Marsden Rocks and Cleadon Hills

The cliffs at Marsden Bay are spectacular even in December. Composed of 16-20 metres of cream and buff dolostone of the Concretionary Limestone formation, commonly referred as the Mag limestone formed in the late Permian period. The large sea stack in the picture below is composed of collapse-brecciated Concretionary Limestone.  Stacks like Marsden Rock were once joined to the mainland but weaknesses in the limestone create caves, arches and stacks over time. A spectacular coast is the result.

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The cliffs are made of layers of Magnesian Limestone which formed in the ancient Zechstein Sea. Within the original rock sequence was a thick layer of a soluble salty mineral (Hartlepool Anhydrite), which formed during a period when the Zechstein Sea evaporated and became saltier. After millions of years, the sequence was tilted and uplifted above sea level and the anhydrite dissolved away. The limestone above it collapsed and broke up. These broken up and fractured rocks are known as ‘collapse breccias, they are visible in the deformed cliffs below on the bottom right hand corner.

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Seabirds use these coastal features for nesting. Although the fulmar pairs below won’t be nesting until May, the female has glands that store sperm to allow weeks to pass between copulation and the laying of the egg.

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Sinkholes are a feature of this coastline.

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These impressive limekilns were built in the 1870s. Layers of limestone and coal were dropped in the top and burnt to make lime, which was used to improve acid soils and to make cement and concrete. Lime was also important for the steel and chemical industries. Coal sourced from from Whitburn Colliery fired the kilns. A village was built to house workers for the colliery and limeworks. After the colliery closed in 1968 the village was no longer needed, people moved to new houses nearby and the village was demolished. The cliff-top grassland where the village stood became a grassland of lime loving or calcicole plants.

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Cleadon Hill is a ridge of high ground standing between the village and the coast. Around 260 million years ago the hills were, together with others in the area, a group of small low islands in a tropical lagoon formed by the Zechstein Sea. Is it a conservation area due to its plant-rich magnesian grasslands. Exmoor ponies are helping to maintain the flower rich areas by grazing the rougher grass species.

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Some lichens prefer limestone as a substrate such as bright white Aspicilia calcarea below, growing on a wall.

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and the orange yellow rosettes of Caloplaca flavescens.

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The site is also dominated by the landmark Cleadon Water Tower, in fact a chimney for the former steam-powered pumps, which is visible for miles around, as far south as the Headland in Hartlepool.

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The views to all sides are worth the short climb. To the South, Roker pier is visible,

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while looking to the North, Tynemouth Pier and Priory are prominent.

OLYMPUS DIGITAL CAMERAMarsden Old quarry is a Nature Reserve forming a patchwork site of a variety of habitats which include areas of lowland meadow and pasture, magnesian limestone grassland and some semi-improved neutral grassland. This site of approximately 6.3ha supports an abundance of wildflower species such as Kidney vetch, Hoary plantain and Common Bird’s-foot Trefoil as well as Lady’s Bedstraw and Bee orchids. The geology is also of great interest and worth further exploration.

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Gorse (Ulex europaeus)is always a thorny subject but this one was not in flower.

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With the coming evening the clouds were colouring up over the golf course,

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and The Cheviot hills unmistakeable in the distance.

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Reference:

Durham coast SSSI

A Magnesian Limestone Geotrail

Cleadon geology

Rothley Circular Walk

This winter walk took a route along part of the the Wanney line, Rothley Lake, Crag and Mill.

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Without leaves it was difficult to identify this tree from it’s shining berries but the fallen leaves looked like cotoneaster so probably it was Hedge cotoneaster (Cotoneaster lucidus.)  A flock of Fieldfare were seen nearby so the berries might be as attractive to them as to us.

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The path took us along the Wanney or Wannie line named after the river Wansbeck. Originally thirteen miles long, starting from Morpeth, it reached Rothbury in 1870 after seven years in construction. It was used to carry coal, stone, livestock, lime and passengers before its closure to passengers in 1952 and freight in 1963. Sir Walter Trevelyan, owner of Wallington (1846-1879) was the driving force behind the building of the railway. The revenue that came to the estate was spent on his house and improving the estate.

