Late Pleistocene Vegetation and Climate Near Melaleuca Inlet, South-Western Tasmania

1991 ◽  
Vol 39 (4) ◽  
pp. 315 ◽  
Author(s):  
GJ Jordan ◽  
RJ Carpenter ◽  
RS Hill
Keyword(s):  
Species Composition ◽  
Late Pleistocene ◽  
Fire Frequency ◽  
Present Species ◽  
Human Occupation ◽  
Sclerophyll Forest ◽  
Minimum Age ◽  
Heath Communities ◽  
Vegetation And Climate ◽  
Pleistocene Deposit

Macrofossils of 27 taxa and microfossils of 47 taxa are identified from a Late Pleistocene deposit at Melaleuca Inlet with a minimum age of 38 800 years. Interpretation of the fossil assemblage suggests that at the time of deposition the climate was cooler than at present and at least as wet. The local vegetation was dominated by wet scrub and sedgeland-heath communities with rainforest and wet sclerophyll forest also present. Species composition was similar to extant vegetation in the region but now-extinct species and possibly communities were present. Charcoal occurs in the sediments and the taxonomic make-up of the assemblage is consistent with the presence of a well established high fire frequency, despite the deposit pre-dating the earliest known human occupation of Tasmania.

Paleoecological and archaeological implications of a Late Pleistocene/Early Holocene record of vegetation and climate from the Pacific coastal plain of Panama

2003 ◽  
Vol 59 (1) ◽  
pp. 79-87 ◽  
Author(s):  
Dolores R. Piperno ◽  
John G. Jones
Keyword(s):  
Tropical Forest ◽  
Late Pleistocene ◽  
Coastal Plain ◽  
Deciduous Forest ◽  
Early Holocene ◽  
Tropical Deciduous Forest ◽  
Human Occupation ◽  
Core Sediment ◽  
The Pacific ◽  
Holocene Record

AbstractA phytolith record from Monte Oscuro, a crater lake located 10 m above sea level on the Pacific coastal plain of Panama, shows that during the Late Pleistocene the lake bed was dry and savanna-like vegetation expanded at the expense of tropical deciduous forest, the modern potential vegetation. A significant reduction of precipitation below current levels was almost certainly required to effect the changes observed. Core sediment characteristics indicate that permanent inundation of the Monte Oscuro basin with water occurred at about 10,500 14C yr B.P. Pollen and phytolith records show that deciduous tropical forest expanded into the lake’s watershed during the early Holocene. Significant burning of the vegetation and increases of weedy plants at ca. 7500 to 7000 14C yr B.P. indicate disturbance, which most likely resulted from early human occupation of the seasonal tropical forest near Monte Oscuro and the development of slash-and-burn methods of cultivation.

Late Pleistocene Human Occupation In Tasmania: A Reply To Thomas

1994 ◽  
Vol 38 (1) ◽  
pp. 28-35 ◽  
Author(s):  
R. Cosgrove ◽  
J. Allen ◽  
B. Marshall
Keyword(s):  
Late Pleistocene ◽  
Human Occupation

scholarly journals Didelphidae marsupials (Mammalia, Didelphimorphia) from the Late Pleistocene deposit of the Gruta dos Moura Cave, northern Brazil

2015 ◽  
Vol 87 (1) ◽  
pp. 193-208 ◽  
Author(s):  
Patricia Villa Nova ◽  
Leonardo S. Avilla ◽  
Édison V. Oliveira
Keyword(s):  
Late Pleistocene ◽  
Open Environment ◽  
The Past ◽  
Intimate Association ◽  
Actual Environment ◽  
Gallery Forests ◽  
Northern Brazil ◽  
Open Forests ◽  
Didelphis Albiventris ◽  
Pleistocene Deposit

The present study acknowledges the diversity of fossil marsupials from the Gruta dos Moura cave, as well as environmental and climatic aspects during the Quaternary. The results show that this is the largest diversity of Pleistocene marsupials recorded in a single cave: Didelphis albiventris, D. aurita, Gracilinanus agilis, G. microtarsus, Marmosa murina, Monodelphis brevicaudata, M. domesticaand Sairadelphys tocantinensis. Furthermore, the described specimens are also part of the only fossil assemblage unequivocally referable to the late Pleistocene. Paleontological studies suggest an intimate association with dry and open environments with high abundance of water sources. Since most of the identified taxa are characteristic of open forests and gallery forests, this could represent the actual environment around the Gruta dos Moura cave. Recent studies identified sympatric occurrences between species from open and dry environments and species from humid forests that were identified among our material and are characteristic of humid regions. Therefore, these species could inhabit gallery forests and capons, or even ecotones, inside a dry and open environment. Moreover, the extinction of Sairadelphyscould also indicate that the climatic and environmental conditions changed or that the past environment was more heterogeneous than the current environment of the region.

