense (Petrosaviaceae).
Journal of Plant Research 117: 13–18. https://doi.org/10.1007/s10265-003-0121-7
Yamanaka, T.
(1953). Pinguicula
vulgaris var. macroceras Herd. newly found
in Shikoku. Journal of Japanese Botany 28: 30–31. https://jjbotany.com/pdf/JJB_028_30_31.pdf
Zamudio, S. (2005). Lentibulariaceae.
Flora del Bajío y de Regiones
Adyacentes 136: 1–61.