Bas Van Geel
Dados Biográficos
| ID | 1244058 |
|---|---|
| NOME | Bas Van Geel |
| PRENOMES | Bas |
| SOBRENOME | Van Geel |
| ASSINATURA | VAN GEEL B |
| AFILIAÇÕES | University of Amsterdam |
| ORCID | 0000-0003-4432-320X |
| VERIFICADO | Sim |
| TOTAL DE OBRAS | 58 |
| TOTAL DE CITAÇÕES | 439 |
| TOTAL COMO AUTOR | 58 |
| TOTAL COMO EDITOR | 0 |
| PRIMEIRO ANO DE PUBLICAÇÃO | 1978 |
| ANO MAIS RECENTE DE PUBLICAÇÃO | 2025 |
| ÍNDICE H | 10 |
Commercial late medieval bog peat exploitation in the Low Countries
The ‘Monnikenven’ is a former, isolated peat bog in the Pleistocene sand landscape near Hilversum (Central Netherlands), During works aiming at restoration of the original mire, a very regular pattern of peat extraction pits was discovered, covering the whole former bog. The pits were separated by vertical, sharply cut, narrow in situ walls, composed of residual bog deposits. Datings by Optical Stimulated Luminescence analysis (osl) of pit fills …
On the Use of Spores of Coprophilous Fungi Preserved in Sediments to Indicate Past Herbivore Presence
Fungal spores that grew on the faeces of herbivores in the past can be extracted from sediments and used to identify the presence of herbivores in former ecosystems. This review: (i) examines the factors that should be considered when interpreting these fungal spores, (ii) assesses the degree to which they can be used to estimate past herbivore populations and biomass density change, and (iii) identifies gaps in our current understanding that lim…
The origin of alkaline fen in the Mosbeek Valley in the Netherlands is due to human impact rather than a natural development
Alkaline fens are important Natura 2000 habitats, which harbor many endangered plant species. Alkaline fens are formed in areas with groundwater discharge and usually developed in a natural way in the early Holocene. We radiocarbon dated the base of three peat deposits from spring fens along the flanks of the ice-pushed ridge near the village of Ootmarsum to find out when and why peat-forming vegetation started to grow. We cored a sequence in the…
NPP-Id
Non-pollen palynomorphs (NPPs) form a large group of biological objects found in palynological slides besides pollen grains. This includes various remains of algae and fungi, shells, resting stages and eggs of invertebrates, among others. Publications of NPP-types started in the 1970s with studies of BvG and colleagues, and large numbers of new types continue to be published every year. For an overview of this diverse world of “extra fossils”, we…
Multicore Study of Upper Holocene Mire Development in West-Frisia, Northern Netherlands
We studied twelve late Holocene organic deposits in West-Frisia, The Netherlands. Pollen, spores, non-pollen palynomorphs, mosses, other botanical macrofossils and insect remains were recorded for reconstructions of changing environmental conditions. Eastern West-Frisia was a cultivated landscape during the Bronze Age, but it became a freshwater wetland in the Late Bronze Age. In most of our sites, radiocarbon dates show that time transgressive i…
Evidence for the diet and habitat of two late Pleistocene mastodons from the Midwest, USA
We analyzed intestinal contents of two late-glacial mastodons preserved in lake sediments in Ohio (Burning Tree mastodon) and Michigan (Heisler mastodon). A multi-proxy suite of macrofossils and microfossils provided unique insights into what these individuals had eaten just before they died and added significantly to knowledge of mastodon diets. We reconstructed the mastodons’ habitats with similar multi-proxy analyses of the embedding lake sedi…
Typha as a wetland food resource
A multidisciplinary study of a Late Pleistocene arctic ground squirrel ( Urocitellus parryii ) midden from Yukon, Canada
Middens (nests and caches) of Late Pleistocene arctic ground squirrels ( Urocitellus parryii ) that are preserved in the permafrost of Beringia archive valuable paleoecological data. Arctic ground squirrels selectively include the plant material placed in middens. To account for this selectivity bias, we used a multi-proxy approach that includes ancient DNA (aDNA) and macro- and microfossil analyses. Here, we provide insight into Pleistocene vege…
