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PS24 Alba territory vegetation

You are here: Home1 / Civic Museum of Archaeology and Natural Sciences “Federico Eusebio”, Alba2 / PS24 Alba territory vegetation

PS24a. Cool side

ECOLOGY

Langhe north-west hilly sides are cool and damp because of their exposure and geological strata. Here woods are luxuriant: natural competition and cuttings made by man accentuate samples growth in height.

THE WOOD

The shady mantle of the forest is made up of many arboreal species, among which stand out beech trees (Fagus sylvatica), chestnut trees (Castanea sativa), maples (Acer sp.Pl.), hornbeams (Carpinus betulus), cherry-trees (Prunus avium), oaks (Quercus sp. Pl) and lindens (Tilia platyphylla).

HUMAN INTERVENTION

In this watery and little steep sides, man has always placed side by side forest care to agriculture and farming. Therefore, there are cereals arables (barley, wheat, corn), pastures and poliphita meadows which are destined to zootechnics for meat production (Piedmont bovine race), milk for cheese production (Langhe sheep), or also to particular hazel trees cultivations (Langhe “tonda gentile”).

THE UNDERGROWTH

The cool side undergrowth hosts plants that prefer high humidity levels and are pleased with low light that seeps in leafy branches. Because of  shadows, species that live in this habitat carry out their reproductive cycle (blooming and fecundation) before trees come into leaf. At the end of february, when snow is melting, there is the blooming of Hellebores (Helleborus foetidus and Helleborus viridis), Dog’s-tooth violet (Erythronium dens-canis), Primrose (Primula vulgaris), Liverleaf (Hepatica nobilis), Wood anemone (Anemone nemorosa), Lily of the valley (Convallaria majalis), Perwinkle (Vinca minor), Solomon’s Seal (Polygonatum multiflorum), etc. Moreover, in dampest places, terrains and trunks are fungi and moss-covered.

 

PS24b. Dry side

ECOLOGY

South-east sides are more dry because of layers grade, that directs subsoil water to the opposite slope. Here trees create xerophilic woods, i.e woods populated by organisms that prefer dry lands.

THE WOOD

Langhe and Roero dry wood is almost entirely composed by the association between Pine (Pinus sylvestris) and Downy oak (Quercus pubescens), in addition to Manna ash (Fraxinus ornus), the invasive false Acacia (Robinia pseudoacacia) and a set of shrubs (Viburnum lantana, Coronilla emerus, Ligustrum vulgare, Cytisus spp.).

THE UNDERGROWTH

The wood is less dense than the one located in damp sides and leave enough space for clearings that in spring and summer are plenty of luxuriant and colorful blooming, of which Broom yellow (Spartium junceum) and Cupid’s dart blue (Catananche caerulea) stand out.

Moreover, this also is the habitat where the largest part of the characteristic 44 species of Native Orchid is found.

HUMAN INTERVENTION

Given that south side is sunny, it is the ideal place for particular cultivations; for this reason man has always tried to create terracings that promoted an high quality viticulture. The exposure to majors winds that came from the sea, the more delicate vegetation and the peculiar dryness ensure that this sides are easily vulnerable to fires.

 

PS24c. Damp environments

VALLEY  FLOORS AND WATERCOURSES

Valley floor areas that are associate with the three main Alba territory watercourses (Tanaro, Belbo and Bormida rivers) show a peculiar flora. Terrains which are next to rivers are periodically submerged by overflows and host an association between shrub-like and bushy plants, known as “Gorreto” (from “gorra”= willow). In addition to different species of willows (Salix caprea, alba, purpurea and triandra) there is also the Tree of heaven (Ailanthus altissima). Where water becomes stagnant or remains several months of the year there is the prevalence of the Bulrush (Typha latifolia) and of the Common reed (Phragmites australis); underfoot there are sedge-grass and reeds. In spring and summer “Coltellaccio” (= “large knife” for leaves shape) (Sparganium erectum) and Purple loosestrife (Lythrum salicaria) blooming is clear. The flat terrain and the presence of water make these environments ideal for agriculture. In this sense the development of forage crops and the Poplar plantation are remarkable.

DAMP AREAS

The last natural swampy area in Langhe is located near sources of the torrent Belbo, in the  district of Montezemolo. In this area, protected as a natural reserve, there are many species of botanical interest, as the rare Carex hartmanii.

