Journal of Threatened Taxa | www.threatenedtaxa.org | 26
February 2018 | 10(2): 11271–11284
Vascular plant
assemblage of cliffs in northern Western Ghats, India
Mandar N. Datar 1
& Aparna V. Watve 2
1 Biodiversity and Paleobiology
group, Agharkar Research Institute, G.G. Agarkar Road, Pune, Maharashtra 411004, India
2 Biome Conservation Foundation,
34/6, Gulawani Maharaj
Road, Pune, Maharashtra 411004, India
1 mndatar@aripune.org (corresponding
author), 2 aparnawatve1@gmail.com
doi: http://doi.org/10.11609/jott.3611.10.2.11271-11284
Editor: N.P. Balakrishnan,
Coimbatore, India. Date of publication:
26 February 2018 (online & print)
Manuscript details: Ms # 3611 |
Received 30 June 2017 | Final received 15 February 2018 | Finally accepted 18
February 2018
Citation: Datar, M.N. & A.V. Watve (2018). Vascular
plant assemblage of cliffs in northern Western Ghats, India. Journal of Threatened
Taxa 10(2): 11271–11284; http://doi.org/10.11609/jott.3611.10.2.11271-11284
Copyright: © Datar & Watve 2018. Creative Commons Attribution 4.0
International License. JoTT allows
unrestricted use of this article in any medium, reproduction and distribution
by providing adequate credit to the authors and the source of publication.
Funding: Agharkar Research Institute
In-house grant BOT 15 for MND and self-funded by AW.
Competing interests: The authors declare no competing interests.
Author Details: Dr. Mandar Datar works as a scientist,
is interested in diversity, distribution and endemism of flowering plants of
the northern Western Ghats. Dr. Aparna Watve is a
scientist with Biome Conservation Foundation and teaches at the Tata Institute
of Social Sciences, Tuljapur Campus. She has been working on the rock
outcrops habitats in India and on the conservation of rocky plateaus in
Maharashtra.
Author Contribution: MD and AW did field work and wrote the manuscript.
Acknowledgements: We are thankful to the Director Agharkar
Research Institute, Pune for facilities and encouragement. We are also thankful to the authorities
of BSI and GU for granting us permission to check herbarium specimens. We thank Dr. Karthick
Balasubramanian and Dr. Sanjay Molur
for their critical suggestions on the manuscript and Dr. Stefan Porembski, Rostock University, Germany for fruitful
discussions.
Abstract: Vertical rocky cliffs, which consist of
various types of rock, are widespread all over the world. IndiaÕs northern Western Ghats
consisting of basaltic rocks form probably the largest cliff ecosystem
globally, however, almost no studies are available concerning their floristic
richness. In an attempt to understand the vascular plant assemblage of
this habitat, cliffs of the northern Western Ghats were surveyed for their
microhabitats, species diversity, distribution of endemics, occurrence of particular adaptive traits and potential threats. A total of 102 species of vascular
plants were documented from the cliff habitats of which 55 are endemic.
Flowering of the species on cliffs is triggered by the advent of the south-west monsoon and peak flowering is seen between August
and October. Of the total species,
27 grow exclusively on cliffs. Owing to habitat specificity, cliffs show a
greater number of narrow endemic and threatened species when compared with
other habitats like deciduous, evergreen and semi-evergreen forests, which are
widespread in the northern Western Ghats.
Unfortunately, this habitat faces threats in the form of landslides,
periodic burning and habitat loss due to road-widening.
Keywords: Cliff ecology, endemic species, vertical
cliffs, Western Ghats.
INTRODUCTION
The Western Ghats form a mountain
range that runs parallel to the western coast of India from 8.3188890N
to 21.273330N for more than 1,600km. Together with Sri Lanka it is one of the
34 biodiversity hotspots designated based on high
species endemism and also high degree of threat due to habitat loss (Myers et
al. 2000). The region has diverse habitats
ranging from dense tropical forests to sholas, swamps and rocky outcrops
supporting endemic flora and fauna.
The entire range is an important watershed area with many hill streams
and river valleys formed by deep weathering. The weathering has given rise to hills
with steep slopes, tall cliffs and flat or conical mountain
tops (Images 1 & 2).
The Western Ghats are of igneous
origin and geomorphologically the range is actually
the western escarpment of the Deccan Plateau formed by volcanic eruption between 60 and 68 million
years ago.
The Western Ghats go down steeply to the coastal plains on the western
side, but towards the east, they merge gently through a series of hills or
spurs with the Deccan
Plateau (Gunnell & Radhakrishna 2001).
Based on the parent rock, the
Western Ghats can be separated into two sections. The south of the river Kali in Karnataka
(15⁰N), is the region of Precambrian archean crystalline rocks. The hills have rounded tops and
they rise to 2,000m or more. This section, known as the southern Western Ghats
is rich in arboreal diversity sheltered by dense evergreen forests. North of the Kali River is the Deccan
trap country having relatively fragile rocks with hills not rising beyond 1,650m
and having flat hill tops showing outcroppings of laterite and basalt (Gunnell
& Radhakrishna 2001). Pascal (1988)
describes this section as the northern Western Ghats (henceforth referred to as
NWG), which has a high annual rainfall (3,000–4,000 mm) but a longer dry
period (almost 8 months) as compared to the southern and central Western Ghats
(rainfall above 5,000mm and almost 4 dry months). Strong seasonality together with typical
geological and geomorphological features of this region have
influenced the plant and animal ecology with regards to diversity of
life-forms. Monsoon herbs are
abundant and show higher endemism as compared to the woody endemics. The NWG comprise a large number of
habitat types including forests, grasslands, and rocky outcrops. In addition to
these, cliffs are also a very prominent habitat in the NWG and are seen
throughout the escarpment and on the major eastern and western spurs of the NWG
(Fig. 1).