Columbus’ environmental impact in the New World
Columbus' arrival in the New World in AD 1492 on the northern coast of Hispaniola was followed by a suite of changes in land-use. We reconstruct environmental change from a 225-cm-long sediment core from site Los Indios from an abandoned and sediment-filled meander of the Yaque River, Cibao Valley, northeastern Dominican Republic. The sediment record starts ca. AD 195 (ca. 1755 cal. yr BP) and the history of the meander infill was monitored by ch…
Columbus' footprint in Hispaniola
Centennial-scale lake-level lowstand at Lake Uddelermeer (The Netherlands) indicates changes in moisture source region prior to the 2.8-kyr event
The Uddelermeer is a unique lake for The Netherlands, containing a sediment record that continuously registered environmental and climatic change from the late Pleistocene on to the present. A 15.6-m-long sediment record was retrieved from the deepest part of the sedimentary basin and an age–depth model was developed using radiocarbon dating, 210 Pb dating, and Bayesian modeling. Lake-level change was reconstructed using a novel combination of hi…
Raised bed agriculture in northwest Europe triggered by climatic change around 850 BC
A sudden decline of solar activity around 850 calendar years BC caused a shift to a cool and wet climate in northwest Europe. Food production suddenly became problematic because of shorter, wetter growing seasons and increased night frost. This climate change triggered innovation and the development of a new agricultural system in continental northwestern Europe: arable farming on raised beds (Celtic field banks) laid out in a more or less checke…
Pollen‐based quantitative reconstructions of Holocene regional vegetation cover (plant‐functional types and land‐cover types) in Europe suitable for climate modelling
We present quantitative reconstructions of regional vegetation cover in north‐western Europe, western Europe north of the Alps, and eastern Europe for five time windows in the Holocene [around 6k, 3k, 0.5k, 0.2k, and 0.05k calendar years before present ( bp )] at a 1° × 1° spatial scale with the objective of producing vegetation descriptions suitable for climate modelling. The REVEALS model was applied on 636 pollen records from lakes and bogs to…
Analysis of coprolites from the extinct mountain goat Myotragus balearicus
Humans colonized the Balearic Islands 5–4 ka ago. They arrived in a uniquely adapted ecosystem with the Balearic mountain goat Myotragus balearicus (Bovidae, Antilopinae, Caprini) as the only large mammal. This mammal went extinct rapidly after human arrival. Several hypotheses have been proposed to explain the extinction of M. balearicus . For the present study ancient DNA analysis (Sanger sequencing, Roche-454, Ion Torrent), and pollen and macr…
Non-pollen palynomorphs show human- and livestock-induced eutrophication of Lake Nussbaumersee (Thurgau, Switzerland) since Neolithic times (3840 bc )
Lake Nussbaumersee, located SW of Lake Constance (Switzerland/Germany), was studied at high temporal resolution for non-pollen palynomorphs (NPPs) within a calcareous gyttja sediment core from the deepest part of the lake. At the Nussbaumersee lakeshore, three pile-dwelling settlements have been excavated and dendrochronologically dated (to the Neolithic, 3840–3695 bc; late Early Bronze Age, 1580–1538 bc; and Late Bronze Age, 850–780 bc). The NPP…
A database and synthesis of northern peatland soil properties and Holocene carbon and nitrogen accumulation
Here, we present results from the most comprehensive compilation of Holocene peat soil properties with associated carbon and nitrogen accumulation rates for northern peatlands. Our database consists of 268 peat cores from 215 sites located north of 45°N. It encompasses regions within which peat carbon data have only recently become available, such as the West Siberia Lowlands, the Hudson Bay Lowlands, Kamchatka in Far East Russia, and the Tibetan…
Bog burst in the eastern Netherlands triggered by the 2.8 kyr BP climate event
