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[PDF] Top 20 Late Holocene vegetation changes in relation with climate fluctuations and human activity in Languedoc (southern France)

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Late Holocene vegetation changes in relation with climate fluctuations and human activity in Languedoc (southern France)

Late Holocene vegetation changes in relation with climate fluctuations and human activity in Languedoc (southern France)

... that human activity caused forest loss before the 7th century ...the late Holocene aridification and the arid event 1, the increase in deciduous Quercus indicates that climatic conditions in ... See full document

16

Climate and vegetation changes during the Lateglacial and early–middle Holocene at Lake Ledro (southern Alps, Italy)

Climate and vegetation changes during the Lateglacial and early–middle Holocene at Lake Ledro (southern Alps, Italy)

... pollen-based climate reconstructions were coupled with lake level variations and abiotic proxies, such as magnetic susceptibility and elemental variation from the Lake Ledro long core, to reveal the local impacts ... See full document

21

Holocene climate aridification trend and human impact interrupted by millennial- and centennial-scale climate fluctuations from a new sedimentary record from Padul (Sierra Nevada, southern Iberian Peninsula)

Holocene climate aridification trend and human impact interrupted by millennial- and centennial-scale climate fluctuations from a new sedimentary record from Padul (Sierra Nevada, southern Iberian Peninsula)

... detailed climate reconstruction for the last 4700 cal yr BP for the Padul area and the western Mediter- ...between vegetation, atmospheric dynamics, insolation, and solar activity during the ... See full document

21

Pollen-based reconstruction of Holocene vegetation and climate in southern Italy: the case of Lago Trifoglietti

Pollen-based reconstruction of Holocene vegetation and climate in southern Italy: the case of Lago Trifoglietti

... burn activity, were probably too small to modify regional pollen influx at Trifoglietti, and/or that the steep slopes between the site and the sea were unfavourable to ...of human impact and it may offer ... See full document

24

Impact of precession on the climate, vegetation and fire activity in southern Africa during MIS4

Impact of precession on the climate, vegetation and fire activity in southern Africa during MIS4

... fire activity occurring during maxima of the climatic precession index (e sin ω, with e the eccentricity and ω the longitude of the perihelion), when the boreal winter solstice occurs near the ...fire ... See full document

18

Ecology and long-term history of fire in New Zealand

Ecology and long-term history of fire in New Zealand

... Whether ragamuffin communities are quasi-stable or whether they will inevitably move towards either high- flammability exotic-dominated communities or lower flammability native forest is unclear. Many of New Zealand’s ... See full document

20

Late Holocene climate reorganisation and the North American Monsoon

Late Holocene climate reorganisation and the North American Monsoon

... Annual proxy rainfall record of the late Holocene North America Monsoon.. Present day North American Monsoon patterns were established after 3ka BP..[r] ... See full document

21

Effects on New Zealand Vegetation of Late Holocene Erosion and Alluvial Sedimentation

Effects on New Zealand Vegetation of Late Holocene Erosion and Alluvial Sedimentation

... the vegetation when Europeans arrived was linked closely to the alluvial history of the ...to vegetation which has survived essentially unchanged by cultural ...on Late Holocene alluvium in ... See full document

14

Late Weichselian and Holocene palaeoceanography of Storfjordrenna, southern Svalbard

Late Weichselian and Holocene palaeoceanography of Storfjordrenna, southern Svalbard

... The lowermost unit L1 (Fig. 4) was significantly coarser, more compacted and devoid of foraminifera, which indi- cates that it is likely of subglacial origin. During the late Weichselian Glacial Maximum, ... See full document

17

Human impact on the hydroenvironment of Lake Parishan, SW Iran, through the late Holocene

Human impact on the hydroenvironment of Lake Parishan, SW Iran, through the late Holocene

... 2015 Human impact on the hydroenvironment of Lake Parishan, SW Iran, through the late Holocene.. This is the author’s version of a work that was accepted for publication in The Holocene.[r] ... See full document

25

Deglacial and Holocene vegetation and climatic changes in the southern Central Mediterranean from a direct land–sea correlation

Deglacial and Holocene vegetation and climatic changes in the southern Central Mediterranean from a direct land–sea correlation

... from southern Italy where scattered woodlands have been detected (Magri and Sadori, 1999; Allen et ...the vegetation or (2) mainte- nance of some degree of moisture since cedar is generally considered as a ... See full document

21

Multi-decadal atmospheric and marine climate variability in southern Iberia during the mid- to late-Holocene

Multi-decadal atmospheric and marine climate variability in southern Iberia during the mid- to late-Holocene

... Summer temperatures. Reconstructed summer SSTs based on foraminiferal assemblage variations vary around 22.8 ◦ C in the Alboran Sea and around 22.4 and 21.7 ◦ C before and after approximately 4.0 ka cal BP, respectively, ... See full document

18

Strengths and challenges for transient Mid- to Late Holocene simulations with dynamical vegetation

Strengths and challenges for transient Mid- to Late Holocene simulations with dynamical vegetation

... simulated climate and vege- tation characteristics (see Appendix and ...present-day climate (Guimberteau et ...dynamical vegetation is ac- tive. With interactive vegetation, however, ... See full document

28

Late Glacial to Holocene dune development at southern  Krakower See

Late Glacial to Holocene dune development at southern Krakower See

... the southern shore of Krakower See shows the Quaternary geology of the surrounding ...to Holocene environmental changes, including lake-level fluctuations, aeolian dynamics, and pedological processes ... See full document

6

Modelling Weather and Climate Related Fire Risk in Africa

Modelling Weather and Climate Related Fire Risk in Africa

... how changes in climate and vegetation impact the risk of fire in Africa (vulner- ability of a region to fire ...investigate climate and vegetation factors which may induce wildfire, is ... See full document

16

The history of the vegetation and climate in southern Tasmania since the late Pleistocene (ca  13  000   0 BP

The history of the vegetation and climate in southern Tasmania since the late Pleistocene (ca 13 000 0 BP

... wash residues with distilled water, centrifuge and decant at this point, heat water bath on hotplate to ca.. distilled water to residue, "Whirlimix" and pour su,Ipension.[r] ... See full document

58

The history of the vegetation and climate in southern Tasmania since the late Pleistocene (ca  13  000   0 BP

The history of the vegetation and climate in southern Tasmania since the late Pleistocene (ca 13 000 0 BP

... Given the well—defined climatic gradients across Tasmania and differences in the area of vegetation represented by different pollen assemblages, it is prima facie improbable that pollen [r] ... See full document

306

The history of the vegetation and climate in southern Tasmania since the late Pleistocene (ca  13  000   0 BP

The history of the vegetation and climate in southern Tasmania since the late Pleistocene (ca 13 000 0 BP

... TO enable as objective an interpretation as possible of this fossil pollen data, the present-day pollen rains across Tasmania were studied via surface sampling and pollen trapping progra[r] ... See full document

211

Influence of orbital forcing and solar activity on water isotopes in precipitation during the mid- and late Holocene

Influence of orbital forcing and solar activity on water isotopes in precipitation during the mid- and late Holocene

... winter climate in Central Eu- rope center around ...and late Holocene, the δ 18 O signal of BU4 seems not to be clearly dominated by the orbital forcing (typically expressed as a change in incoming ... See full document

14

Mid-Tertiary paleoenvironments in Thailand: pollen evidence

Mid-Tertiary paleoenvironments in Thailand: pollen evidence

... from Late Oligocene and Miocene fossil sites of ...jor climate reorganization that brought warmer and wetter conditions over Southeast Asia around 22 ...flect climate variations linked to insolation ... See full document

13

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