Late Pleistocene - Holocene vegetation and climate from the palaeolake sediments, Rukti valley, Kinnaur, Himachal Himalaya

2018 ◽  
Vol 479 ◽  
pp. 79-89 ◽  
Author(s):  
Parminder S. Ranhotra ◽  
Jyoti Sharma ◽  
Amalava Bhattacharyya ◽  
N. Basavaiah ◽  
Koushik Dutta
Keyword(s):  
Late Pleistocene ◽  
Vegetation And Climate

Re-evaluating the origins of late Pleistocene fire areas on Santa Rosa Island, California, USA

2012 ◽  
Vol 78 (2) ◽  
pp. 353-362 ◽  
Author(s):  
Torben C. Rick ◽  
John S. Wah ◽  
Jon M. Erlandson
Keyword(s):  
Late Pleistocene ◽  
Younger Dryas ◽  
Fire Regimes ◽  
Fire Frequency ◽  
X Ray Diffraction ◽  
X Ray ◽  
Sedimentary Deposits ◽  
Natural Fires ◽  
Human Colonization ◽  
Santa Rosa Island

AbstractAt the close of the Pleistocene, fire regimes in North America changed significantly in response to climate change, megafaunal extinctions, anthropogenic burning and possibly, even an extraterrestrial impact. On California's Channel Islands, researchers have long debated the nature of late Pleistocene “fire areas,” discrete red zones in sedimentary deposits, interpreted by some as prehistoric mammoth-roasting pits created by humans. Further research found no evidence that these red zones were cultural in origin, and two hypotheses were advanced to explain their origin: natural fires and groundwater processes. Radiocarbon dating, X-ray diffraction analysis, and identification of charcoal from six red zones on Santa Rosa Island suggest that the studied features date between ~ 27,500 and 11,400 cal yr BP and resulted from burning or heating, not from groundwater processes. Our results show that fire was a component of late Pleistocene Channel Island ecology prior to and after human colonization of the islands, with no clear evidence for increased fire frequency coincident with Paleoindian settlement, extinction of pygmy mammoths, or a proposed Younger Dryas impact event.

Late Pleistocene and early Holocene rivers and wetlands in the Bonneville basin of western North America

2003 ◽  
Vol 60 (2) ◽  
pp. 200-210 ◽  
Author(s):  
Charles G. Oviatt ◽  
David B. Madsen ◽  
Dave N. Schmitt
Keyword(s):  
Great Basin ◽  
Late Pleistocene ◽  
Theoretical Models ◽  
Coarse Sand ◽  
Early Holocene ◽  
River Channels ◽  
Human Occupation ◽  
Lake Bonneville ◽  
River Bed ◽  
Bonneville Basin

AbstractField investigations at Dugway Proving Ground in western Utah have produced new data on the chronology and human occupation of late Pleistocene and early Holocene lakes, rivers, and wetlands in the Lake Bonneville basin. We have classified paleo-river channels of these ages as “gravel channels” and “sand channels.” Gravel channels are straight to curved, digitate, and have abrupt bulbous ends. They are composed of fine gravel and coarse sand, and are topographically inverted (i.e., they stand higher than the surrounding mudflats). Sand channels are younger and sand filled, with well-developed meander-scroll morphology that is truncated by deflated mudflat surfaces. Gravel channels were formed by a river that originated as overflow from the Sevier basin along the Old River Bed during the late regressive phases of Lake Bonneville (after 12,500 and prior to 11,000 14C yr B.P.). Dated samples from sand channels and associated fluvial overbank and wetland deposits range in age from 11,000 to 8800 14C yr B.P., and are probably related to continued Sevier-basin overflow and to groundwater discharge. Paleoarchaic foragers occupied numerous sites on gravel-channel landforms and adjacent to sand channels in the extensive early Holocene wetland habitats. Reworking of tools and limited toolstone diversity is consistent with theoretical models suggesting Paleoarchaic foragers in the Old River Bed delta were less mobile than elsewhere in the Great Basin.