The nature and cause of the so-called 2.8 kyr BP event have been a subject of much debate. Peat sequences have provided much of the evidence for this event, but the process link between climate and peatland response is not well understood. Multiproxy, high-resolution analysis of a core from Bargerveen in the eastern Netherlands based on pollen, non-pollen palynomorphs, testate amoebae and geochemistry identified an abrupt shift from relatively dr…
Carbon accumulation in peat deposits from northern Sweden to northern Germany during the last millennium
Historic carbon accumulation rates in four bogs on a north to south transect from Sweden to Germany were calculated by using the bulk densities and carbon concentrations of 1-cm peat layers and a fine-resolution radiocarbon chronology. Carbon accumulation rates were compared to environmental data to explore the effects of climatic factors. Carbon accumulation rates in a period without clear human impact on the bog ecosystems ( c.ad 1700–ad 1800) …
Multiproxy study of the last meal of a mid-Holocene Oyogos Yar horse, Sakha Republic, Russia
The last meal of a horse that lived in the northern part of the Sakha Republic (Russia) c. 5400 years ago was studied using pollen, spores, botanical macroremains, lipid composition, and ancient DNA in order to reconstruct its components. Pollen of Poaceae was superabundant, but this may be because of over-representation as a consequence of grazed inflorescenses of grasses. We evaluate the paleo-environmental indicator value of the different meth…
Roman impact on the landscape near castellum Fectio, The Netherlands
Dating Recent Peat Accumulation in European Ombrotrophic Bogs
This study compares age estimates of recent peat deposits in 10 European ombrotrophic (precipitation-fed) bogs produced using the 14 C bomb peak, 210 Pb, 137 Cs, spheroidal carbonaceous particles (SCPs), and pollen. At 3 sites, the results of the different dating methods agree well. In 5 cores, there is a clear discrepancy between the 14 C bomb peak and 210 Pb age estimates. In the upper layers of the profiles, the age estimates of 14 C and 210 P…
Development and refinement of proxy-climate indicators from peats
Mid-Holocene (4200 kyr BP) mass mortalities in Mauritius (Mascarenes)
In the light of the currently increasing drought frequency and water scarcity on oceanic islands, it is crucial for the conservation of threatened insular vertebrates to assess how they will be affected. A 4000 yr old fossil assemblage in the Mare Aux Songes (MAS), southwest Mauritius, Mascarene Islands, contains bones of 100 000+ individual vertebrates, dominated by two species of giant tortoises Cylindraspis triserrata and C. inepta, the dodo R…
Solar Influences on Climate
Understanding the influence of solar variability on the Earth's climate requires knowledge of solar variability, solar-terrestrial interactions, and the mechanisms determining the response of the Earth's climate system. We provide a summary of our current understanding in each of these three areas. Observations and mechanisms for the Sun's variability are described, including solar irradiance variations on both decadal and centennial time scales …
The disappearance of Sphagnum imbricatum from Butterburn Flow, UK
We welcome the comments by Bjorn Robroek et al. ( The Holocene 19 (2009) 1093—1094, this issue) on our paper (McClymont et al., The Holocene 18 (2008) 991-1002) and the opportunity to discuss further the complexities that surround the disappearance of Sphagnum imbricatum from Butterburn Flow (our study), and the implications for understanding the disappearance of this species in northwest Europe. We also wish to clarify our site of study; we pres…
Environmental reconstruction of a Roman Period settlement site in Uitgeest (The Netherlands), with special reference to coprophilous fungi
Climate change and the expansion of the Scythian culture after 850 BC
Early human disturbance of the natural environment recorded in annually laminated sediments of Lake Gosciaz, central Poland
A database and synthesis of northern peatland soil properties and Holocene carbon and nitrogen accumulation