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On the way we sought out this  venerable hollowed ancient ash tree. Ash trees can live for 400 years or more if they have been coppiced or pollarded. The hollow structure actually helps them survive longer.

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Evidence  of ridge and furrow cultivation in the photo above, typical of the open field system in the middle ages when non reversible ploughs were used. It survives on higher ground where arable fields were converted to sheep walk in the 15th Century and not ploughed since.

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The characteristic S shaped pattern of ridges ploughed by oxen is shown in comparison to the straight rig and furrow. Oxen were yoked in larger teams than horses and since they ploughed in a clockwise direction needed more turning room. In the background, Rothley Crags shows its windy exposures by the lack of vegetation unlike the plantation below.

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These interestingly shaped leaves belong to Intermediate wintergreen (Pyrola media).

 

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The lake forms part of the deer-park created by Sir William Calverley-Blackett (2nd Baronet) the owner of Wallington Estate who built Rothley Castle as a folly and the Codger Fort to prove loyalty to King George II during the Jacobite rebellion. The lake was landscaped by Capability Brown. The bird feeders by the lake hide were thronged by tits: Blue, Great, Coal and a pair of delightful Marsh tits. Nuthatch and chaffinch also visited while a Crossbill was heard in the trees.

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The lake surroundings have been planted with Scots Pine, Sitka spruce and Beech but moss thrived among old stumps as did Caluna vulgaris and Bilberry. Given the red stems, this moss is Red-stemmed feather moss (Pleurosium schreberi) an inhabitant of open heathy woodland.

c portentosa.JPGLichens survive in exposed moorland conditions of Rothley Crag. The lichen above is Cladonia portentosa, perhaps not as widespread as it should be in these conditions. Parmelia omphalodes, below, commonly seen on exposed base-poor rocks such as the Rothley grits.

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Sphaerophorus globosus is a bushy attractive lichen apparently fairly common in upland areas.

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Sphaerophorus fragilis, however, forms more compact cushions, lacks the pinkish tinge and usually grows at greater altitude.

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All we saw of Rothley mill was this attractive trough. The mill was a water-powered cornmill on the Hartburn, now a private dwelling, interesting in legend as the dwelling place of Queen Mab and her fairies. A dipper was seen on the Hartburn and a yellowhammer on the trees nearby.

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Reference:

Lichens – Frank S. Dobson

Collins Wild Flower Guide- David Streeter at al.

 

 

 

Bolam and St Andrews church

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It was a cold day when the Botany group went for a winter walk at Bolam. The Lake is artificial, designed by John Dobson and constructed in 1816 for the Rev John Beresford, who became Lord Decies in 1819. Beresford wanted to help local people through the agricultural depression and upheaval after the Napoleonic Wars by providing employment. It was, however, a fashionable enterprise since his neighbours were busy making improvements to their estates. Sir Charles Monck was undertaking building and landscaping work on Belsay Hall and grounds, while Sir John Trevelyan created a grand estate at Wallington landscaped by Capability Brown.

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In spite of the cold some fungi were flourishing, Velvet Shank (Flamulina velutipes) had colonised this tree trunk.

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St Andrew’s Church has a square late Saxon Tower but the interior is largely Norman with the arcading dated to 1180-1200. The quatrefoil piers with their broad moulded capitals are unique to St Andrew’s.

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These mysterious Saltire crosses inscribed on a pillar inside are presumably in honour of the martyrdom of St Andrew.

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Medieval gravestones bearing skulls and crossbones were common. The name is obscured by lichen but the message of ‘memento mori’ is still visible. Lichens are long lived and thrive on old gravestones. The lichen with the black apothecia looks like Tephromela atra while its neighbour with the red/brown discs is Trapelia coarctata.

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Ramalina farinacea, the bushy lichen and the bluish leafy Parmelia saxatilis are pictured on another stone below.

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From the churchyard the view shows the stretched ovoid form of a drumlin and craters in the foreground, formed in 1942 when bombs fell from a German Dornier airplane.

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Two roe deer can be seen running across the fields adding to a memorable winter scene.