A Good Place to Live: Plants and People at the Santa Elina Rock Shelter (Central Brazil) from Late Pleistocene to the Holocene

2020 ◽  
Vol 31 (2) ◽  
pp. 273-291
Author(s):  
Rita Scheel-Ybert ◽  
Caroline Bachelet
Keyword(s):  
Late Pleistocene ◽  
Late Holocene ◽  
Vegetation Changes ◽  
Vegetation Types ◽  
Rock Shelter ◽  
Good Place ◽  
Central Brazil ◽  
Cultural Preference ◽  
Vegetation And Climate ◽  
Over Time

The Santa Elina rock shelter (Central Brazil) was recurrently occupied from the Late Pleistocene to the Late Holocene. We compare sets of previously published anthracological analyses with new data to reconstruct the landscape, vegetation, and climate over the several thousand years of occupation, providing information on firewood management from about 27,000 to about 1500 cal BP. Laboratory analyses followed standard anthracological procedures. We identified 34 botanical families and 84 genera in a sample of almost 5,000 charcoal pieces. The Leguminosae family dominates the assemblage, followed by Anacardiaceae, Bignoniaceae, Rubiaceae, Euphorbiaceae, and Sapotaceae. The area surrounding the shelter was forested throughout the studied period. The local landscape was formed, as it is today, by a mosaic of vegetation types that include forest formations and open cerrado. Some regional vegetation changes may have occurred over time. Our data corroborate the practice of opportunistic firewood gathering in all periods of site occupation, despite a possible cultural preference for some taxa. The very long occupation of Santa Elina may be due not only to its attractiveness as a rock shelter but also to the continuously forested vegetation around it. It was a good place to live.

Effects of fire frequency on species composition in a Mediterranean shrubland

Ecoscience ◽  
2008 ◽  
Vol 15 (4) ◽  
pp. 519-528 ◽  
Author(s):  
Albert Vilà-Cabrera ◽  
Sandra Saura-Mas ◽  
Francisco Lloret
Keyword(s):  
Species Composition ◽  
Fire Frequency ◽  
Mediterranean Shrubland

Changes in an Assemblage of Small Birds in the Understorey of Dry Sclerophyll Forest in Southwestern Australia After Fire

1988 ◽  
Vol 15 (3) ◽  
pp. 331 ◽  
Author(s):  
RD Wooller ◽  
MC Calver
Keyword(s):  
Species Composition ◽  
Western Australia ◽  
Southwestern Australia ◽  
Low Intensity ◽  
Sclerophyll Forest

Changes in the numbers and types of small birds caught in mist-nets in the understorey of dry sclerophyll forest in south-western Australia were recorded for three years after a low intensity fire. There were few changes in the species composition of the assemblage but abundances of the 6-8 most numerous and relatively sedentary species were approximately halved. Many marked individuals (22%) were recaptured up to three years after the fire. After the fire, the number of prey taxa recorded from the faeces of birds caught fell from twelve to six, and the birds ate proportionately more ants and fewer beetles. Ants eaten after the fire were smaller than those eaten before it.

scholarly journals A Holocene pollen record of savanna establishment in coastal Amapá

2008 ◽  
Vol 80 (2) ◽  
pp. 341-351 ◽  
Author(s):  
Mauro B. de Toledo ◽  
Mark B. Bush
Keyword(s):  
Vegetation Change ◽  
Human Impacts ◽  
Detrended Correspondence Analysis ◽  
Fire Frequency ◽  
Pollen Record ◽  
Human Occupation ◽  
Sample Distribution ◽  
River Flooding ◽  
History Of ◽  
Tremendous Impact

The main goal of this study was to investigate how climate and human activities may have influenced ecotonal areas of disjoint savannas within Brazilian Amazonia. The fossil pollen and charcoal records of Lake Márcio (Amapá) were used to provide a Holocene palaeoecological history of this region. Detrended correspondence analysis (DCA) was used to enhance the patterns of sample distribution along the sediment core. A marked vegetation change from closed forests with swamp elements to open flooded savanna at c. 5000 yrs BP was evident from the pollen record. Charcoal analysis revealed a pattern of increased accumulation of particles coincident with the establishment of savannas, suggesting higher fire frequency and human impacts near the lake. A 550-year sedimentary hiatus suggests that the lake depended heavily on floodwaters from the Amazon River, and that it became suddenly isolated from it. When sedimentation restarted in the lake, the environment had changed. A combination of factors, such as reduced river flooding, palaeofires and human occupation may have had a tremendous impact on the environment. As there are no other major changes in vegetation, after 4700 yrs BP, it is plausible to assume that the modern mosaic vegetation formed at that time.

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