Across the world, cliffs are
considered as distinct habitats and studied for their biodiversity,
environment, social, cultural and anthropological aspects. But little attention has been paid to
the cliffs of the Western Ghats and they have not been studied in detail. The present paper addresses this gap in
knowledge and attempts to give an overview of existing studies, floristic
aspects and the ecological features of cliff vegetation.
Cliffs have attracted the attention
of biologists, geologists and geomorphologists
throughout the world. IUCNÕs (2014)
habitat classification of the world recognizes inland cliffs as part of the
general category of Òrocky areasÓ which are generally defined as high, steep or
overhanging face of rock. Though
they are very distinct land forms, their spatial
extension is difficult to quantify on geographical maps because of vertical
surfaces. Larson et al. (2000)
state that cliffs are a type of rock outcrop, having three essential elements:
a level or sloping platform or plateau at the top; a pediment consisting of
base-rock at the bottom; and a vertical or near-vertical part, called the cliff
face or free-face in between.
Cliffs usually do not form smooth walls but show crevices, caves and
ledges. Talus or scree is the accumulated matter at the bottom consisting of
loose rock fragments derived from the weathering of cliff. A toe is the point where the talus slope meets the pediment. Ledges are the section of cliff faces that are more or less horizontal and may have
undercuts forming overhangs (Larson et al. 2000). Figure 2 shows a representative diagram
of cliffs in NWG.
The degree of slope for defining the
cliffs has been debatable, but is generally taken as more than 45¡. Distinctness of abiotic conditions from
other habitats is a characteristic of cliffs; however, similar to other rock outcrops, the
microclimate of the cliffs is more extreme in terms of moisture, humidity,
radiation and soil nutrient availability as compared to the surrounding
landscape. According to Larson et
al. (2000), vertical exposed cliffs are very dry, hot, have little or no humus
and support a very limited group of species adapted to a harsh
environment. The vertical
nature of cliffs, however, also leads to vegetation being strongly influenced
by wind and difficulty in formation and retention of soil. Coates & Kirkpatrick (1992) describe
cliffs as extreme environments where plant growth is limited by the combined
effects of moisture availability, light, and gravity. Light may not be a limiting factor in
the case of tropical regions such as the NWG, but availability of moisture, in
the cliff environments certainly varies drastically with seasonal changes. In the wet period (June–October),
most cliffs in the NWG have waterfalls and hill streams that support the lush
growth of seasonal chasmophytes.
As seen from Fig. 2, cliffs include
a variety of microhabitats and hence can have a diversity of plant life forms.
Perennial shrubs and tree species are well established wherever humus or soil
is present. The ephemeral
vegetation seen during and post monsoon, however, is abundant on the cliff
face, ledges and crevices. The
habitat is not easily accessible, but secondary vertical cliffs faces seen
along roads in mountain passes, known as ÒghatsÓ in
vernacular (Marathi) also support a majority of typical elements of cliff
flora. Many floristic exploratory works on various district floras of the
Indian state of Maharashtra have studied vegetation of the ghats. These studies mention ghats as a habitat or location of certain species but do
not give detailed information regarding microhabitat preference or adaptive
features of ghat flora. Also none of them discussed the presence
of specific features generally reported as life strategies for cliff species or
mentioned the general floristic composition. A detailed compilation of ghat flora from the entire Western Ghats is a much-needed
one.
Ecological studies of cliff habitats
in the NWG are also scarce. Bharucha & Ansari
(1963) published plant associations on slopes and screes in the NWG, and
included specific communities seen on steep slopes. Chasmophytic grasses of southern Western
Ghats were reported by Thomas et al. (2012). Work on lithophytic grasses of Maharashtra was carried out by Gosavi (2010), which included certain cliff grasses (Image
5). These were only sporadic
efforts and any exclusive review of cliff flora or vegetation ecology or
autecological accounts of endemic species of this
special habitat have not been published till now. Similar is the situation in the rest of
India as well, where floristic literature takes cognizance of cliff as a
habitat but ecological studies of cliffs have not been undertaken. Lack of baseline information on the
floral composition and detailed studies on the diversity patterns on this
habitat and effects of degradation are hampering the conservation efforts in
the Western Ghats.
Cliffs are well studied in other
parts of the world. Several
researchers have contributed to our knowledge of cliff vegetation (Escudero 1996; Cooper 1997; Dimitrov
& Vutov 2015; Bogges et
al. 2017). Studies by Davis (1951), Wilson & Cullen (1986), Lavergne et al.
(2004) are focused exclusively on cliffs, and try to bring out patterns of
endemism in flora, fauna, niche requirements, habitat preferences and adaptive
features. Impacts of human activities such as trekking and mountaineering on
cliffs have also been studied by Nuzzo (1996). Most notable
among cliff research is the review by Larson et al. (2000), which documents
biological, environmental as well as social and cultural aspects of cliff
ecology. The review indicates that
cliffs harbor a multitude of rare, endemic and endangered plant species and
contribute substantially to regional biodiversity.
The scope of this paper, as a
preliminary report is mainly to compile a list of species that primarily use
cliffs as habitat in the NWG. It
also discusses the microhabitats and particular plant adaptive traits,
endemism, conservation significance and future research needs.
MATERIALS AND
METHODS
Study area
The
study was carried out in the NWG between 15¡ and 21¡N latitudes, one-third of
the total length of the Western Ghats. To
understand the distribution of species in NWG, the region was divided into
three parts: northern, (between 19¡ and 21¡ N), central (between 17¡ and 19¡ N), and southern (between 15¡ and 17¡ N) parts of the northern Western Ghats.
Data collection and analysis
Primary information for this paper
has been collected during field studies between 2008 and 2016 in various parts
of the NWG. During field work observations related to species distribution,
details of microhabitats, phenology of the species and particular plant
adaptive traits were made. Based on
these observations a checklist of vascular plants growing on primary as well as
secondary cliffs was prepared (Table 1).