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In spite of the frost some plants were flowering, like this Daisy (Bellis perennis) growing among Parsley piert (Aphanes arvensis) on the bank of this ha-ha. A ha-ha is a recessed landscape design element that creates a vertical barrier while preserving an uninterrupted view of the landscape beyond.

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Peltigera lichen was thriving on the mossy bank. Most Peltigera species have the cyanobacterium Nostoc as the dominant algal partner but some contain small gall-like growths of the chlorophyte Coccomyxa containing Nostoc. Because of their ability to fix nitrogen from the atmosphere, such lichens are influential in soil composition and generation.

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An ornamental ivy, probably Canarian Ivy (Hedera canariensis) naturalised on a roadside verge added a seasonal interest.

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Reference: https://www.northumberland.gov.uk/NorthumberlandCountyCouncil/media/Neigbourhood-and-Local-Services/Parks%20and%20open%20spaces/Bolam%20Lake%20200years%20project/17957-Bolam-Interpretation-Booklet-A5-Print2-LR.pdf

Hindhope Linn

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This secluded waterfall on the edge of Kielder Forest, now mostly conifer plantation, proved an interesting field trip for Ferns, Bryophytes, Fungi and Lichen. Linn is a Northumbrian word for a waterfall or the pool at the base of it. The Blakehope Burn tumbles over a sandstone escarpment in the Carboniferous sequences that make up most of Northumberland’s bedrock to form an impressive cascade. We visited in late October but Pink Purslane (Claytonia sibirica) was abundant and still in flower by the base of the fall.

The picture below is of Scots Pine (Pinus sylvestris), a species regarded as one of the three native conifers of the UK, but only the subspecies scotica is a genuine native. These are grown from non-native seed.

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The forest included large stands of Sitka Spruce (Picea sitchensis) and Douglas Fir (Pseudotsuga menziesii)  both of which were originally introduced from the US by the botanist David Douglas. On the outskirts of the forest near the car park deciduous trees were still in green leaf: Common Alder, Goat, Grey and Eared Willow were thriving. Eared willow (Salix aurita) native to Europe, is a multi-branched woody shrub and a pioneer species, commonly occurring in wet sites in the Caledonian Forest and upland Northumberland. It is identified by its conspicuous stipules.

It was too dull and wet for successful photography but Ferns such as this Lady fern (Athyrium filix-femina) shrugged off the rain.

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Common Polypody (Polypodium vulgare) often grows as an epiphyte, in this case on a side branch of a Sessile Oak (Quercus petraea).

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Various ferns were noted: Hard fern (Blechnum spicant), Male fern ( Dryopteris filix-mas), Borrer’s scaly male (Dryopteris affinis subsp Borreri), Broad Buckler (Dryopteris dilatata), Lemon scented (Oreoptteris limbosperma) and Bracken (Pteridium aquilinum).

Liverworts like it wetter than ferns and this Greater Featherwort (Plagiochila asplenioides) pictured below was growing near the footpath. White Earwort (Diplophyllum albicans), Bifid Crestwort (Lophocolea bidentata) and Overleaf Pellia (Pellia epiphylla) which prefers acid soils, were recognized.

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A good selection of Moss species were growing well. Common Haircap (Polytrichum commune) with Wood sorrel attempting to grow through it, likes high humidity and rainfall.

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As does this Tamarisk Moss (Thuidium tamariscinum). It often appears transparent especially in the wet.

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Other Bryophyte species: Bank Haircap (Polytrichastrum formosum), Juniper Haircap (Polytrichum juniperinum), Swan’s neck thyme moss (Mnium hornum), Big Shaggy (Rhytidiadelphus triquetrus) and Litttle Shaggy mosses (Rhytidiadelphus loreus). It was wet enough for Sphagnum mosses such as Flat topped bog moss (Sphagnum fallax), Blunt leaved Bog moss (Sphagnum palustre), and even Red Bogmoss (Sphagnum capillifolium) to form cushions on the woodland floor.

Among the rich lichen flora it was a surprise to see Bryoria fuscescens growing well on Scots Pine where sufficient light lit the rough bark. Platismatia glauca is the leafy lichen on the right hand side of the photo.

