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Lieu-dit · Cersot

Le Clos Renard

Le Clos Renard is a lieu-dit in Cersot, Côte Chalonnaise, Burgundy, whose largest tier is regional.

32.0 ha

delimited

368 m

elevation

10.7 h

sun at harvest

Open on the mapWith the boundary, the plots, the sun through the year and the bedrock.

In figures

LevelRegionalinao-aoc-viticoles-bulk (c. 4 September 2026)
VillageCersot
RegionCôte Chalonnaise, Burgundy
Delimited32.0 hainao-aoc-viticoles-bulk (c. 4 September 2026) · cadastre-etalab (4 September 2026)
Planted1.89 hacadastre-etalab (4 September 2026) · ign-bdtopo-vigne (5 September 2026) · ign-rpg-2024 (5 September 2026)
Parcels19
Grape varietypinot noir, gamay, césar also permitted: aligoté, chardonnay, gamay de bouze, gamay de chaudenay, melon, pinot blanc, pinot grisinao-cahiers-des-charges (7 September 2026) · dgddi-superficies-produits (7 September 2026) · franceagrimer-observatoire-viticulture (not in this commune)
Organic0%agence-bio-cartobio (c. 5 September 2026) · agence-bio-operateurs (5 September 2026)

Place in the village

Among all 13 named plots of Cersot, from high to low:

sun at harvest 11th
elevation 3rd
slope 4th
on the slope 4th

Position

368 m

elevation

10.3%

firm

SE

southeast

upper

concave fold

Elevation368 m 338 to 389 mign-rge-alti (5 September 2026)
Daytime temperature±0.00 °C not measurable: smaller than the uncertainty. by day, relative to the village centre at 368 m, ± 0.03 °Cmeteo-france-quotidiennes (18 September 2026) · meteo-france-postes (6 September 2026) · meteo-france-lsh (6 September 2026) · ign-rge-alti (5 September 2026)
Slope10.3% 5.9°ign-rge-alti (5 September 2026)
Aspectsoutheast 143°ign-rge-alti (5 September 2026)
On the slope49% upper slope, in a concave hollow, 169 m drains onto itign-rge-alti (5 September 2026)

Bedrock

youngold
  • 23%Oxfordian marl with iron oolites 159.5–⁠157 million years
  • 6%Argovien marl and marly limestone 159.5–⁠157.5 million years
  • 21%Marl and limestone, upper Callovian about 164–⁠161 million years
  • 26%Oolitic limestone, marl and chailles (late Bathonian to Callovian) 165.5–⁠161.5 million years
  • 22%Massive Bathonian limestone, dolomitic top 166.5–⁠165.3 million years
  • 3%Bathonian oolite and fine-grained limestone 168–⁠166 million years

Not a borehole: ordered by age, thickness by share of surface.

In the glass. Plots where the decalcified clay with chailles dominates are often described as fresher and firmer. This is an observation from practice, probably via the lower pH and the stony top layer, not a measured relationship. (weak indication)

A mixed sequence of oolitic limestone, marl bands and chailles, siliceous nodules that grew in the lime mud during hardening. Chailles resemble flint but are less pure and more porous, with more lime in the siliceous mass. Where the limestone has dissolved at the surface, a decalcified clay remains in which the insoluble chailles lie loose; about 165.5 to 161.5 million years old.

For the vine. Mixed behaviour: the oolite drains readily, the marl bands retain water and the chailles form a stony, fast-warming top layer. Where the decalcified clay with chailles dominates, the soil is more acidic and poorer in active lime, which lowers the chlorosis risk. Rooting depth varies greatly over a few metres, depending on where a marl band lies.

Occurs on the plateaus and upper slopes of the Côte and in the Hautes-Côtes, where the decalcified clay with chailles lies at the surface.

BRGM geological map at 1:50,000. It tells vineyards apart, not plots within a vineyard. The link between rock and taste is indirect: soil depth, water and warmth do the work, and slope, vine age and the cellar do the rest. Units on that map: j3c-4, j5a, j3c, j4b, j5b, j3a.

brgm-bdcharm50 (4 September 2026)

Sun and horizon

07:42

above the hill

18:25

behind the hill

10.7 h

sun at harvest

1.2 h

lost to the hill

Grey: sun up, behind the hill or its own slope.

Around harvest the sun rises here at 07:42 above the hill and disappears at 18:25 behind the hill: 10.7 hours of direct sun on a clear day. The ridge reaches 13.8° above the horizon to the west. The relief costs 0.5% of the irradiation from April to October, direct and diffuse together.

