Friday, 26 October 2012

Field trip in Canarias, La Palma island in October 2012

A trip to La Palma Island took place this month to work along the elevational gradient that is located in the eastern slope of the island. The team was composed by Pr. Dr. Juana María González Mancebo, Raquel Hernández Hernández and Julio Leal Pérez that is the collaborator of La Laguna Bryologists group.

Pix: La Palma's team during the field work of october 2012, from left to right, Raquel Hernández-Hernández, Julio Leal and Juana María González-Mancebo


The transect includes 24 plots from 40 to 2200 m a.s.l., among them 18 plots were made in this expedition.
Here it is a brief description and some pictures of the plots that were sampled.

40 m – Fajana de La Galga
Vegetation is mainly composed by coastal shrubs like Peripoloco laevigata, Euphorbia canariensis and Rumex lunaria. Bryophytes were more frequent in soil and rocks, although the cover was very reduced. The dominant species were Tortella nitida, Bryum spp. and Frullania ericoides.





Pix 2: Raquel and Julio working in Fajana de la Galga



200 m- Barranco del Cubo de La Galga
The dominant tree species at this elevation were Apollonias barbujana and Visnea mocanera, so thermophilous laurel forest trees. Canopy is quite closed, so we found a higher bryophyte cover and species like Homalia webbiana, Radula lindenbergiana, Eurhynchium meridionale.

Pix 3: Raquel and Juana María working at 400 m in the first forests along the elevational gradient

400 m- Cubo de La Galga

The canopy at this elevation was mainly dominated by Laurus novocanariensis and Persea indica. Some exotic herbaceous species were also present and unfortunately relatively abundant like Ageratina adenophora. Bryophytes were way more abundant in rocks (75%) than in other microhábitats.




600 m- Cubo de La Galga
Laurel forest dominated by Persea indica and Ocotea foetens. Bryophytes cover increases highly respect the previous elevational plots. The most common species were the Iberian-Macaronesian endemic Heteroscyphus denticulatus and a widespread species in the laurel forest, Isothecium myosuroides, mainly in rocks.

800m- Barranco de Los Tilos
Forest dominated by Persea indica and Laurus novocanariensis. Total canopy cover reaches 95%. Dominant bryophytes were: Rhynchostegium megapolitanum, Saccogyna viticulosa and Frullania tamarisci.

Pix 4: Plot in the Laurel forests in Barranco de Los Tilos

1000m- Pista del Mulato (Barranco de Los Tilos)
Laurel forest composed mainly by Laurus novocanariensis, but there were also presence of Persea indica, Morella faya and Ilex canariensis. Some of the species we found were Saccogyna viticulosa, Isothecium myosuroides and the Macaronesian endemic Leptodon longisetus.

1200m- Under the “Casa del Monte” (Barranco de Los Tilos)
Laurel forest in which Laurus novocanariensis is the dominant species together with some individuals of Erica arborea and Ilex canariensis and with a narrow closed canopy. Bryophytes cover on rocks raised 80%.

1400m- Casa del Monte (Barranco de Los Tilos)
Mixed pine forest dominated by Pinus canariensis, Morella faya and Erica arborea and Pinus canariensis. The total canopy cover is 80%. Bryophytes very scarce and only present on soil under the pine litter.

1800m- Topo Mosquito
This correspond with the highest plot with pine forest in our transect.  At this elevation the schrub Adenocarpus viscosus was quite abundant. Bryophytes relatively abundant (45%) on rocks, but absent on soils and very scarce as epiphytes (only Dicranoweissia cirrata and Orthotrichum sp. On rocks Grimmia trichophylla was the most common species.



Pix 5: The highest level for the pine forest in La Palma is around 2000 m a.s.l.

2000m- Fuente Vizcaína

Schrub-land vegetation dominated by Adenocarpus viscosus, with presence of other species like Erysimum scoparium and some graminae species. Bryophytes only present on rocks.



Pix 6: High montane vegetation in La Palma at 2000 m a.s.l.

Some additional work

In this island two additional transects are being studied at the same altitudinal level. Both are transects with a different degree of disturbance as part of the thesis of the PhD of Raquel Hernández-Hernández, in which we are trying to analyse the influence of disturbance along the elevation gradient on both, biodiversity and functional traits of bryophytes.  



Text and Photographs: Juana María González-Mancebo





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Monday, 15 October 2012

On the use of "elevation" and "altitude"

In a recent paper Vicar & Körner (2012) in  Oecologia (doi:10.1007/s00442-012-2416-7)  clarified the use of elevation, altitude and height that have been used with confusion in literature. Here, I report from their note the definition of these terms, which sometimes have been misused from translations between Romanic languages.