Primary cliffs are the natural cliffs seen in the Western Ghats while
secondary ones are the man-made cliffs during construction of roads in the ghat sections.
Available literature on floristic studies of the NWG especially district
floras for ghats like Trimbakeshwar
and Kasara (Billore 1972; Lakshminarasimhan & Sharma 1991); Malshej
(Billore 1972); Bor (Santapau 1953); Tamhini & Varandha (Kothari & Moorthy
1993); Ambenali & Kumbharli
(Almeida 1983–1986; Deshpande et al.
1993–95); Amba, Bhuibavda,
Gaganbavda and Phonda (Kulkarni 1988; Yadav & Sardesai 2002); Amboli and Tilari (Kulkarni 1988; Almeida
1990); Sattari (Rao
1985–1986) and Anmode (Rao
1985–1986; Datar & Lakshminarasimhan
2013a&b) was consulted.
Additional ecological information was collected from the specimens and
field notes in the herbaria of Botanical Survey of India, Western Regional
Center (BSI), Agharkar Research Institute Herbarium
(AHMA) and Goa University herbarium (GU).
The microhabitats of cliff plants were categorized into six major
microhabitat groups (Table 1). The
species were categorized as generalist (GN) and restricted (RI). Their specific adaptations for survival
in cliffs were also recorded. In
the checklist all the names are as per the Plant List (2013).
RESULTS
Our studies yielded a total of 102
species of vascular plants belonging to 35 families and 69 genera for the cliff
flora of the main range of the NWG which pass through Sindhudurg,
Ratnagiri, Kolhapur, Sangli,
Satara, Pune, Nashik, Ahmednagar, Palghar and Thane
districts of Maharashtra state and north and south Goa districts of Goa
State. Of the total species 91 are
angiosperms and 11 are pteridophytes. Although pteridophytes
are less in the number of species, they can be seen as dominant members with
respect to percentage cover on some cliffs. In case of some species there was not
enough or accurate ecological information available from earlier floristic
works to assign them conclusively to a life form category. We have categorized them based upon
field observations and habit, however further research
on these aspects is necessary. In
the list, therophytes are represented by 54 species
followed by 27 geophytes, 12 phanerophytes and nine hemicryptophytes (Fig. 3) based on RaunkiaerÕs
classification (Cain 1950) of life forms.
This is consistent with the seasonal climate of the region, which is
more favorable for the growth of therophytes and
geophytes.
As far
as distribution of cliff species is concerned, 61 species are spread throughout
the NWG while five are exclusively in the northern part of NWG, 13 in the
central part of NWG and 16 in the southern part of NWG. Five species are distributed in the
southern and central parts of NWG while two species in the northern and central
part of NWG. Five species viz. Kalanchoe bhidei
Cooke, Kalanchoe olivacea
Dalzell, Senecio edgeworthii
Hook.f., Dyerophytum indicum
(Gibs. ex Wt.) O. Ktze. And
Chlorophytum bharuchae
Ansari et al. were found to grow exclusively on cliffs of ghats
connecting north and south which are comparatively drier than the east-west ghats (Fig. 1).
These hill passes are located at about 40km towards east of the main
crest of the Western Ghats.
DISCUSSION
Cliffs are known to support
ecologically specialized taxa.
Extreme climatic conditions have made species growing on cliffs flower
for a limited duration. From the
phenology of the species it can be seen that flowering is triggered by the
advent of the monsoon. The maximum
flowering is seen between August and December when the monsoon is settled. During the monsoon mostly therophytes and geophytes flower, while post monsoon
flowering is observed in phanerophytes (Fig. 4).
Microhabitats on cliffs
All 102 plant
species growing on cliffs grow in 6 major microhabitats. All these microhabitats are present on
most of the cliffs, but their relative area on each cliff in various regions
may differ. A brief description of
the prominent microhabitats is given below:
Edge of the plateau tops: plateau top edges are often marked by deep crevices and fissures in
the rock due to natural erosion processes. Many small or large waterfalls can be
seen along the plateau edges during monsoon.
Most of the species found in this
microhabitat have also been noted on plateau tops and boulders as well but they
are abundant on plateau edges.
Although ecological research on their habitat preference has not been
carried out, these observations have been made during fieldwork and are
supported by literature data. In
most areas, plateau tops are heavily grazed and trampled by people as well as
livestock. Some monsoon agriculture
is also practiced and very often they are subject to burning during the summer
for increasing the grass flush. It
is possible that one or more of these processes have heavily impacted
populations of these species on the plateau tops and they are thus restricted
or abundant only along the edge of the plateaus.
Hill slopes: Slope varies between
30–60 degrees along the hill ranges of NWG. They are mostly covered with soil of
varying depth formed by weathering.
The vegetation cover may vary from scrub grassland to forest depending
on the local land use. Very often
hill slopes are burnt as part of developing secondary grasslands for
cultivation where they are easily accessible to people.
Seasonally moist vertical rock face
(MVR): exposed vertical rock with almost 90 degree
inclination and devoid of soil is a classic feature of most cliffs. Geomorphologically
it is termed as free face or cliff face (Image 7). In the rainy season waterfalls are
present and in general water seepage is common. Here a biofilm made up by cyanobacteria,
diatoms and lichens occurs. In the
monsoon they are moist due to continuous trickling of water even during the gap
in rain owing to the availability of water from the plateau. If a waterfall is large, the cliff face
has a spray zone near waterfalls, which is also moist. Moist crevices on vertical faces can be
treated under this microhabitat.
Narrow cracks are often seen on vertical rock faces. These crevices have some amount of humus
accumulated over the years. Water
trickles continuously during the wet period (Image 3).
Ledges: They are sections of cliff
face that are more or less horizontal and may be undercut, thus forming
overhangs (Larson et al. 2000).