Here, we present results from the most comprehensive compilation of Holocene peat soil properties with associated carbon and nitrogen accumulation rates for northern peatlands. Our database consists of 268 peat cores from 215 sites located north of 45°N. It encompasses regions within which peat carbon data have only recently become available, such as the West Siberia Lowlands, the Hudson Bay Lowlands, Kamchatka in Far East Russia, and the Tibetan…
Columbus' footprint in Hispaniola
Results of the Cerpolex/Mammuthus Expeditions on the Taimyr Peninsula, Arctic Siberia, Russian Federation
Climatic change in Chile at around 2700 BP and global evidence for solar forcing
Palaeoecological and geological evidence for changing atmospheric circulation patterns in Chile indicates that equatorward and poleward shifts of the Southern Westerlies (Pacific precipitation source) were an important factor during Weichselian and Holocene climate change. We focus on the evidence and possible causes of considerable climate change in the Holocene at around 2700 BP, which was associated with a steep rise in atmospheric radiocarbon…
Evidence from northwest European bogs shows ‘Little Ice Age’ climatic changes driven by variations in solar activity
Fluctuations in Holocene atmospheric radiocarbon concentrations have been shown to be due to variations in solar activity. Analyses of both 10Be and 14 C nuclides con” rm that production-rate changes during the Holocene were largely modulated by solar activity. Analyses of peat samples from two intact European ombrotrophic bogs show that climatic deteriorations during the ‘Little Ice Age’ are associated with transitions to increasing atmospheric …
NPP-Id
Non-pollen palynomorphs (NPPs) form a large group of biological objects found in palynological slides besides pollen grains. This includes various remains of algae and fungi, shells, resting stages and eggs of invertebrates, among others. Publications of NPP-types started in the 1970s with studies of BvG and colleagues, and large numbers of new types continue to be published every year. For an overview of this diverse world of “extra fossils”, we…
Early Holocene environmental change, the presence and disappearance of early Mesolithic habitation near Zutphen (The Netherlands)
Columbus’ environmental impact in the New World
Columbus' arrival in the New World in AD 1492 on the northern coast of Hispaniola was followed by a suite of changes in land-use. We reconstruct environmental change from a 225-cm-long sediment core from site Los Indios from an abandoned and sediment-filled meander of the Yaque River, Cibao Valley, northeastern Dominican Republic. The sediment record starts ca. AD 195 (ca. 1755 cal. yr BP) and the history of the meander infill was monitored by ch…
Raised bed agriculture in northwest Europe triggered by climatic change around 850 BC
A sudden decline of solar activity around 850 calendar years BC caused a shift to a cool and wet climate in northwest Europe. Food production suddenly became problematic because of shorter, wetter growing seasons and increased night frost. This climate change triggered innovation and the development of a new agricultural system in continental northwestern Europe: arable farming on raised beds (Celtic field banks) laid out in a more or less checke…
Mid- to late-Holocene vegetation and land-use history in the Hadrian's Wall region of northern England
Pollen analyses of a peat profile collected from Butterburn Flow, northern England have been used to reconstruct vegetation and land-use change from the late Neolithic ( c. 3230 cal. BC) to the present day. `Wiggle-matching' of 42 AMS 14 C dates has enabled a precise (decadal scale) chronology to be established, and the results are interpreted within the context of previous studies of vegetation change in the area. Three late Neolithic—Bronze Age…
Solar forcing of climatic change during the mid-Holocene
Two cores of mid-Holocene raised-bog deposits from the Netherlands were 14 C wiggle-match dated at high precision. Changes in local moisture conditions were inferred from the changing species composition of consecutive series of macrofossil samples. Several wet-shifts were inferred, and these were often coeval with major rises in the Δ 14 C archive (probably caused by major declines in solar activity). The use of Δ 14 C as a proxy for changes in …
The Sharp Rise of Δ 14 C ca . 800 cal BC