Elevation is the vertical distance between  a point on the land surface and a reference point, usually taken to be the mean sea level.
Altitude is the vertical distance between an object (e.g., a bird, aircraft, or parcel of air) and a reference point or stratum, where the object is not in direct contact with the reference point/stratum.
Height is the vertical distance between the top of an object and the land surface, where the object is in direct contact with the ground.

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Monday, 1 October 2012

Field trip in Azores, Terceira island: 25-28th september 2012

An expedition in Terceira island (Azores)  along an elevational gradient took place between the 25th and 28th of September 2012. The team was composed by Pr. Dr. Rosalina Gabriel, Márcia Coelho, Raquel Hernández, Débora Henriques and by Fernando Pereira.
This study of this gradient in the Azores is carried out in the framework of Débora’s PhD (University of Azores). Raquel (PhD student in Canaries) joined the Azorean team to be trained on the collecting methodology of the Moveclim project.
The weather was good, allowing the fieldwork to proceed within 4 days. Six altitudes were sampled along the gradient from 40 to 1000 m. This transect was set up along the western side of the island.
We briefly describe here the sampling sites and illustrate the gradient with some photographs:
40 m – Serreta lighthouse
Vegetation is composed of shrubs (scrubland). Bryophytes are more abundant on rocks, the canopy is low < 2m. The vascular flora is dominated by Erica azorica and Myrica faya.

Pix: Vegetation type of the lowland (M. Coelho)

200 m – Canada das Covas – Serreta
The forest was unfortunately dominated by non-native Pittosporum undulatum, but also by native trees like Erica azorica and Myrica faya
Pix: Bryophytes were there mainly recorded on the rocks ( R. Gabriel)

400 m – Pico Carneiro - Serreta
Forest system, the canopy is higher (maximum of 6 m). Vegetation is dominated by Pittosporum undulatum (70%). Erica azorica, Juniperus brevifolia and Myrica faya were also present but in lower quantities (25-30%).
Pix: Raquel on the field in Pico Carneiro-Serrata (R. Gabriel)

600 m – Pico da Lagoinha – Serreta
Forest vegetation dominated by Laurus azorica (40%), Juniperus brevifolia (30%) and Ilex azorica (30%). Cover of bryophytes is predominant on the soil (100%) but also very significant in trees (75%).

800 m – Trail to Lagoa do Pinheiro - Serreta
Forest system with trees up to 4 m high. Juniperus brevifolia and Ilex azorica were the most frequent trees composing the native vegetation together with Laurus azorica and Vaccinium cylindraceum. Bryophytes were more common in the trees (95%) and in the soil (75%).
Pix: Sphagnum sp in Lagoa do Pinheiro-Serrata (M. Coelho)
1000 m –Serra de Santa Bárbara
Serra de Santa Bárbara is a Natural reserve of 1863 ha with the highest peak at 1021 m. The vegetation is dominated by scrubland; bryophyte cover is predominant on the soil and schrubs. Vascular species are < 2 m high. Juniperus brevifolia and Calluna vulgaris dominate the plant composition, Hymenophyllum sp. is also abundant.
Pix: Bazzania azorica and filmy ferns (R. Gabriel)

Pix: Vegetation type in Serra de Santa Barbara (M. Coelho)

Three other islands of the Azores will be explored along an elevational gradient in the framework of Débora's PhD thesis, the rest of the field work will take place in mid 2013. Samples of the Pico and Terceira gradients are now being curated and processed for analysis at the University of Azores.

Text and Photographs: Dr. Rosalina Gabriel, Márcia Coelho, Débora Henriques, Raquel Hernández.


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Saturday, 15 September 2012

Field trip in Azores, Pico island: 4-12th September 2012

An expedition in the Azores with the purpose of sampling bryophyte communities along an elevational gradient took place between the 4th and 12th of September 2012 in Pico island. The team was composed by Pr. Dr. Rosalina Gabriel (local Moveclim coordinator), Dr. Claudine Ah-Peng (Moveclim co-coordinator), Márcia Coelho (PhD student in Azores), Silvia Aranda (PhD student in Spain), Débora Henriques (PhD student in Azores) and by Fernando Pereira (technician in the Azores University). The weather was good, allowing the fieldwork to proceed without major drawbacks within 6 days. There were twelve altitudes to sample along the gradient from 10 to 2200 m, every 200 m two permanent plots of 10 X 10 m were set, according to the BRYOLAT methodology. From 1200 to 2200 m the sampling was conducted in the Pico Mountain (2351 m), highest summit of Portugal, a stratovolcano that created the island 300 000 years ago. 