These are step like formations due to weathering of cliff faces and look
like small terraces with accumulation of soil and humus. These ledges can support phanerophytes and geophytes. Caves and overhangs are often seen and
can be of varying depth. Vascular
plants, however, hardly ever occur in caves.
Dry vertical rock (DVR): exposed
vertical rock with almost 90 degree inclination and
devoid of soil. DVR can be distinguished
from MVR in having no trickling of water on the rocks. These rock faces are moist during
the rains, but in the absence of trickling water these rocks dry up very
quickly as compared to the MVR.
As seen from the description, MVR and DVR are both moist in heavy
rainfall period, but the moisture lasts longer on MVR due to waterfalls or
streams thus influencing the vegetation.
Scree: This is a well-defined
habitat consisting of accumulation of large rock fragments derived from
weathering of the cliff face (Larson et al. 2000). Soil of varying depth can be seen and in
the absence of intensive biotic pressures, scree has dense shrub or low tree
growth.
Ecological amplitude of species
For the sake of understanding we
have classified plants into generalist (GN) and restricted (RI) here. Recently Kypriotakis
& Tzanoudakis (2001) have categorized plant taxa
occurring on cliffs into three categories (a) obligate chasmophytes,
which exclusively occur on cliffs and in crevices; (b) plants that are mainly chasmophytes, occurring mostly on vertical cliffs, but
occur in other habitats with lower frequency; and (c) plants that are partially
or occasionally occurring on cliffs and mostly occur in other habitats.
The term generalist (GN) is used as
a descriptor in Table 1 indicating that these species were also seen in
habitats other than cliffs, e. g. Delphinium malabaricum
is also seen on high altitude plateaus while Begonia crenata
is seen on boulders in exposed or shaded areas and it grows as an epiphyte in
dense forest as well. The same is the case with other species marked GN in
Table 1. But our observations
suggest that these species do have a greater abundance on cliffs as compared to
the rest of the habitats in which they occur. The reasons of this could be many
ranging from environmental parameters to biotic pressures.
Many species, which are facultative
or opportunistic cliff dwellers, were excluded from this list, for the reason
that they do not show more abundance on the cliffs as compared to the other
habitats, e.g., Senecio bombayensis
grows on cliffs but is much more abundant on plateaus.
The term RI (Restricted) is used in
Table 1 instead of specialist. It
indicates that these species are observed or reported so far only from the
cluster of microhabitats identified under the broad category of cliff. Some of them such as Utricularia
striatula (Image 9) or Rhynchoglossum
notonianum can be called specialists considering
the fact that their pattern of growth and root system appeared to be adapted to
vertical cliffs.
About 62 species are noted as
generalists while 40 are restricted to cliffs. More detailed ecological and autecological studies are needed for a more reliable
categorization into generalists and specialists. In the case of species such as Silentvalleya chandwadensis,
which are known from a limited number of specimens it is not possible to
ascertain whether they are specialists or not.
Adaptations
Some of the species recorded in
cliffs in the NWG showed characteristic adaptations to grow under harsh
environmental conditions. They are
explained below:
Poikilohydry: Poikilohydry is a highly specialized
adaptation shown by plants growing under conditions of periodic water
stress. These species are more
commonly known as desiccation tolerant or resurrection plants owing to the
unique adaptation for sustaining during the dry period. At the beginning of a dry spell the
tissues of these plants lose water and become dry and shriveled. But if a small amount of water becomes
available from rainfall or streams, these plants absorb water and resume normal
growth even during the dry period.
Eight poikilohydric species were listed on
cliffs, viz. Tripogon lisboae,
T. capillatus, T. filiformis
(Image 4), Didyimocarpus pygmaea,
Microchirita hamosa, Actinopteris sp., Cheilanthes
sp., etc. Poikilohydry has not been studied for
Indian plants with the exception of a paper by Gaff & Bole (1986). It is quite possible that more such
species can be found on cliffs and other outcrop habitats in future.
Carnivory: Carnivory is an adaptation by plants
to overcome the scarcity of nutrients like nitrogen, phosphorus and potassium
(Ellison 2006). Carnivorous plants
are abundant and diverse in the ephemeral flush vegetation on rock outcrops (Porembski & Watve 2005) such
as ferricretes, mesas and inselbergs
in India. But only two species of
bladderworts were recorded on cliff microhabitats in this study. Utricularia
striatula is a specialist that often covers large
MVR, and many individuals are seen on wide, open faces with trickling
water. U. graminaefolia is another generalist carnivorous
species seen on cliffs.
Succulence: Frerea
indica and Sarcostemma
intermedium (Apocynaceae)
are the only two succulent species growing on cliffs. Frerea
indica grows on hills of the main NWG, while Sarcostemma intermedium
grows on offshoots of Ghats, in drier areas as compared to the former. Frerea
indica was considered as one of the most
threatened species of the region, but it is now reported from six localities on
plateau edges (Misra & Singh 2001). Frerea indica is
also found to show C4 pathway of photosynthesis (Lange & Zuber 1977), which is one of the adaptations for surviving
in harsh environment on cliffs.
Geophytes: Presence of tubers, bulbs
and rhizomes is a classic adaptation to seasonal climate, where growing period
is limited to only a certain part of the year. This is by far the most common
adaptation shown by cliff species.
A total of 2 bulbous, 22 tuberous and 2 rhizomatous species are included
in table 1. The reproductive phase
of these plants is over after the monsoon and the plant remains in the form of
underground organs until the next monsoon.
This group includes species like Ceropegia
huberi (Image 8), C. mahabalei,
and C. santapaui which generally
grow on moist vertical rocks or hill slopes with some amount of soil
accumulation.
In addition to these well documented adaptations, certain species show perennating organs in the form of dry cottony balls
produced next to the soil surface at the base of the stem. This understudied adaptation is observed
in species belonging to genera like Blumea and
Senecio.
These species are treated here under hemicryptophytes.