FISH FARMS

In the upland that from the top of the Roero cliffs goes as far as Torino man creates many small lakes or “fish farms”, taking advantage of the impermeability of the layers. The majority are destined to irrigation and fish farming (Tinca tinca). Moreover, these host fauna and flora components of high interest, such as Indian Lotus (Nelumbo nucifera) that populates the fish farm of Cascina Gallina in Ceresole d’Alba.

 

PS24d. Microenvironments

TERRACINGS

South-east sides are dry and steep and have been fitted for cultivation thanks to a long and impressive  work of terracing. The big dry sandstone walls is juxtaposed in order to support terrains which host a peculiar flora from Mediterranean area, such as bush of Red valerian (Centranthus ruber), Snapdragons (Antirrhinum spp.) or the rare Navelwort (Umbilicus rupestris). Not to be negligible is the presence of succulent plants such as the yellow-blooming  Sedum or the red Sempervivum.

I “CROTIN”

Where the terracing work meet a waterproof clay layer intercepting a phreatic layer, man has created small products called “Crotin” to collect the precious water.

These cool environments are adorned with elegant bushes of Maidenhair fern (Adiantum capillus-veneris) and perfumed mint (Mentha aquatica). In near terrains, in which some water  permeates, we can find the Celandine (Chelidonium majus), the Wall rocket (Diplotaxis muralis) and the certain Upright pellitory (Parietaria officinalis).

LE “ROCCHE”

The geological phenomenon called “cattura del Tanaro” and the water course erosion have created steep and semi-desert sides in Langhe e Roero: the “Rocche” (i.e. Cliffs). From south to north “rocche” that are more evident are both located in the high Bormida valley and Clavesana, Farigliano, Cherasco and Barbaresco.

Otherwise, Roero is crossed by a unique system of “rocche”, geologically indicated as “Orlo di Terrazzo”. In these dry and poor of nutrients terrains, that are exposed to temperature ranges and wind action, live species adapted to the environment, such as Broom (Spartium junceum), Heather (Calluna vulgaris) and Thyme (Thymus vulgaris).

CASTLE WALLS

A very singular environment is the one of Roero Castle Walls (Sommariva Perno, Pocapaglia, Santa Vittoria, Govone, Cisterna d’Asti, etc), that hold considerable colony of Caper bushes (Capparis spinosa) and Sea fennel (Crithmum maritimum).

 

PS24e. Langhe and Tanaro left side

One of the main museum wealthes is its herbarium. The exsiccata collection reaches up to 11,000 samples that represent 1,515 species. The gathered, prepared, conserved and identified material is the result of research activity that has been coordinated by the researcher as natural continuation of collecting activity and past botanic studies: Carlo Bertero (1789-1831), Teodoro Ferraris (1871-1943) and Ferdinando Vignolo-Lutati (1878-1965).

The relevance of the collection is proved by the inclusion of the museum between locations that have been registered in the New York “Index erbariorum”, under the tag  “ALB”.

Langhe and Roero herbarium proves the fact that Alba territory is one of the most studied under the floral area in Italy and highlights the unique features of the territory: more than 1,500 species, i.e. over 27% of italian identified species, live in only 1,400 kms, i.e. less than 0.5% of the whole national landscape.

 

Old tree tell story: Dendochronology

 

DENDROCHRONOLOGY (from greek “dendron”= tree, “kronos”= time, “logos”= tale) is the science that studies the arboreal plants growth over time, its modalities and key factors.

The thickness of every single ring depends on:

  • Biological factors (species, age, possible diseases,…)
  • Geographical factors (soil, exposition, elevation, side slope,…)
  • Climatic factors (temperature, dampness, precipitations,…)

All these factors are recorded in the plant annular sequence, giving each ring a particular feature (density, colour, zonationes) and make dendrochronology an absolute and highly precise dating method.

The study of growth rings allows to know not only age and wealth of the plant, but also its developmental climate and environment conditions.

Dendrochronolgy is used in many research fields, from climatology to ecology as well as geomorphology, atmospheric pollution problems, archaeology, art history, architecture.