In this study we report on accelerator mass spectrometry (AMS) wiggle-match dating of selected macrofossils from organic deposits ca . 800 cal bc ( ca . 2650 bp). Based on paleological, archaeological and geological evidence, we found that the sharp rise of atmospheric 14 C between 850 and 760 cal bc corresponds to the following related phenomena: 1. In European raised bog deposits, the changing spectrum of peat forming mosses and a sharp decline…
High-Resolution 14 C Dating of Organic Deposits Using Natural Atmospheric 14 C Variations
The occurrence of atmospheric 14 C variations complicates calibration, ie , the translation of 14 C ages into real calendar ages. The procedure of wiggle matching, however, allows very precise calibration, by matching known 14 C variations with wiggles in the floating chronology. In principle, wiggle matching can also be applied to a series of 14 C dates from organic (peat) deposits. Where, in general, 14 C ages are required at short distances an…
Changes in solar activity and Holocene climatic shifts derived from 14C wiggle-match dated peat deposits
Closely spaced sequences of accelerator mass spectrometer (AMS) 14 C dates of peat deposits display century-scale wiggles which can be fitted to the radiocarbon calibration curve. By wiggle-matching such sequences, high-precision calendar age chronologies can be generated which show that changes in mire surface wetness during the Bronze Age/Iron Age transition (c. 850 cal. BC) and the ‘Little Ice Age’ (Wolf, Spörer, Maunder and Dalton Minima) occ…
Late-Holocene human impact and peat development in the Černá Hora bog, Krkonoše Mountains, Czech Republic
Pollen analysis of a small peat bog at Černá Hora, Czech Republic, shows late-Holocene human impact on the vegetation. The palynological results are compared with historical documentation. Macrofossil analysis and changing pollen concentrations provide evidence that human impact on the regional vegetation determined changes in the hydrological conditions of the bog, and in the peat accumulation rate. From approxi mately 2100 BP (start of peat gro…
Dating Recent Peat Accumulation in European Ombrotrophic Bogs
This study compares age estimates of recent peat deposits in 10 European ombrotrophic (precipitation-fed) bogs produced using the 14 C bomb peak, 210 Pb, 137 Cs, spheroidal carbonaceous particles (SCPs), and pollen. At 3 sites, the results of the different dating methods agree well. In 5 cores, there is a clear discrepancy between the 14 C bomb peak and 210 Pb age estimates. In the upper layers of the profiles, the age estimates of 14 C and 210 P…
The disappearance of Sphagnum imbricatum from Butterburn Flow, UK
The disappearance of the previously abundant moss species Sphagnum imbricatum has been investigated at Butterburn Flow, northern England, using organic geochemical, elemental, macrofossil, pollen and testate amoebae analyses. Variations in the assemblage of peat-forming plants were tracked using the macrofossil distributions as well as the relative chain lengths of n-alkanes and concentrations of 5- n-alkylresorcinols and triterpenols. No signifi…
Response of an ombrotrophic bog to a regional climate event revealed by macrofossil, molecular and carbon isotopic data
We examined the variations in vegetation, organic carbon isotopic compositions and biomarker distributions spanning a well-constrained climatic shift in a Sub-Boreal Dutch raised bog. The macrofossils record a vegetation shift from a predominance of degraded Ericaceae rootlets to a predominance of well-preserved Sphagnum species, first S. cuspidatum, followed by S. imbricatum. This shift, as well as evidence from other macrofossils and fungal spo…
Typha as a wetland food resource
Bog burst in the eastern Netherlands triggered by the 2.8 kyr BP climate event
The nature and cause of the so-called 2.8 kyr BP event have been a subject of much debate. Peat sequences have provided much of the evidence for this event, but the process link between climate and peatland response is not well understood. Multiproxy, high-resolution analysis of a core from Bargerveen in the eastern Netherlands based on pollen, non-pollen palynomorphs, testate amoebae and geochemistry identified an abrupt shift from relatively dr…