As seen from above, the adaptations recorded so far seem to be more for the seasonal
dryness and nutrient scarcity experienced by the flora in this habitat. More research is necessary to understand
if adaptations related to wind velocity, radiation or any other factors are
also present.
Endemism and rarity
Numerous endemic (Image 6) species
are found on cliffs owing to their geographical isolation and selective
pressure towards evolution of adaptive features (Larson et al. 2000). Cliffs of the NWG also support many
endemic species. The list (Table 1)
includes 55 species reported as endemic in previous studies of which 35 are endemic to the NWG (Singh & Karthikeyan
2000; Datar & Lakshminarasimhan 2013a). The number of endemics shows a fairly
large percentage (50%+) of the cliff flora. Many of these are restricted (RI) as per
our observations and 19 species are reported as Critically Endangered (CR), Endangered(EN) and Vulnerable (VU) as per the Botanical
Survey of India (Mishra & Singh 2001) and IUCN indicating high
conservation significance of cliff habitats.
The species growing on cliffs also
show microhabitat preference, for example species like Hubbardia
diandra, Eria reticosa, Ceropegia
huberi, C. santapauii
are restricted to moist vertical rocks while species like Begonia concanensis, B. phrixophylla
prefer to grow in moist areas on edges of plateau tops. Species like Frerea
indica always prefer dry vertical rocks while Trachyspermum roxburghianum
and Ceropegia noorjahanae
grow on hill slopes where some amount of soil is accumulated.
Cliffs shelter six narrow endemic
species viz. Hubbardia diandra
(Image 10), Silentvalleya chandwadensis,
Ceropegia mahabalei, C. santapaui, C. noorjahanae and
Begonia concanensis. It was found that narrow endemic species
showed a clear pattern of ecological differentiation from their widespread
congeners as they occurred in steeper habitats, higher bedrock and sparser
vegetation. This is consistent with
observations of Baskin & Baskin (1988) that rocky areas have a higher
number of narrow endemic species.
Endemism and the presence of
threatened plants on cliffs is also reported by Shmida (1984) and Aronne et al.
(2014). They have documented 7%
endemic plants from coastal vertical cliffs of the national park of Cilento. But compared to this region cliffs of the NWG have
a much higher percentage of endemic plants emphasizing again its high
conservation value.
Threats to the habitat and vegetation
During this first study, the focus
was on floristics, however, notes were recorded on
pressures and threats to the habitat.
As compared to the plateau tops, valleys, forests and other more
accessible habitats near human habitations, cliffs are less
intensively used by humans and livestock. Hill slopes are used for grazing by
sheep and cattle, but the vertical cliffs faces (MVR, DVR) and edges, ledges or
overhangs are rarely accessed by people, making these safe
sites for some species. A
major threat for cliff vegetation appears to be from manmade fires, which are
lit for developing scrub grasslands, or hill slope cultivation. These are mostly seen
during hot months (January to April) and often fire escapes and burns
many habitats. Widening of roads
and railway track expansion is another threat to established vegetation on the
cliffs. This can be seen in Anmode
Ghat (Datar & Lakshminarasimhan 2013a). The vegetation of cliffs is heavily
dependent on accumulated humus and intense burning can affect it severely. Landslides are also a threat to
vegetation, but in the absence of any specific data on frequency or intensity
of landslides, their actual effect at species level cannot be predicted. This is more evidenced in secondary
cliffs. Nuzzo (1996), Camp & Knight (1998) and
McMillan & Larson (2002) have addressed effect of rock climbing on cliff
vegetation and their effect on endemic flora. So far this does not appear to be a
threat to cliff flora of this region as rock climbing or mountaineering is not
common. It may be a local factor of
importance in case of some localities such as forts and peaks such as Raigad, Sinhagad, Kalsubai and others popular for these sports.
CONCLUSION
The cliff ecosystem of the Western
Ghats is among the largest worldwide, but botanically it is still rather
neglected. This review of species, vegetation and microhabitats of cliffs in
the NWG is a preliminary documentation of existing information and field
studies. As seen above, this cliff
ecosystem has many environmental peculiarities, which are reflected in the
species adaptations and life forms. Particularly outstanding is the fact that
desiccation tolerant grasses (Tripogon spp.)
are dominant colonizers of steep vertical cliffs throughout the NWG. The cliffs of this mountain range seem
to form the largest rocky surface area on Earth, which is colonized by
resurrection plants. The high
number of endemic and threatened species, special ecological features, and
specific threats due to biotic activities indicates need for conservation and
protection measures. The habitat is
also important from the watershed point of view and more research is needed on
floristic, ecological and ecosystem processes and services to take the
necessary steps for conservation.
It is hoped that this paper will provide baseline information for future
detailed studies on this unique habitat in the northern Western Ghats and other
parts of India as well.
Table 1. Vascular
plant species growing on cliffs in the northern Western Ghats.
|
Name of
the species |
Family |
Life form |
Specificity |
Adaptation |
Microhabitats
|
Distribution
in NWG |
Endemicity -range |
Voucher
specimen* |
1 |
Delphinium
malabaricum (Huth)
Munz |
Ranunculaceae |
TH |
GN |
|
HS |
Northern
and central parts of NWG |
NWG |
15929 |
2 |
Thalictrum dalzellii Hook. |
Ranunculaceae |
TH |
GN |
|
DVR, L |
Throughout
NWG |
NWG |
78 |
3 |
Reinwardtia indica Dumort. |
Linaceae |
TH |
GN |
|
DVR, L |
Throughout
NWG |
|
2159 |
4 |
Impatiens acaulis Arn. |
Balsaminaceae |
GE |
RI |
UPO |
MVR |
Throughout
NWG |
|
2289 |
5 |
Rhamnus virgata var. hirsuta (Wight & Arn.)