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There was a confusing collection of Cladonia lichen; C foliacea is the leafy lichen at the bottom of the photo, the cups probably belong to C pyxidata but they are difficult to identfy. Parmelia sulcata is the leafy lichen at the top.

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This one looks like Cladonia glauca.

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Stone also provides a good substrate for crustose lichens; Porpidia cineroatra below has ashy black fruiting bodies and black prothallus. Other lichen noted: Cladonia sulphurina, C squamosa, C polydactyla, C furcata.

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Fungi were much in evidence given the wet mild weather. This coral fungus looks like  a Ramaria of some kind.

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Wrinkled club (Clavicula rugosa).

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Amanita vaginata, the Grisette, though not poisonous has a volva like a Deathcap.

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Ochre Brittlegill (Russula ochroleuca,) one of the most common of all the brittlegills, is  plentiful in pine forests and has mycorrhizal associations with the tree roots.

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The Myxomycetes, or slime moulds, are a group of  protists. They are microscopic, non-pathogenic bacterivores, which help to decompose plant remains. They are found in all terrestrial ecosystems, and about 1000 species are known worldwide. They are particularly abundant in temperate and tropical forest, but many species are also adapted to live in extreme environments. They form part of a group now called Amoebozoa. They are evolutionary significant, since they are considered to be one of the first attempts in the evolution of organisms towards multicellularity. They coalesce, in favourable conditions, into a moving plasmodial stage to meet mating partners and form spores.

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Possibly this is Badhamia folilcola which often coats grasses.

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Rainbows are formed by reflection, refraction and dispersion of light in water droplets. This one appeared to have an end in the woodland but rainbows are not located at a specific distance from the observer. They are an optical illusion caused by any water droplets viewed from a certain angle relative to a light source. Unfortunately, a rainbow is not an object and cannot be physically approached. Indeed, it is impossible for an observer to see a rainbow from water droplets at any angle other than the customary one of 42 degrees from the direction opposite the light source. Even if an observer sees another observer who seems to be at the end of a rainbow, the second observer will see a different rainbow—farther off—at the same angle as seen by the first observer.

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Reference: http://www.myxotropic.org/myxomycetes/

http://www.myxotropic.org/myxomycetes/

https://en.wikipedia.org/wiki/Rainbow

Lichens – Frank S Dobson

Collins Complete Guide to British Mushrooms and Toadstools – Paul Sterry and Barry Hughes

 

Warks Burn Woodland Lichen

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In mid July this woodland had some interesting lichen on show.  Many looked like the writing lichen. Graphis. The photo above looks like Graphis scripta and the lichen with the dark fruits and rhizines, shown below, Physcia leptalea.

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Thelotrema lepadinum below is an indicator species for ancient woodland. Its doughnut fruits look like acorn cups.

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A classic version of Graphis scripta below. It prefers smooth barked trees like Hazel.

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Above and below depict more scribble lichen, perhaps Graphina anguina below?

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Another example of a Opegrapha lichen looks like O atra.

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A tableau of lichen: Ramalina fastigiata with the trumpet apothecia; Lecanora symmicta with the flat jade mosaic of apothecia and the common urban sunburst lichen, Xanthoria parietina coloured yellow.

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Lastly, another woodland lichen possibly Micarea lignaria.

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Warks Burn is noted for much rarer lichen mentioned in the SSSI. My walk through was brief and limited to a few quick photographs.

Reference: https://designatedsites.naturalengland.org.uk/PDFsForWeb/Citation/1000455.pdf

Holystone – Lichen

On the 20th January 2019 another visit to Holystone woods brought blue skies and this view of the Simonside hills. Lichen stands out in the winter, even this Bryoria fuscescens, camouflaged half way up an Oak tree in the ancient planted woodland, stood out.

There were two Peltigera lichen growing by a farm entrance, Peltigera rufescens below has red/brown discs.

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Peltigera membranacea has a bullate (wrinkled) upper surface with many white rhizomes visible underneath.

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Fallen rotting tree trunks provide favourable places for Cladonia lichen. Those below look like C pyxidata (pixie cups).