Pix: Pico mountain (2351 m) from P. Borges.


We here briefly describe the sampling sites and illustrate the gradient with some photographs:

·       10 m – Manhenha (Ponta da Ilha)
Vegetation is composed of shrubs (scrubland). Bryophytes are more abundant on rocks, the canopy is low < 5m. The vascular flora is dominated by Myrica faya, Pteridium and Erica azorica.

Pix: Manhenha, eastern point of the transect (C. Ah-Peng).


·       200 m – Cabeço da Hera
Lowland forest unfortunately disturbed with non-native Pittosporum undulatum and Hedychium gardnerianum. Bryophytes were mainly on the soil and on rocks.

·       400 m – Fetais (Piedade)
Forest system, the canopy is higher (maximum of 8 m). Vegetation is dominated by Pittosporum undulatum (80%). Erica azorica, Picconia azorica and Laurus sp. were also present but in lower quantities (15-30%). 




Pix: Although highly disturbed, this site hosts the endemic moss species Echinodium renauldii, which was here reported fertile (P. Borges). 


·       600 m – Caminho dos Burros (Chão Verde)
Scrubland and forest vegetation.

Pix: Chão Verde's site (C. Ah-Peng).


·       800 m – Caiado
Forest system with trees up to 4 m high.
Ilex azoricaEuphorbia sp., Juniperus brevifolia and Vaccinium cylindraceum composed the native vegetation. 

·       1000 m – Caveiro
Forest system where bryophytes are present and abundant in all available substrates (soil, rock, leaves and trees). Though a natural reserve, this system is surrounded by pastures with cattle. the nearby non indigenous grassland is taking over on Sphagnum colonies. 



Pix: Fernando in the vegetation of Chao Verde (C. Ah-Peng)

Pix: Hanging epiphytic bryophytes (C. Ah-Peng)




·       1200 m – Pico Mountain
Scrubland. Bryophyte cover is predominant on rocks, at the base of shrub barks and lower branches.
The dominant vascular species is Erica azorica, followed by Vaccinium cylindraceum and Blechnum spicant.

Pix: Site at 1200 m, above the Pico information centre.

Pix: Epiphytic mosses on Erica azorica (P. Borges)


·       1400 m – Pico Mountain
Scrubland, bryophyte cover is predominant in rocks. Vascular species are < 1 m high.
Erica azorica and Calluna vulgaris dominate the plant composition, with Potentilla sp. also abundant.

Pix: Shrubby vegetation at 1400 m (P. Borges)




·       1600 m – Pico Mountain
Scrubland, similar to 1400 m.

Pix: Ericaceous vegetation at 1600 m (P. Borges)




·       1800, 2000 and 2200 m – Pico Mountain
Scrubland, bryophytes are scarce but mainly present in rocks.
Vascular flora is also rarefied, dominated by Calluna vulgaris and Thymus caespititius, never reaching heights superior to 0,2 m.

Pix: Lower vegetation and rocky habitats (P. Borges).

Pix: The 2200 m site, Pico peak in the background (C. Ah-Peng)


Pix: Native Calluna vulgaris, (C. Ah-Peng)

Pix: Daboecia azorica, endemic of the Azores (C. Ah-Peng)


Apart from the lowland sites, which were disturbed with alien species, the rest of the gradient present native habitats. Near 1000 bryophyte ecological specimens of 50 cm2 were collected during this expedition, these samples are being air-dried and processed at the University of Azores for identification.




Pix: The Pico's team on the last day of field work, from left to right: Paolo Borges, Claudine Ah-Peng, Rosalina Gabriel, Fernando Pereira, at the bottom, Márcia Coelho, Débora Henriques and Silvia Aranda (P. Borges) 




This expedition was also the opportunity to discuss the PhD work of the two Portuguese students who will start working on the elevational gradients of bryophytes in the Azores, to sign the agreement between the National Park of Pico and the University of the Azores for the MOVECLIM project, to see the basaltic vineyard landscape which is Unesco Word heritage Site and to visit a lava tube of 1500 years old (Gruta das Torres).


Márcia Coelho, Débora Henriques, Rosalina Gabriel and Claudine Ah-Peng.

