Results 71 to 80 of about 43,956 (239)
PLANTS, PEOPLE, PLANET, EarlyView.Large palynological collections have been built over decades and contain vital information. However, they are often difficult to access and use effectively. What is the point of having such collections if they are not fully utilizable? To solve this problem, we digitized the Smithsonian palynological collection using both light and confocal microscopy.
Carlos Jaramillo +37 more
wiley +1 more source
Reconciling diverse lacustrine and terrestrial system response to penultimate deglacial warming in southern Europe [PDF]
, 2015 Unlike the most recent deglaciation, the regional expression of climate changes during the penultimate deglaciation remains understudied, even though it led into a period of excess warmth with estimates of global average temperature 1–2 °C, and sea level
Frogley, Michael R +4 more
core +3 more sources
From Rackham to REVEALS : Reflections on Palaeoecological Approaches to Woodland and Trees [PDF]
, 2017 In this paper we reflect on aspects of palaeoecological approaches to understanding past woodland environments. With increasing requirements for interdisciplinarity in research, and an increase in popular interest in the ‘natural environment’ such as ...
Gearey, B.R., Richer, Susan
core +2 more sources
Island biodiversity conservation needs palaeoecology [PDF]
Nature Ecology & Evolution, 2017 The discovery and colonization of islands by humans has invariably resulted in their widespread ecological transformation. The small and isolated populations of many island taxa, and their evolution in the absence of humans and their introduced taxa, mean that they are particularly vulnerable to human activities.
Sandra Nogué +8 more
openaire +6 more sources
Shared leadership can promote success in collaborative research networks in ecology
Functional Ecology, EarlyView.Read the free Plain Language Summary for this article on the Journal blog. Abstract While collaborative science is becoming the norm in ecology, many ecologists participating in collaborations are less aware of the body of research that studies the processes by which collaborative teams organize and communicate.
Daniel C. Allen +27 more
wiley +1 more source
Post-disturbance vegetation dynamics during the Late Pleistocene and the Holocene: An example from NW Iberia [PDF]
, 2012 This is the post-print version of the final paper published in Global and Planetary Change. The published article is available from the link below. Changes resulting from the publishing process, such as peer review, editing, corrections, structural ...
Allen +67 more
core +2 more sources
Integrative Zoology, EarlyView.This study provides the first isotopic analysis of Oligocene mammals from Quebrada Fiera, Mendoza, Argentina, filling a major gap in South American paleontology. It reveals a latitudinal gradient in aridity due to the Andean rain shadow and highlights the role of (semi)permanent water bodies in sustaining diverse herbivore communities. Additionally, it
Dánae Sanz‐Pérez +4 more
wiley +1 more source
PAST GLOBAL CLIMATE CHANGE: A HIGH RESOLUTION EVIDENCE FROM SW SIBERIA
Литосфера, 2019 The southern Siberian loess, being a continuation of the Eurasian loess-belt, has provided one of the most complete terrestrial proxy records on the global past climate development.
doaj
The osteoderm microstructure in doswelliids and proterochampsids and its implications for palaeobiology of stem archosaurs [PDF]
Acta Palaeontologica Polonica, 2017 Osteoderms are common in most archosauriform lineages, including basal forms, such as doswelliids and proterochampsids. In this survey, osteoderms of the doswelliids Doswellia kaltenbachi and Vancleavea campi, and proterochampsid Chanaresuchus bonapartei
Denis A. Ponce +3 more
doaj +1 more source
Hominin palaeoecology in Late Pliocene Malawi : first insights from isotopes (13C, 18O) in mammal teeth [PDF]
, 2011 Carbon-13 and oxygen-18 abundances were measured in large mammal skeletal remains (tooth enamel, dentine and bone) from the Chiwondo Beds in Malawi, which were dated by biostratigraphic correlation to ca. 2.5 million years ago.
Bocherens, Herv +3 more
core +2 more sources