Y.L. Chen & P.K. Chou |
Rhamnaceae |
PH |
GN |
|
HS |
Throughout
NWG |
PI |
25386 |
6 |
Kalanchoe bhidei Cooke |
Crassulaceae |
TH |
RI |
|
EP |
Central
part of NWG |
NWG |
|
7 |
Kalanchoe olivacea Dalzell |
Crassulaceae |
TH |
RI |
|
EP |
Central
part of NWG |
NWG |
899 |
8 |
Sonerila scapigera Dalzell |
Melastomataceae |
GE |
RI |
UPO |
MVR |
Throughout
NWG |
NWG |
20880 |
9 |
Rotala floribunda (Wt.) Arn. |
Lythraceae |
TH |
RI |
|
MVR |
Central
part of NWG |
NWG |
1981 |
10 |
Begonia concanensis DC. |
Begoniaceae |
GE |
RI |
UPO |
EP |
Throughout
NWG |
NWG |
8149 |
11 |
Begonia crenata Dryand |
Begoniaceae |
GE |
GN |
UPO |
MVR |
Throughout
NWG |
|
8155 |
12 |
Begonia phrixophylla Blatt. & McCann |
Begoniaceae |
GE |
RI |
UPO |
EP |
Central
part of NWG |
NWG |
|
13 |
Begonia trichocarpa Dalzell |
Begoniaceae |
GE |
RI |
UPO |
MVR |
Central
and Southern parts of NWG |
WG |
21028 |
14 |
Heracleum grande (Dalzell & A. Gibson) Mukhop. |
Apiaceae |
GE |
GN |
UPO |
EP |
Throughout
NWG |
WG |
1023 |
15 |
Pinda concanensis (Dalzell) P.K. Mukh.
& Constance |
Apiaceae |
GE |
GN |
UPO |
EP |
Throughout
NWG |
NWG |
8174 |
16 |
Scandix stellata Banks
& Soland |
Apiaceae |
TH |
GN |
|
HS |
Central
part of NWG |
|
|
17 |
Trachyspermum roxburghianum (DC.) Craib. |
Apiaceae |
GE |
RI |
UPO |
HS |
Throughout
NWG |
PI |
8295 |
18 |
Argostemma verticillatum Wall. |
Rubiaceae |
GE |
RI |
UPO |
MVR |
Southern
part of NWG |
|
186753
(BSI) |
19 |
Argostemma courtallense Arn. |
Rubiaceae |
GE |
RI |
UPO |
MVR |
Southern
part of NWG |
|
186777
(BSI) |
20 |
Hymenodictyon obovatum Wall. |
Rubiaceae |
PH |
GN |
|
EP |
Throughout
NWG |
India |
|
21 |
Hymenodictyon orixensis (Roxb.) Mabb. |
Rubiaceae |
PH |
GN |
|
EP |
Throughout
NWG |
|
15522 |
22 |
Neanotis lancifolia (Hook.f.) W. H. Lewis |
Rubiaceae |
TH |
GN |
|
MVR |
Throughout
NWG |
WG |
5443 |
23 |
Neanotis montholonii (Hook.f.) W. H. Lewis |
Rubiaceae |
TH |
GN |
|
MVR |
Throughout
NWG |
PI |
6093 |
24 |
Spermadictyon suaveolens Roxb. |
Rubiaceae |
PH |
GN |
|
HS |
Throughout
NWG |
|
26272 |
25 |
Artemisia
japonica Thunb. |
Asteraceae |
PH |
GN |
|
HS |
Central
part of NWG |
|
7468 |
26 |
Artemisia nilagirica (C.B.Clarke) Pamp. |
Asteraceae |
PH |
GN |
|
HS |
Throughout
NWG |
|
|
27 |
Blumea membranacea DC. |
Asteraceae |
TH |
GN |
|
HS |
Throughout
NWG |
|
7533 |
28 |
Kleinia grandiflora (wallich ex DC.) N.Rani |
Asteraceae |
TH |
GN |
|
EP |
Throughout
NWG |
|
1177 |
29 |
Senecio edgeworthii Hook.f. |
Asteraceae |
HE |
RI |
DCB |
DVR, HS |
Throughout
NWG |
PI |
7895 |
30 |
Gynura bicolor (Roxb. ex Willd.) DC. |
Asteraceae |
TH |
GN |
|
S |
Throughout
NWG |
|
7818 |
31 |
Campanula alphonsii Wall. ex A.DC. |
Campanulaceae |
GE |
RI |
UPO |
DVR |
Central
part of NWG |
NWG |
8823 |
32 |
Dyerophytum indicum (Gibbs ex Wight) Kuntze |
Plumbaginaceae |
PH |
RI |
|
DVR |
Northern
part of NWG |
|
8894 |
33 |
Ceropegia huberi Ansari |
Apocynaceae |
GE |
RI |
UPO |
MVR |
Southern
and Central part of NWG |
NWG |
26636 |
34 |
Ceropegia mahabalei Hemadri & Ansari |
Apocynaceae |
GE |
RI |
UPO |
HS |
Northern
part of NWG |
NWG |
17548 |
35 |
Ceropegia noorjahanae Ansari |
Apocynaceae |
GE |
RI |
UPO |
HS |
Central
part of NWG |
NWG |
175465
(BSI) |
36 |
Ceropegia sahyadrica Ansari
& Kulkarni |
Apocynaceae |
GE |
RI |
UPO |
EP,HS |
Throughout
NWG |
NWG |
17713 |
37 |
Ceropegia santapaui Wadhwa & Ansari |
Apocynaceae |
GE |
RI |
UPO |
MVR |
Southern
part of NWG |
NWG |
26091 |
38 |
Frerea indica Dalzell |
Apocynaceae |
HE |
RI |
SUC |
DVR |
Northern
and central parts of NWG |
NWG |
17540 |
39 |
Sarcostemma intermedium Decne. |
Apocynaceae |
HE |
GN |
SUC |
DVR |
Central
part of NWG |
NWG |
17824 |
40 |
Canscora concanensis C.B.Clarke |
Gentianaceae |
TH |
GN |
|
EP |
Throughout
NWG |
NWG |
20139 |
41 |
Canscora diffusa (Vahl) R.Br. ex Roem. & Schult. |
Gentianaceae |
TH |
GN |
|
EP |
Throughout
NWG |
|
14145 |
42 |
Kickxia incana (Wall.)