Photographs: C. Ah-Peng and P. Borges
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Wednesday, 29 August 2012

International Symposium: Hawai'i August 4-7, 2012


The international conference “Vulnerable islands in the sky: management of tropical island alpine and sub-alpine ecosystems” was hosted in Hawaii (Big Island), Waimea, from August 4-7th 2012. The University of Hawaii at Hilo (UHH), the office of Mauna Kea management and the Gordon and Betty Moore foundation supported this conference.
Thirty papers were presented and almost 50 people gathered at HPA Waimea for this symposium. I report below some highlights of what we talked about; linking science and management was central in the discussion.
Donald Straney (UHH chancellor), in the welcoming remarks, highlighted the responsibility of the university for managing these alpine mountain ecosystems and the unique opportunity of gathering scientists of high islands in the world for replicated systems.

Session 1: Tropical Mountain Climate Change
In his introductory talk “Losing the high ground: rapid transformation of tropical island alpine and sub-alpine environments”, James Juvik and co-authors raised the fact that the temperature inversion layer found in most oceanic islands with trade winds, has a major impact on increasing aridity at the summit areas. 
Pix: Sea of cloud on Mauna Loa (4170 m), from the trade wind inversion (TWI) layer

This phenomenon has dramatic effect on the water balance of these high altitude ecosystems. Similarly, Patrick Martin (Colorado University) showed for the Dominican Republic on a 10-year survey a rise of temperature and specifically an increase in the frequency of the inversion temperature layer. From his HALENET network climatic data sets (24 years recordings), Thomas W. Guimelluca (University of Hawaii, Manoa) could enounce with confidence an increase of temperature in the future, with less confidence a lower amount of precipitation, higher solar radiations and less clouds.


Pix: Climatic station on Mauna Kea

Consequences of increased aridity is already noticeable on the flanks of Mauna Kea, Paul Krushelnyky (University of Hawaii, Manoa) gave the example of climate associated population declines of the iconic endemic silversword, associated with continued warm and dry conditions added to damage by introduced ungulates and human vandalism.


Pix : Endangered silversword: Argyroxiphium sandwicense ssp. macrocephalum on Mauna Kea

In his talk, Henri F. Diaz (NOAA) specified that warmer oceans lead to enhance hydrological cycle as an increase of latent heat input to the atmosphere. Data from the last 80 years indicate enhanced upper elevation warming include a reduction in the frequency of occurrence of freezing temperature in the upper slopes of the higher terrain in Maui and Big island (Hawai’i archipelago). Michael Prentice (Indiana University) and Geoffrey Hope (Australian National University) supported this result, by reporting the glacier recession in Papua and New Guinea provinces, as well as the sensitivity of the alpine vegetation to climatic and anthropogenic disturbances. G. Hope highlighted the use of paleoecology to reconstruct vegetation dynamics, also emphasized by Shelley Crausbay (Colorado University) in session 2, on her study case on a glacier Lake of Haleakala volcano in Hawai’i. To end the first session Wouter Buytaert (Imperial College) gave an overview of the importance of tropical alpine grasslands for ecosystem services including water supply, biodiversity and carbon storage, with the example of the Paramó in the Andes.

Session 2: Evolution in Mountain Environments
Oceanic island summits offer a high degree of endemic species especially for plants. Mountains act as islands within islands, for space that has been already isolated. In his paper, Manuel Steinbauer (University of Bayreuth) related space and the geological evolution of island archipelagos to the diversity of high elevation ecosystems, and took the example of single island endemics, which increase with elevation. José Maria Fernandez Palacios (University of La Laguna) accentuated the effect of erosion (habitat history) on those sub-alpine island ecosystems. José Maria reminded us that summit biota frequently displays a very high endemism, which may originate from dispersal from other close summit ecosystems during peak period (multiple summit endemics), when a dispersal window remains open for pre-adapted summit biota, or more usually from the colonisation of the summits and later evolution to the new conditions from low or mid-altitude generalist species of the same island (single summit endemics). In the “No Way Out” scenario, when peaks are absent, the disappearance of summit ecosystem implies the extinction or extirpation of their competitive species. Allen Allison (Bishop Museum) gave the only example on animals, with the high altitude herpetofauna of New Guinea. Thirty-one species of amphibians and reptiles found above 2000 m are related to groups inhabiting adjacent lowlands and most are confined to single mountains summits suggesting localized evolution for amphibians (lizards and frogs).
In his talk, Jonathan Price (University of Hawai’i, Hilo) examined how biodiversity originates in tropical island ecosystems from three distinct mechanisms (1) single species colonizer like the silverword species (2) colonization from pre-adapted species (Sophora sp.) (3) shift to alpine. He looked at the relative contribution of colonization, adaptation and speciation on three archipelagos (Hawaii, Canarias and Mascarenes). He found that Hawai’i hosts the highest number of endemic species, which can be related to extreme isolation of this archipelago) and that most of these islands are endemic originate from pre adapted taxa. Community assembly has therefore been shaped somewhat by habitat filtering in these island systems.

