Abstract:Abstract. Two new 14C-dated Holocene pollen profiles from Marais des Baux, Bouches-du-Rh6ne, France, are presented. The record begins in the Younger Dryas, when the vegetation consisted mainly of grasses and mugwort (Artemisia). The Preboreal was marked by a transitory expansion of pine forests and was followed by the establishment of a rich deciduous oak-forest that included hazel (Corylus) and elm (Ulmus). During the Boreal, hazel played a dominant role within the oak-forest. The oak forests, which included … Show more
“…Moreover, previous pollen investigations in the Apennines (Lowe 1992) and other Mediterranean regions, e.g. Provence, France (Andrieu‐Ponel et al . 2000), indicate that the distribution Abies alba during the early Holocene was much wider than today.…”
Summary1 A Holocene sedimentary sequence from a coastal lake in the Mediterranean area (Lago di Massaciuccoli, Tuscany, Italy, 0 m a.s.l.) was sampled for pollen and microscopic charcoal analyses. Contiguous 1-cm samples represent an estimated time interval of c. 13 years, thus providing a high-resolution sequence from 6100 to 5400 cal. years . 2 Just before 6000 cal. years , sub-Mediterranean and Mediterranean forests were present together with fir ( Abies alba ), a submontane species that is today absent at low altitudes in the Mediterranean. A sharp vegetational change occurred after 6000 cal. years involving a drastic decline of Abies alba around the site. 3 Time-series analyses suggest that increased fire activity at this time caused a strong decline in Abies alba , a highly fire-sensitive species. During 100 years of higher fire incidence, diverse (predominantly evergreen) forest communities were converted to low-diversity fire-prone shrub communities. 4 Cross-correlations reveal that fire during the mid-Holocene hindered the expansion of holm oak ( Quercus ilex ), the most common tree species today in Mediterranean environments. While the factors that triggered the Holocene expansion of this species in the Mediterranean area are unclear, our results do not support the hypothesis that fire was key for holm oak expansion. 5 Diatom analyses of the same sediment core provide an independent palaeoenvironmental proxy for palaeoclimatic reconstruction. A change in the eutrophy and salinity of the lake occurred just before 6000 cal. years , suggesting that a climatic shift towards aridity may have triggered the observed change in hydrology and possibly also in fire regime. 6 Over the millennia fire has decisively contributed to the establishment of the present fire-adapted vegetation type (macchia). Native fire-sensitive species were displaced or repressed, and arboreal vegetation became less diverse. Combined ecological and palaeoecological data may help to assess possible future scenarios of biosphere responses to global change. Our results imply that the forecasted global warming and fire increase may trigger irrecoverable biodiversity losses and shifts in vegetational composition within a few decades or centuries at most. In particular, fire and droughtsensitive vegetation types, such as the relict forests of Abies alba in the Apennines, seem particularly threatened by large-scale displacement.
“…Moreover, previous pollen investigations in the Apennines (Lowe 1992) and other Mediterranean regions, e.g. Provence, France (Andrieu‐Ponel et al . 2000), indicate that the distribution Abies alba during the early Holocene was much wider than today.…”
Summary1 A Holocene sedimentary sequence from a coastal lake in the Mediterranean area (Lago di Massaciuccoli, Tuscany, Italy, 0 m a.s.l.) was sampled for pollen and microscopic charcoal analyses. Contiguous 1-cm samples represent an estimated time interval of c. 13 years, thus providing a high-resolution sequence from 6100 to 5400 cal. years . 2 Just before 6000 cal. years , sub-Mediterranean and Mediterranean forests were present together with fir ( Abies alba ), a submontane species that is today absent at low altitudes in the Mediterranean. A sharp vegetational change occurred after 6000 cal. years involving a drastic decline of Abies alba around the site. 3 Time-series analyses suggest that increased fire activity at this time caused a strong decline in Abies alba , a highly fire-sensitive species. During 100 years of higher fire incidence, diverse (predominantly evergreen) forest communities were converted to low-diversity fire-prone shrub communities. 4 Cross-correlations reveal that fire during the mid-Holocene hindered the expansion of holm oak ( Quercus ilex ), the most common tree species today in Mediterranean environments. While the factors that triggered the Holocene expansion of this species in the Mediterranean area are unclear, our results do not support the hypothesis that fire was key for holm oak expansion. 5 Diatom analyses of the same sediment core provide an independent palaeoenvironmental proxy for palaeoclimatic reconstruction. A change in the eutrophy and salinity of the lake occurred just before 6000 cal. years , suggesting that a climatic shift towards aridity may have triggered the observed change in hydrology and possibly also in fire regime. 6 Over the millennia fire has decisively contributed to the establishment of the present fire-adapted vegetation type (macchia). Native fire-sensitive species were displaced or repressed, and arboreal vegetation became less diverse. Combined ecological and palaeoecological data may help to assess possible future scenarios of biosphere responses to global change. Our results imply that the forecasted global warming and fire increase may trigger irrecoverable biodiversity losses and shifts in vegetational composition within a few decades or centuries at most. In particular, fire and droughtsensitive vegetation types, such as the relict forests of Abies alba in the Apennines, seem particularly threatened by large-scale displacement.