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Slender ashen grey podetia are a hallmark of C glauca on the same tree.

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The lichen with the thick yellow green podetia is C sulphurina.

In contrast to the Cladonia above this acid green squamulose one is C squamosa.

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The cladonia below has red/ brown fruits and could be C ramulosa.

By St Ninian’s Well or Lady’s Well there were various Pertusaria (bored through) type lichens such as P pertusa below on a beech tree.

P multipuncta below looks like tiny pepperpots,

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whereas P amara tastes bitter. It has been used a treatment for malaria.

Thelotrema lepadinum is an indicator of ancient woodland and good air quality. It is surrounded by other lichens: Parmelia sulcata and Ramalina farinacea.

The statue of St Ninian has acquired some lichen and a covering of orange algal Trentepohlia. It is actually a green alga and often associates with fungi as lichen.

Big Waters – Lichen, Fungi etc.

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This Hawthorn bush was still covered in fruit. According to The Woodland Trust:

Common hawthorn can support more than 300 insects. It is the foodplant for caterpillars of many moths, including the hawthorn, orchard ermine, pear leaf blister, rhomboid tortrix, light emerald, lackey, vapourer, fruitlet mining tortrix, small eggar and lappet moths. It provides nectar and pollen for bees and other pollinating insects. The haws are rich in antioxidants and are eaten by many migrating birds such as redwings, fieldfares and thrushes, as well as small mammals. The dense thorny foliage makes a good nesting shelter for many species of bird.

An example of Ramalina fraxinea growing on an Ash tree. I was surprised to find it here at Big Waters among  abundant Xanthoria polycarpa.

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On the same trees Ramalina fastigiata was flourishing and R farinacea was present but less spectacular. All of these like well lit nutrient enriched bark.

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Lichen often forms mosaics on tree trunks. Lecidella elaeochroma is lined by a black prothallus separating it from Lecanora chlarotera with the buff apothecia.

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The green Lichen with the large black apothecia is Physcia aipolia.

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Another common physcia pictured below looks like P caesia.

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The bryophyte on the picture above and below is Orthotrichum diaphanum. It had silvery leaf tips.

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In the nature reserve Jelly Ear fungus (Auricularia auricula-judae) sprouting from Elder.

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The fungi below, festooning the fallen log is Stereum hirsutum.

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Not all fungi are easy to identify. It is late in the year. so it is possible that this violet stiped gilled mushroom is a Wood Blewit (Lepista nuda). It will fruit until December.

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References:

The Woodland Trust

Blyth South Beach to St Mary’s in December

This picture of South Beach shows the blue sky and white topped waves driving onto the sands invigorating dog walkers, sailors and surfers. The dunes are well covered in Marram and Lyme grass.

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The wind turbines on the horizon are two of the five that comprise Blyth Offshore Demonstrator Wind Farm.  Newly installed, they have gravity based foundations that ‘float and submerge’ in the 40 meter depth of water. They provide electricity for 34,000 homes and were built locally in Wallsend.

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The driving seas had whipped up foam and rainbow bubbles on the shore. According to the wiki: Sea foam, ocean foam, beach foam, or spume is a type of foam created by the agitation of seawater, particularly when it contains higher concentrations of dissolved organic matter (including proteins, lignin, and lipids) derived from sources such as the offshore breakdown of algal blooms.

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A raft of Eider Duck had no trouble negotiating the swells. They are true sea ducks feeding on molluscs especially mussels. A few of the males were still in their colourful breeding plumage. Eider are a feature of the Northumberland coast and are Amber listed.

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Oyster catchers were quick to feed on the rocks at Seaton Sluice as the tide receded. Like the Eider, they also eat cockles and mussels when at the coast.

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While walking along I took notice of the plants in flower such as the Prickly Sow thistle (Sonchus asper) shown below. The plants still in bloom were mostly ruderals like Groundsel (Senecio vulgaris), Daisy (Bellis perennis), Ragwort (Jacobaea vulgaris), Dandelion (Taraxacum agg.), Chickweed (Stellaria media), Shepherd’s purse (Capsella bursa-pastoris), Yarrow (Achillea millefolium), Annual meadow grass (Poa annua), White Dead Nettle (Lamium album). Among the many sea-side plants, Thrift (Armeria maritima), though not in flower, had dried flower heads on show.