Pennell |
Scrophulariaceae |
TH |
RI |
|
HS |
Southern
part of NWG |
|
11886 |
43 |
Kickxia ramosissima (Wall.) Janchen |
Scrophulariaceae |
TH |
GN |
|
DVR |
Throughout
NWG |
|
11855 |
44 |
Utricularia striatula Sm. |
Lentibulariaceae |
TH |
RI |
CAR |
MVR |
Throughout
NWG |
|
26941 |
45 |
Utricularia graminifolia Vahl |
Lentibulariaceae |
TH |
GN |
CAR |
MVR |
Southern
part of NWG |
|
12903 |
46 |
Microchirita hamosa (R.Br.)
Yin Z.Wang |
Gesneriaceae |
TH |
RI |
POIK |
MVR |
Southern
part of NWG |
|
|
47 |
Didymocarpus pygmaeus C.B.Clarke |
Gesneriaceae |
TH |
RI |
POIK |
DVR |
Central
part of NWG |
|
12936 |
48 |
Epithema carnosum Benth. |
Gesneriaceae |
TH |
RI |
|
MVR |
Southern
part of NWG |
|
|
49 |
Rhynchoglossum notonianum (Wall.) Burtt. |
Gesneriaceae |
TH |
RI |
|
MVR |
Southern
part of NWG |
|
12941 |
50 |
Rhynchoglossum obliquum Blume |
Gesneriaceae |
TH |
RI |
|
MVR |
Central
part of NWG |
|
12947 |
51 |
Strobilanthes callosa Nees |
Acanthaceae |
PH |
GN |
|
HS |
Throughout
NWG |
NWG |
13083 |
52 |
Eranthemum capense L. var. concanense (T. Anders.) Santapau |
Acanthaceae |
TH |
GN |
|
HS |
Southern
part of NWG |
WG |
186720
(BSI) |
53 |
Haplanthodes neilgherryensis
( Wight) Majumdar |
Acanthaceae |
TH |
GN |
|
HS |
Throughout
NWG |
NWG |
13078 |
54 |
Haplanthodes plumosa (T.
Anders.) Panigr. & G. C. Das |
Acanthaceae |
TH |
GN |
|
EP |
Throughout
NWG |
WG |
|
55 |
Haplanthodes verticillatus
(Roxb.) R.B.Majumdar |
Acanthaceae |
TH |
GN |
|
HS |
Throughout
NWG |
WG |
13388 |
56 |
Justicia wynaadensis B.Heyne |
Acanthaceae |
TH |
GN |
|
HS |
Southern
part of NWG |
NWG |
187501
(BSI) |
57 |
Strobilanthes scrobiculatus
Dalzell ex C.B.Clarke |
Acanthaceae |
PH |
RI |
|
HS |
Southern
part of NWG |
NWG |
1786 |
58 |
Anisochilus carnosus (L.f.) Wall. |
Lamiaceae |
TH |
GN |
|
S |
Throughout
NWG |
|
13559 |
59 |
Anisochilus adenanthus Dalzell
& A.Gibson |
Lamiaceae |
TH |
RI |
|
HS |
Southern
part of NWG |
WG |
13563 |
60 |
Leucas montana (Roth) Spreng. |
Lamiaceae |
PH |
GN |
|
HS |
Central
part of NWG |
|
14628 |
61 |
Lecanthus peduncularis (Wall. ex Royle) Wedd. |
Urticaceae |
TH |
GN |
|
MVR |
Throughout
NWG |
|
11109 |
62 |
Ficus arnottiana (Miq.) Miq. |
Moraceae |
PH |
GN |
|
EP |
Throughout
NWG |
|
11263 |
63 |
Eria reticosa Wt. |
Orchidaceae |
HE |
RI |
|
MVR |
Throughout
NWG |
India |
21009 |
64 |
Habenaria brachyphylla (Lindl.) Aitch. |
Orchidaceae |
GE |
GN |
UPO |
MVR |
throughout NWG |
NWG |
21092 |
65 |
Habenaria rariflora A. Rich. |
Orchidaceae |
GE |
GN |
UPO |
MVR |
Throughout
NWG |
WG |
6271 |
66 |
Crinum brachynema Herb. |
Amaryllidaceae |
GE |
RI |
UPO |
HS |
Throughout
NWG |
NWG |
6640 |
67 |
Crinum woodrowii Baker |
Amaryllidaceae |
GE |
GN |
UPO |
HS |
Throughout
NWG |
NWG |
17557 |
68 |
Chlorophytum arundinaceum Baker |
Asparagaceae |
GE |
GN |
UPO |
L |
Southern
part of NWG |
|
|
69 |
Chlorophytum bharuchae Ansari, Sundararagh. & Hemadri |
Asparagaceae |
GE |
GN |
UPO |
HS |
Central
and Southern parts of NWG |
NWG |
20490 |
70 |
Chlorophytum glaucum Dalzell |
Asparagaceae |
GE |
GN |
UPO |
EP |
Throughout
NWG |
NWG |
24500 |
71 |
Chlorophytum glaucoides Blatt. |
Asparagaceae |
GE |
GN |
UPO |
EP |
Northern
and central parts of NWG |
PI |
165260
(BSI) |
72 |
Chlorophytum nimmonii Dalzell |
Asparagaceae |
GE |
GN |
UPO |
L |
Southern
part of NWG |
|
25048 |
73 |
Phoenix loureiroi var. pedunculata
(Griff.) Govaerts . |
Arecaceae |
PH |
GN |
|
HS |
Northern
part of NWG |
PI |
12367 |
74 |
Ariopsis peltata Nimmo |
Araceae |
GE |
GN |
UPO |
MVR |
Throughout
NWG |
|
187924
(BSI) |
75 |
Eriophorum comosum (Wall.) Nees |
Cyperaceae |
TH |
RI |
|
DVR |
Northern