Session 3: Ecosystem Dynamics
This session was diverse and varied from studies on tree line shifts in Taiwan from Sarah Greenwood and Alistair Jump (University of Stirling), ecology, altimontane bryophyte diversity and distribution, effect of herbivores and fire on diversity in Canarias from Severin Irl (University of Bayreuth), conservation and management in West Africa (Drew Cronin, Drexel University) and paleoecology (Shelley Crausbay, University of Colorado).
I presented the functional diversity structure of bryophyte communities along the upper elevation gradient of the Piton des Neiges volcano showing that the functional diversity index based on 8 traits decreased with altitude, supporting the hypothesis that increased environmental adversity leads to an homogenization of traits for this sub alpine bryophyte communities indicating also that these community may be resilient to perturbations.
Fabien Anthelme (Institut de Recherche et Développement) presented his work on the Andes, considering alpine islands are summits surrounded by continental lowlands. He documented, from 24 literature sources, the percentage of species restricted to alpine environments, the isolation by spatial distance and by size of alpine environments for plants and invertebrates. Among his results, he showed that tropical alpine environments for these organisms behave distinctly from their counterparts in extratropical alpine environments.

Session 4: Mauna Kea
James Juvik, in his conference introduction, raised concern about the Mauna Kea volcano (4169 m), which is at the same time considered as a sacred mountain by the native community but is also used by scientists (astronomy…), hunters, hikers, these users share a small area with high human impact.

Pix: James Juvik holding some very hard rock obsidian, which the polynesians used as an adze. This hard rock comes from the previous glacier that existed on the highest part of Mauna Kea above the basalt. So Polynesians were taking a long journey to collect this rock and purify and heal in the lake Waiau (below); left Stéphanie Nagata (OMKM)

This last session of the symposium was about the Mauna Kea volcano, Stéphanie Nagata (Head of the Office of Mauna Kea Management) reviewed the 12 years of community-based management of this high system. Grant Gerrish (University of Hawai’I, Hilo) described this alpine vegetation and habitat types. Jesse Eiben, entomologist, showed how research program centred on a single alpine endemic insect the Wekiu bug (Nysiuswekiucola) informs ecosystems level resource management. This bug is found only on the summit of Mauna Kea and is highly dependent on wind-blown, gravity-deposited, insect prey from lower elevation.
To end this conference, discussion was lead on the management of the high alpine zone of tropical oceanic islands especially on the effect of tourism and scientific activity. Sonia Juvik in her paper “ In search of a post modern paradigm for land use management on tropical high mountains” gave her analysis on the Mauna Kea case study.
Recommendations from the representatives of the different islands present at this symposium were gathered into three main points:
1) Public use issues
2) Science management interface
3) Long term environmental monitoring.
There was a strong will from the audience to build local expertise, to initiate comparative studies on the tropical alpine environments and to consolidate this network, with the possibility to set a future meeting in the Canaries.

This symposium was punctuated with social events including Hapuna Beach swim and barbecue, a night at Hale Pohaku at the astronomy centre where we did star gazing and were granted to see Saturn’s rings very clearly. The next morning we were very lucky to go to the Mauna Kea summit and hiked to Lake Waiau. 

Pix: Summit of Mauna Kea 


Pix: The monitored Lake Waiau (3979 m) utilizing 3D technological approaches by Donna Delparte's team (UHH). Concern about declining lake levels has created the stimulus for this study to use techniques to monitor lake level without disturbing the lakes.

To end the conference we attended a Luau in Kona, which is a celebration of South Pacific culture rythmed by Polynesian dances from Hawaii, Samoa, Fiji, Tahiti...


Pix: Luau in Kona

With another six attendees we embarked on a two day- post conference field trip with John Delay (PhD student at the University of Hawaii). We had the opportunity to visit and learn more about the different habitats on Big Island (Kipukas, lava tubes, Akaka waterfalls…).

Pix: the crew of the post conference field trip

Pix: Waipi'o coast

Pix: Akaka falls

Pix: Acacia koa, closest relative is Acacia heterophylla in Réunion island.

Pix: Metrosideros polymorpha, endemic pioneer tree on lava flows

Pix: Current eruption at Mauna Loa volcano

I feel very lucky to have the opportunity to take part to this symposium and wish to thank the organizing committee for the excellent job they did to assemble this program, the time and energy they dedicated to make this symposium inspiring and enriching.
For those who would be interested to learn more, the proceedings of this symposium will be featured in the journal of Arctic, Antarctic and Alpine Research.

Mahalo!

Claudine Ah-Peng
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