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As the tide ebbed many birds flew in to feed, like this Curlew. Redshank were fairly numerous but there were some Dunlin, Lapwing, Turnstone and two pairs of Ringed plover. Gulls of various kinds and crows had also taken to the rocks.

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The lake on the bird reserve held a pair of Canada Geese, Mallard, Heron, Moorhen and a flock of Teal. On the scrub by the wetland I had caught a glimpse of a small bird with a white belly. Although I wondered what it could be, a bird watcher later told me to watch out for a pair of Snow Bunting. It seems likely the birds I had seen were Snow Bunting (Plectrophenax nivalis). Regularly wintering along the coast they are Arctic specialists, though a few nest in the Cairngorms. On Whitley Beach, avoiding the walkers and dogs, a flock of Sanderling, another Arctic breeder also here for the winter, was in constant movement along the water’s edge by the tide wrack.

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At Seaton Sluice, on a stone wall, this Acarospora fuscata lichen looked like dried mud.  Crab’s Eye Lichen (Ochrolechia parella) was covering the wall tops in large white patches.

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This Lichen looked like Lecanora campestris with its dark red apothecia.

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On the same wall, always worth a visit, a brightly coloured Caloplaca glowed, perhaps C verruculifera?

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Lichen often grow on top of one another. The whitish base lichen is (Apsicilia caesiocinerea) but there is a Lecanora possibly L dispersa growing on top.

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References:

Wind Farm

Sea foam

Holystone Woods – Lichen

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Holystone wood is noted for its lichen flora. The SSSI mentions a luxuriant community of epiphytic lichen including Bryoria and Usnea subfloridana.  Many species are present which are associated with ancient woodland: Mycoblastus sanguineus, Thelotrema lepadinum and Pertusaria spp. The large oak shown above was a haven for Bryoria lichen. The tree in top left is covered in Usnea, Bryoria and Ramalina sp.

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A close up the fruiticose Bryoria fuscescens on the large oak reveals its dark smoky-brown colours, and pendant, hair like filaments. It grows on acid barked trees.

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Chrysothrix candelaris a leprose lichen formed a bright yellow/green splash on an oak tree.

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Thelotrema lepadinum is another lichen with a Western and Northern distribution.  The name  lepadinum refers its limpet like appearance though it is also commonly known as the barnacle lichen.

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This crustose lichen growing near the Thelotrema is Pertusaria pertusa. The same Beech tree also hosted P amara (a bitter tasting lichen) and P hymenea. Pertusaria corallina was abundant on rocks and walls.

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Arthonia radiata has crowded black starry apothecia. Itis often found on smooth barked trees like Ash.

OLYMPUS DIGITAL CAMERA Mycoblastus sanguineus is a crustose lichen found on hard sandstone rocks. Could this be a specimen?

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This crustose lichen, thickly covered in apothecia, looks like Lecanora gangaloides although I did not scratch it to reveal the orange colour underneath. Its lookalike Tephromela atra flourished further along the same wall.

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Many species of crustose rock lichen such as Lecidea lithophila pictured above were abundant on the stones.  Frequently red coloured from the deposition of iron oxides,  L lithophila is common in the upland North and West.

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It was surprising that so many of the lichen were fruiting, like this Lecanora rupicola above.

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The apothecia shown above on this fruiting Parmelia saxatilis have orange-brown discs and isidiate margins.

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Cladonia (cup lichen) also featured on this wall. The example above is the two pronged, Cladonia furcata.

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Cladonia polydactyla seems to be ubiquitous in upland Northumberland. It has scarlet red fruits on its many fingers. The lichen with the thicker stalks is C sulphurina.