and central parts of NWG |
|
19985 |
76 |
Arthraxon jubatus Hack. |
Poaceae |
TH |
RI |
|
MVR |
Throughout
NWG |
WG |
13665 |
77 |
Arthraxon hispidus (Thunb.) Makino |
Poaceae |
TH |
RI |
|
MVR |
Throughout
NWG |
|
13657 |
78 |
Arthraxon meeboldii Stapf |
Poaceae |
TH |
RI |
|
MVR |
Throughout
NWG |
NWG |
13704 |
79 |
Garnotia arborum Stapf. ex T. Cooke |
Poaceae |
TH |
GN |
|
MVR |
Throughout
NWG |
NWG |
204 (GU) |
80 |
Hubbardia diandra Chandore , Gosavi & S.R.Yadav |
Poaceae |
TH |
RI |
|
MVR |
Southern
part of NWG |
NWG |
182304
(BSI) |
81 |
Isachne gracilis C.E. Hubb. |
Poaceae |
TH |
RI |
|
MVR |
Throughout
NWG |
NWG |
20284 |
82 |
Ischaemum raizadae Hemadri & Billore |
Poaceae |
TH |
GN |
|
MVR |
Throughout
NWG |
NWG |
25817 |
83 |
Ischaemum diplopogon Hook. f. |
Poaceae |
TH |
GN |
|
MVR |
Throughout
NWG |
NWG |
15614 |
84 |
Lakshmia venusta (Thwaites) Veldkamp |
Poaceae |
TH |
RI |
|
MVR |
Southern
part of NWG |
NWG |
|
85 |
Silentvalleya chandwadensis
Gosavi, B.R. Pawar & S.R. Yadav |
Poaceae |
TH |
RI |
|
DVR |
Northern
part of NWG |
NWG |
|
86 |
Pseudodichanthium serrafalcoides
(Cooke & Stapf) Bor |
Poaceae |
TH |
GN |
|
EP |
Throughout
NWG |
India |
17757 |
87 |
Tripogon bromoides Roth |
Poaceae |
HE |
GN |
POIK |
MVR |
Throughout
NWG |
|
21266 |
88 |
Tripogon capillatus Jaub. & Spach |
Poaceae |
HE |
GN |
POIK |
MVR |
Throughout
NWG |
WG |
21501 |
89 |
Tripogon filiformis Nees ex Steud. |
Poaceae |
HE |
GN |
POIK |
MVR |
Central
part of NWG |
|
|
90 |
Tripogon lisboae Stapf |
Poaceae |
HE |
RI |
POIK |
MVR |
Throughout
NWG |
PI |
21030 |
91 |
Tripogon trifidus Munro ex Stapf |
Poaceae |
HE |
GN |
|
MVR |
Northern
part of NWG |
|
|
92 |
Selaginella tenera Spring |
Selaginellaceae |
TH |
GN |
POIK |
HS |
Throughout
NWG |
|
|
93 |
Adiantum capillus-veneris L. |
Pteridaceae |
TH |
GN |
|
HS |
Throughout
NWG |
|
|
94 |
Cheilosoria tenuifolia (Burm. f.) Trevis. |
Pteridaceae |
TH |
GN |
|
HS,EP |
Throughout
NWG |
|
|
95 |
Cheilanthes albomarginata C.B.
Clarke |
Pteridaceae |
TH |
GN |
POIK |
HS,EP |
Throughout
NWG |
|
|
96 |
Cyclosorus interruptus (Willd.) H. It™ |
Thelypteridaceae |
TH |
GN |
|
HS |
Throughout
NWG |
|
|
97 |
Thelypteris parasitica (L.)
Farwell |
Thelypteridaceae |
TH |
GN |
|
HS |
Throughout
NWG |
|
|
98 |
Ampelopteris prolifera (Retz.) Copel. |
Thelypteridaceae |
TH |
GN |
|
HS |
Throughout
NWG |
|
|
99 |
Macrothelypteris torresiana (Gaudich.) Ching |
Thelypteridaceae |
TH |
GN |
|
HS |
Throughout
NWG |
|
|
100 |
Athyrium hohenackerianum
(Kunze) T. Moore |
Athyriaceae |
TH |
GN |
|
HS |
Throughout
NWG |
|
|
101 |
Diplazium esculentum (Retz.)
Sw. |
Athyriaceae |
TH |
GN |
|
MVR |
Throughout
NWG |
|
|
102 |
Leptochilus decurrens Blume |
Polypodiaceae |
TH |
GN |
|
MVR |
Throughout
NWG |
|
|
Abbreviations: Adaptations: UPO - Underground Protecting or storage organ; POIK - Poikilohydrous; CAR - carnivorous plants; DCB - Dry cottony
balls; SUC - Succulent. Life forms: TH - Therophyte;
PH - Phanerophyte; GE-Geophyte; HE - Hemicryptophyte. Habitat specificity: GN - Generalist; RI- Restricted. Habitats: DVR-Dry vertical rocks; EP -
Edge of the plateau top; HS - Hill slopes; L - Ledges; MVR- Moist vertical
rocks; S - Scree. Endemism: NWG - northern Western Ghats; WG - Western Ghats;
PI - Peninsular India.
Acronyms and short name of herbaria to which voucher specimens are
referred: AHMA - Herbarium of Agharkar Research
Institute, Pune, India; GU - Goa University herbarium, Goa, India; BSI -
Botanical Survey of India, Western Circle Herbarium, Pune, India.
* All specimens without any acronym in bracket are referred to
AHMA.
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