Carbon accumulation in peat deposits from northern Sweden to northern Germany during the last millennium
Historic carbon accumulation rates in four bogs on a north to south transect from Sweden to Germany were calculated by using the bulk densities and carbon concentrations of 1-cm peat layers and a fine-resolution radiocarbon chronology. Carbon accumulation rates were compared to environmental data to explore the effects of climatic factors. Carbon accumulation rates in a period without clear human impact on the bog ecosystems ( c.ad 1700–ad 1800) …
Roman impact on the landscape near castellum Fectio, The Netherlands
A palaeoecological study of holocene peat bog sections in Germany and The Netherlands, based on the analysis of pollen, spores and macro- and microscopic remains of fungi, algae, cormophytes and anima…
Paleoecological studies in the Klokkeweel bog near hoogkarspel (prov. of Noord-Holland)
A palaeoecological study of an upper late glacial and holocene sequence from “de borchert”, The Netherlands
A late holocene deposit under the Westfriese Zeedijk near Enkhuizen (Prov. of Noord-Holland, The Netherlands)
Palaeoecology and stratigraphy of the lateglacial type section at Usselo (the Netherlands)
High-Resolution 14 C Dating of Organic Deposits Using Natural Atmospheric 14 C Variations
The occurrence of atmospheric 14 C variations complicates calibration, ie , the translation of 14 C ages into real calendar ages. The procedure of wiggle matching, however, allows very precise calibration, by matching known 14 C variations with wiggles in the floating chronology. In principle, wiggle matching can also be applied to a series of 14 C dates from organic (peat) deposits. Where, in general, 14 C ages are required at short distances an…
Early human disturbance of the natural environment recorded in annually laminated sediments of Lake Gosciaz, central Poland
Dating raised bogs
The Sharp Rise of Δ 14 C ca . 800 cal BC
In this study we report on accelerator mass spectrometry (AMS) wiggle-match dating of selected macrofossils from organic deposits ca . 800 cal bc ( ca . 2650 bp). Based on paleological, archaeological and geological evidence, we found that the sharp rise of atmospheric 14 C between 850 and 760 cal bc corresponds to the following related phenomena: 1. In European raised bog deposits, the changing spectrum of peat forming mosses and a sharp decline…
Improving Methodology for High-Resolution Reconstruction of Sea-Level Rise and Neotectonics by Paleoecological Analysis and AMS 14 C Dating of Basal Peats
Sea-level research in several submerging coastal regions has traditionally been based on 14 C dating of basal peats that overlie a compaction-free substratum and can be related to paleo-(ground)water levels. Provided that an unequivocal relationship between (ground)water level and sea level can be assumed, this approach contains two sources of uncertainty: (1) the paleoenvironmental interpretation of samples is usually based on inherently inaccur…
Comment on “A Large California Flood and Correlative Global Climatic Events 400 Years Ago” (Schimmelmann et al., 1998)
Fine-resolution Upper Weichselian and Holocene palynological record from Navarrés (Valencia, Spain) and a discussion about factors of Mediterranean forest succession
Reduced solar activity as a trigger for the start of the Younger Dryas
Climatic change in Chile at around 2700 BP and global evidence for solar forcing
Palaeoecological and geological evidence for changing atmospheric circulation patterns in Chile indicates that equatorward and poleward shifts of the Southern Westerlies (Pacific precipitation source) were an important factor during Weichselian and Holocene climate change. We focus on the evidence and possible causes of considerable climate change in the Holocene at around 2700 BP, which was associated with a steep rise in atmospheric radiocarbon…
Late-Holocene human impact and peat development in the Černá Hora bog, Krkonoše Mountains, Czech Republic