Reference:

Lichens – Frank Dobson, BLS, 2018.

http://www.lichens.lastdragon.org/indexP.html

Rothley Crags and Greenleighton Field-trip

The main aim of the outing was to examine and understand the geological context for the formation of the soils in the area. In the Carboniferous period (359 to 299 million years ago) the Great Limestone sequence was deposited across Northern England. Rothley Crags originated from the sediment of a large river that once flowed through Northumberland. The crags have been exposed by a series of geological faults running SW- NE and subsequent glaciation. From the top of Rothley Crags, the misty view below shows the agricultural field-scape, clearly different from the foreground rough grassland of the Crags. Bilberry and Bracken vegetation predominate on the exposed high ground of the grits. Typical acid plants like Climbing Corydalis and Tormentil were identifiable. OLYMPUS DIGITAL CAMERA

The influence of glacial processes of erosion and deposition can be deduced in the types of soil that we can see today such as clay and silt based loam.plantation core.JPG

We dug a pit about one foot deep in a modern conifer plantation. The soil was dry Mor with a thick unconsolidated humus layer on top. Conifers like Norway and Sitka Spruce depend on fungal networks (mycorrhiza) within this layer to provide them with nutrients such as nitrogen. The fine roots in this layer had visible white mycorrhizal tips.  A nitrogen supplying fungal associate, (Russula ochroleuca), was fruiting throughout the plantation. The soil was a shallow Ranker. Rankers are soils developed over non-calcareous material, usually sandstone rock. They are are often called A/C soils, as the topsoil or A horizon is immediately over the C horizon (parent rock) and lack a B horizon of leached material.

We moved on to test other areas area in the grassland on the approach to the Crags.  The right hand core pictured below was from a wetter rushy area and the left from a drier section nearby. Both of these were well turfed with no unconsolidated humus litter on top. The wet core harboured several worms, common inhabitants of Mull soils. They both contained ABC horizons. The B horizon largely consisted mainly of clay and was gleyed in both cases. The greyish or bluey-grey colours and orange mottling are characteristic  of gley soils but of secondary origin, replacing those inherited from the parent material. They result from the absence or very low levels of oxygen when iron compounds are changed chemically from their usual brown colours (reduction of ferric iron compounds to ferrous compounds).  This layer had no roots visible. The C Horizon in both samples was of unconsolidated parent rock (sandstone). There was a more obvious gleyed horizon in the wet sample due to greater waterlogging.

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These fields were grazed by cattle and sheep and had been in use since probably late Neolithic/Bronze Age. Janet found evidence of this; a worked flint in the left hand core. The grassland was rich in fungi but mostly associated with the animal manure.

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The moss and lichens on the sandstone crags formed intricate gardens of numerous species such as Cladonia sulphurina depicted below. C diversa,  C polydactyla, C macilenta, C ciliata and C furcata were abundant. Crustose lichens such as Pertusaria coralina, Parmelia saxatilis and Acrospora fuscata were visible on the bare sandstone.   Sphagnum mosses, such as S capillifolium and S palustre indicated the waterlogged soil conditions.

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In Greenleighton Quarry the Great limestone was exposed in thick posts with thinly bedded shales between.

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We augured a core from the field on top of the quarry. It was a thick Mull soil with ABC horizons showing little gleying. The deep brown  A layer was thick and wormy. There were many large mole hills in the field suggesting a deep fertile soil. It had been cleared  of large rocks at some time judging by the scatter on the wetter field below.  A thin gleyed B horizon was present but unexpectedly there was no limestone in the C horizon. Unconsolidated pebbly sandstone and some stony material were sandstone. The field looked as if it had been improved since white clover and perennial ryegrass were predominant and fungi was scarce.

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The quarry floor was rich in fossils found in tumbled rock including the type fossil of Pleuoplugnoides greenleightonensis, a carboniferous brachiopod pictured below in the shale.

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A  broken mass of fossils below hints at the turbulent history of the shale, the chainmail like pieces are possibly the bryozoan (Fenestella plebeia).

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I was intrigued by these traces along this rock,

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and this Echinoid fossil.

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The species of moss and lichen were different here, reflecting the calcareous nature of the limestone rock. The crustose lichen, with marked pitting. is probably Verrucaria baldensis,  a species common on hard limestone. The acrocarpous moss is Grimmia pulvinata.

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References: Mycorrhiza