  • ↑ Civic Museum of Archaeology and Natural Sciences “Federico Eusebio”, Alba
  • P1. The founder of the museum: Federico Eusebio
  • P2 GIOVANNI BATTISTA TRAVERSO. THE BIRTH OF THE PREHISTORICAL RESEARCHES IN ALBA
  • P3 GIUSEPPE GALLIZIO. THE PASSION TO SERVE THE SCIENCE
  • P4 THE DIDIUS VICARIUS’ STELE
  • P5 THE RIVERS TANARO AND CHERASCA. GEOLOGY AND GEO-MORPHOLOGY OF THE TERRITORY
  • P7 The stream Cherasca and its geological environment
  • P8 The river Tanaro and its geological environment
  • P9 The right bank of the river Tanaro from Neolithic to Iron age
  • P10 From the forests to the fields. The development of the Neolithic economy.
  • P11 The booming of the Neolithic economy.
  • PS0 Palm tree leaves fossil track (Sabal major Ung.)
  • P12 The quest for the Greenstone
  • P13 The floor of an Early Neolithic dwelling
  • P13B Living in Alba
  • P14 The ancestors’ house
  • P15 The tomb of the warrior
  • P16 The Bronze Age. The control of the territory and of the river communication routes
  • P17 The cremation necropolis in Piave Street
  • P18 The cults and the funerary rites
  • P19 The Intermediate Bronze Age tomb from Piave Road 199
  • P20 The funerals: the inhumation tomb of the Bronze Age
  • P21 Sailers and farmers in the Intermediate-Late Bronze Age
  • P22 Metallurgy of Bronze and itinerant artisans
  • P24 In the Bagienni’s territory
  • P25 Shepherds and mercenaries: the economy of the Late Iron Age
  • P26 The Roman sewers and the medieval tower
  • P27 The hypogean tomb
  • P27b The monumental marble gravestone
  • P28 The Peutinger’s Tabula
  • P29 The Romanization
  • P30 The territory of Alba
  • P31 The archaeological map of the territory
  • P32 General planimetry of the town superimposed upon the current historical city centre
  • P33 The urban layout plan of Alba Pompeia
  • P34 The brick stamps
  • P34B ACROLITO
  • P35 The forum and the public buildings
  • P36 The theatre
  • Black board 2, theatre room
  • Marble base
  • P36b The garnished cornice
  • P36c The rosette
  • P37 The cults
  • P38 The domus of the social theatre
  • P39 The houses
  • P40 The domus in Cerrato road
  • P41 The domus in Acqui Street
  • P42 The Hercules’myth
  • P43 Common artifacts
  • P44 The numismatic collection
  • P45 The roman coinage: repubblican and augustan series
  • P47 The canteen, the kitchen and the warehouse
  • P48 The amphorae and the millstones
  • EP2. BLACK BOARD 2, THEATRE ROOM. INSCRIPTIONS.
  • P49 The funerary rites
  • EP8. INSCRIPTIONS
  • P50 The necropolis
  • EP8bis. INSCRIPTIONS
  • P50B The gold ribbon
  • EP10bis. INSCRIPTIONS
  • P50C The cross tomb + tomb 1
  • EP10. INSCRIPTIONS
  • Black board 8b
  • EP11. INSCRIPTIONS
  • EP12. INSCRIPTIONS
  • P23 The sword from the river
  • EP13. INSCRIPTIONS
  • P46 The Roman currency: Imperial series
  • S10.INSCRIPTIONS ON MARBLE SLAB
  • P51 The funeral stelae
  • S17.
  • P52 The citizens of Alba Pompeia
  • S11.
  • PS1 General Paleontology
  • Underground Alba: a journey to the center of the city
  • PS2 Geological eras
  • PS3 “Langhe” and “Roero” Geology
  • PS4 a.Oligocene (from 36 to 23 M.A.) b. Miocene (from 23 to 5.3 mya)
  • PS5 Messiniamo (Upper Miocene, 7.2-5.3 mya)
  • PS6. Pliocene (from 5.3 to 1.8 mya)
  • PS7. Piedmont Pliocene fossil shells
  • PS8-9. Cuneo Alps minerals
  • PS10. Fluorescent minerals
  • PS11 Animals evolution
  • PS12 Invertebrates
  • PS13-16 Insects
  • PS17 Lower vertebrates
  • PS18 Birds
  • PS19 Mammals
  • PS20 Plants evolution
  • PS21 Fungi
  • PS22 Cormophyte
  • PS23 Alba territory trees
  • PS24 Alba territory vegetation

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