Pollen analysis of a small peat bog at Černá Hora, Czech Republic, shows late-Holocene human impact on the vegetation. The palynological results are compared with historical documentation. Macrofossil analysis and changing pollen concentrations provide evidence that human impact on the regional vegetation determined changes in the hydrological conditions of the bog, and in the peat accumulation rate. From approxi mately 2100 BP (start of peat gro…
Evidence from northwest European bogs shows ‘Little Ice Age’ climatic changes driven by variations in solar activity
Fluctuations in Holocene atmospheric radiocarbon concentrations have been shown to be due to variations in solar activity. Analyses of both 10Be and 14 C nuclides con” rm that production-rate changes during the Holocene were largely modulated by solar activity. Analyses of peat samples from two intact European ombrotrophic bogs show that climatic deteriorations during the ‘Little Ice Age’ are associated with transitions to increasing atmospheric …
Major Δ14C excursions during the late glacial and early Holocene
Response of an ombrotrophic bog to a regional climate event revealed by macrofossil, molecular and carbon isotopic data
We examined the variations in vegetation, organic carbon isotopic compositions and biomarker distributions spanning a well-constrained climatic shift in a Sub-Boreal Dutch raised bog. The macrofossils record a vegetation shift from a predominance of degraded Ericaceae rootlets to a predominance of well-preserved Sphagnum species, first S. cuspidatum, followed by S. imbricatum. This shift, as well as evidence from other macrofossils and fungal spo…
Environmental reconstruction of a Roman Period settlement site in Uitgeest (The Netherlands), with special reference to coprophilous fungi
Late Holocene climatic changes in Tierra del Fuego based on multiproxy analyses of peat deposits.
A ca. 1400-yr record from a raised bog in Isla Grande, Tierra del Fuego, Argentina, registers climate fluctuations, including a Medieval Warm Period, although evidence for the ‘Little Ice Age’ is less clear. Changes in temperature and/or precipitation were inferred from plant macrofossils, pollen, fungal spores, testate amebae, and peat humification. The chronology was established using a 14 C wiggle-matching technique that provides improved age …
Changes in solar activity and Holocene climatic shifts derived from 14C wiggle-match dated peat deposits
Closely spaced sequences of accelerator mass spectrometer (AMS) 14 C dates of peat deposits display century-scale wiggles which can be fitted to the radiocarbon calibration curve. By wiggle-matching such sequences, high-precision calendar age chronologies can be generated which show that changes in mire surface wetness during the Bronze Age/Iron Age transition (c. 850 cal. BC) and the ‘Little Ice Age’ (Wolf, Spörer, Maunder and Dalton Minima) occ…
Solar forcing of climatic change during the mid-Holocene
Two cores of mid-Holocene raised-bog deposits from the Netherlands were 14 C wiggle-match dated at high precision. Changes in local moisture conditions were inferred from the changing species composition of consecutive series of macrofossil samples. Several wet-shifts were inferred, and these were often coeval with major rises in the Δ 14 C archive (probably caused by major declines in solar activity). The use of Δ 14 C as a proxy for changes in …
Climate change and the expansion of the Scythian culture after 850 BC
Vegetation disturbance and human population in Colombia - a regional reconstruction
Palaeoecologists using pollen to map vegetation since the last ice age have noted numerous changes - which they feel increasingly obliged to blame on humans. These changes, such as deforestation or the dominance of certain plants, may happen suddenly or take place over thousands of years. The authors study the pollen record in Colombia, identify plants diagnostic of cultivation or disturbed ground ("degraded vegetation") and use them to map human…
Early Holocene environmental change, the presence and disappearance of early Mesolithic habitation near Zutphen (The Netherlands)
Geology and Paleoclimatology Research (47 obras) · Geography (45 obras) · Archaeology (35 obras) · Physical geography (32 obras) · Holocene (31 obras) · Geology (30 obras) · Biology (28 obras) · Peat (25 obras) · Ecology (24 obras) · Pollen (21 obras)