Irradiation+1.6% versus flat land 1,074 kWh/m² from April to October, 42% of it diffuseunder the average cloudiness of 2005 to 2023 (PVGIS-SARAH3, EU JRC); direct, diffuse and reflected light togetherign-rge-alti (5 September 2026) · ign-lidarhd-mnh (6 September 2026) · ign-bdforet-v2 (5 September 2026) · jrc-pvgis-sarah3 (10 September 2026)
Open sky98.9% of the sky the slope itself sees; the surrounding relief blocks the restign-rge-alti (5 September 2026) · ign-lidarhd-mnh (6 September 2026) · ign-bdforet-v2 (5 September 2026)
Three reference days, the caveat
risesetsunday
21 June06:0420:0614.0 h15.9 h
20 September07:4218:2510.7 h12.3 h
21 December08:4015:507.2 h8.5 h

Computed from the IGN elevation model at 5 m: horizon in 36 directions up to six kilometres, sun position per minute, angle of incidence on the mean slope. Clear sky, with the tree canopy from the IGN forest inventory as a raised horizon (15 m closed forest, 5 m heath, trees within 60 m ignored), 24% of the far field is forest (BD Forêt), no buildings.

The irradiation loss does include clouds: the average of 2005 to 2023 (PVGIS-SARAH3, EU JRC), not any particular year.

ign-rge-alti (5 September 2026) · ign-lidarhd-mnh (6 September 2026) · ign-bdforet-v2 (5 September 2026)

Air and cold

31 m

above the lowest point

drains far away

cold air

a combe

23.7 ha flows past

Cold air31 m high on the slope, cold air drains far awayign-rge-alti (5 September 2026)
Cold air passing through23.7 ha a combe, mean over the polygon 0.40 haign-rge-alti (5 September 2026)

Planting

ESE-WNW

diagonal to the slope

1.10 m

between the rows

96%

vineyard in 1950

RowsESE-WNW (103°) diagonal to the slope (40°), every 1.10 m, all rows parallelmeasured over 1.9 of 1.9 ha plantedign-bdortho (5 September 2026)
Vineyard in 195096% abandoned since: 6.58 ha, rows then ran 82° differentlyassessed over 9.2 ha on the 1950-1965 aerial photographign-photos-historiques-1950-1965 (6 September 2026)

Climate over time

196019802000202012°14°16°18°

station MT-ST-VINCENT, 601 m, 14.7 km away

growing season, April to October: 1951-1980: 13.5 °C, 1991-2020: 15.1 °C

Huglin index: 1951-1980: 1,248, 1991-2020: 1,553

last spring frost: 1951-1980: day 107, 1991-2020: day 101

series homogenised through 2022

The name

clos
an enclosed plot, walled or hedged. In Burgundy the wall often carries a monastic or seigneurial past; clou and cloux are the same root in diminutive form. Ownership and saints · Association des Climats du vignoble de Bourgogne, Les noms des Climats (2026)
renard
fox. Animals · Gérard Taverdet, Noms de lieux de Bourgogne (2007)

This is about the words, not about this plot: the same name can have arisen differently elsewhere.

Who owns land here

No parcel here is registered to a legal entity. In France only those owners are public; parcels of private individuals are not.

Where each figure comes from

Classification
The INAO delimitation per denomination, cut against the cadastral parcel. Only the INAO's own plans are legally binding; this map is informational.
Area
Computed on the sphere from longitude and latitude (turf.area), not in Lambert-93. For an appellation this is the union of the INAO polygons across commune boundaries, measured on the unclosed geometry; the fifteen metres used to close the outline for the map are not counted. For a climat it is the union of the cadastral lieu-dit polygons with that name.
Planted
Parcel area times vineyard cover, where cover comes from the IGN vegetation layer supplemented by the agricultural declaration. Checked against the customs harvest declarations: median deviation 5.1 per cent over a hundred appellations.
Elevation
Mean of the elevation-model cells whose centre falls inside the polygon, on a 5 m grid.
Slope
Per-cell slope from the elevation model using Horn's method, then averaged over the cells in the polygon.
Aspect
Vector mean of the per-cell aspect. A plain average would turn north-east and north-west into south.
Sun at harvest
Hours of direct sun on 20 September under a clear sky, with the horizon in 36 directions out to six kilometres and the height of woods and buildings on top of it. Canopy height is measured where LiDAR HD covers the area and estimated from BD Forêt where it does not; the panel states which of the two was used.
Grape variety by appellation
Per appellation and colour the permitted varieties from the approved cahier des charges; per appellation and tier the declared hectares of white and red from the customs harvest declaration (product codes). One colour permitted: the main variety of that colour. Two colours: from 85 percent of the hectares that colour applies, in between it is called mixed. Champagne: the dominant variety from the planted hectares per variety per commune from FranceAgriMer. Per polygon the dominant variety of its parts by area. Derived, not measured: the variety per plot exists only in the customs vineyard register, which is not public. In a two-colour appellation a single plot may carry the other variety. Customs withhold small appellations (statistical secrecy), in which case the split is missing.
Bedrock
The geological unit covering the largest share of the polygon, from the 1:50,000 geological map. At 1:50,000 the map separates one climat from another, but not what varies inside a climat.
Organic
Share of the area certified organic or in conversion, from the CartoBio plot register.