“…The decrease in this pollen percentage in the subsequent periods at nearby sites (Ruas 1996;Andrieu-Ponel et al 2000;Arobba et al 2004) could be due to the colder temperatures of the Little Medieval Ice Age. Olive cultivation, which has been documented in Liguria and Provence in the 12th to 13th centuries corresponds to the Medieval optimum and to ameliorated agronomical and selective techniques (Quaini 1973;Durand and Leveau 2004).…”
The results of an analysis on plant remains (fruit, seeds, pollen and wood) found in sediments in a Roman well in Vada Sabatia (Vado Ligure, Liguria, Italy), dated between the first and fourth centuries AD are presented. The remains are well preserved and constitute an exceptional record of the Ligurian area. Five layers have been recognised: three corresponding to the well when in use and two to the well when it was no longer in use. The vegetational cover of the area has been found to be similar to that observed in the coastal plain near Albingaunum (Albenga) pertaining to the same period. Moreover, the two superficial layers have cumulated a large amount of macroremains related to the period in which the well was no longer in use. The principal tree and vegetable crops and cereals of the coastal plain were present, due to the influence of maritime and mercantile trade, as were the prevailing ruderal and weed species and the tree cover. The presence of carpological remains of Castanea sativa, Secale cereale, Beta vulgaris and Cucumis sativus is reported for the first time in the Roman Age in Liguria. The influence of the arrival of the Romans can be seen from new crops, such as Prunus persica, and the introduction of exotic fruit like Phoenix dactylifera and Ziziphus jujuba. Several wooden artefacts, for example, a rack for drying lucerne and a tool handle, made of Cornus or Viburnum and Viburnum cf. lantana respectively, have been found. The well has proved to be an ideal location for the preservation of plant remains compared with other studied archaeological situations in Liguria and in Southern France, as it presents a higher variety of cultivated fruits, vegetables and cereals.
“…The closest from Cazan were sampled at 25/30 km from the site on both bank of the Durance river and date back to the end of the 1970's (Triat-Laval, 1978). More recently, two well-dated pollen cores were studied in the Marais des Baux (Andrieu-Ponel et al, 2000), around 30 km west from the site, in an area quite similar, edaphically and botanically speaking. In Triat-Laval's study, the Ericaceae -not identified to the genus level -show a subcontinuous curve (but never exceed 5% of the identified pollen grains) since the end of the Boreal at Beauchamp-Pani eres and Moll eges and appear sporadically at Les Autures but are not recorded at L'Isle-sur-la-Sorgue.…”
Cazan-Le clos du Moulin" is an open-air Middle Neolithic site located in the South of France near the village of Vern egues. The excavation of this site has, for the first time in the area, allowed us to reconstruct up to a dozen domestic buildings from the late Chassey culture (4100-3800 BCE), arranged around an area occupied by heated stone combustion structures. Because of the partial erosion of the archaeological horizons, artefacts and ecofacts related to the Neolithic occupation were only found in the fills of structures. Charcoal analysis was carried out on samples from the postholes, the heated-stone hearths and a well. The anthracological results show a selection of natural resources depending on the use of the wood: timber or fuel. The size required for the posts can restrict the scope of the species suitable for timber: oak seems to be preferred for that purpose. On the contrary, the choice of fuel wood seems to be less constrained by technical limitations. Nevertheless, one particular species, Arbutus unedo, accounts for the bulk of the wood gathered for fuel supply, however it was certainly not the only woody resource available during the Middle Neolithic. Overall, charcoal analysis at Cazan-Le Clos du Moulin shows that wood harvesting-as recorded in the fills of structures-is selective. This selection could be imposed by purely technical requirements that we can only partly perceive or by cultural necessity which remains beyond our understanding, but, beyond this, the choices are probably guided by land and vegetation resource management in order to permit the coexistence of various wood-consuming activities in a single territory and to favor the exploitation of easily accessible fuel.
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