Dung fungi as a proxy for megaherbivores: opportunities and limitations for archaeological applications
AG Perrotti, E Van Asperen - Vegetation History and Archaeobotany, 2019 - Springer
The use of spores of coprophilous fungi from sedimentary sequences as proxy evidence for
large herbivore abundance has garnered pronounced attention and scrutiny over the past …
large herbivore abundance has garnered pronounced attention and scrutiny over the past …
A global Bayesian temperature calibration for lacustrine brGDGTs
Despite widespread use of branched glycerol dialkyl glycerol tetraethers (brGDGTs) for
paleo-temperature reconstruction, no global calibration for their application in lakes has …
paleo-temperature reconstruction, no global calibration for their application in lakes has …
An overview of the taxonomic groups of non-pollen palynomorphs
Non-pollen palynomorphs (NPPs) are 'extra'microfossils often found in palynology slides.
These include remains of organisms within the size range of pollen grains (c. 10–250 µm) …
These include remains of organisms within the size range of pollen grains (c. 10–250 µm) …
Contributions of Quaternary botany to modern ecology and biogeography
HJB Birks - Plant Ecology & Diversity, 2019 - Taylor & Francis
ABSTRACT Quaternary (last 2.6 million years) botany involves studying plant megafossils
(eg tree stumps), macrofossils (eg seeds, leaves), and microfossils (eg pollen, spores) …
(eg tree stumps), macrofossils (eg seeds, leaves), and microfossils (eg pollen, spores) …
Tools for Non-Pollen Palynomorphs (NPPs) analysis: A list of Quaternary NPP types and reference literature in English language (1972–2011)
A Miola - Review of Palaeobotany and Palynology, 2012 - Elsevier
A systematic study of Non-Pollen Palynomorphs (NPPs) from Quaternary sediments was
begun in 1968 in the Hugo de Vries-Laboratory (Institute for Biodiversity and Ecosystem …
begun in 1968 in the Hugo de Vries-Laboratory (Institute for Biodiversity and Ecosystem …
Non-pollen palynomorphs
LS Shumilovskikh, B van Geel - Handbook for the analysis of micro …, 2020 - Springer
Non-pollen palynomorphs (NPP) in pollen slides form a large, inhomogeneous group of
remains of organisms that represents a memory of former, often strictly local environmental …
remains of organisms that represents a memory of former, often strictly local environmental …
[HTML][HTML] Spatial distribution of modern pollen and fungal spores and their ecological indication in Qinghai Lake on northeastern Tibetan Plateau, China
H Gou, H Wei, R Duan, T Chen, Q Fan, Y Du, X Cao - Ecological Indicators, 2022 - Elsevier
Abstract The Qinghai-Tibet Plateau (QTP)–also called the “third pole”–is an ideal area to
study the long-term relationship between people and the environment due to its sensitivity to …
study the long-term relationship between people and the environment due to its sensitivity to …
Pollen analysis of middle to late Holocene records shows little evidence for grazing disturbance to alpine grassland on the Tibetan Plateau until modern times
Understanding human impact on the vegetation of the Tibetan Plateau through the
Holocene is important for developing strategies for sustainable ecosystem management in …
Holocene is important for developing strategies for sustainable ecosystem management in …
Mid-Holocene vegetation history and Neolithic land-use in the Lake Banyoles area (Girona, Spain)
This paper focuses on high-resolution analysis of pollen and sedimentology and botanical
macro-remains analysis in a core from Lake Banyoles (Girona, Spain). The core sequence …
macro-remains analysis in a core from Lake Banyoles (Girona, Spain). The core sequence …
Erosion or plant succession—How to interpret the presence of arbuscular mycorrhizal fungi (Glomeromycota) spores in pollen profiles collected from mires
P Kołaczek, S Zubek, J Błaszkowski, P Mleczko… - Review of Palaeobotany …, 2013 - Elsevier
The spores of arbuscular mycorrhizal fungi (AMF), microorganisms which occur
belowground, are recognized as important indicators of erosion in palaeoecological …
belowground, are recognized as important indicators of erosion in palaeoecological …