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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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East Africa
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Kenya (2)
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Lake Turkana (2)
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Sudan (1)
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East African Lakes
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Invertebrata
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Tertiary
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Mesozoic
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sulfates
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Primary terms
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absolute age (3)
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Africa
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East Africa
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Kenya (2)
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Lake Turkana (2)
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Sudan (1)
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East African Lakes
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Lake Turkana (2)
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Southern Africa
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Antarctica (1)
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Asia
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Far East
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atmosphere (3)
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Western Canada
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carbon
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Caribbean region
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Lesser Antilles
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Cenozoic
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Koobi Fora Formation (2)
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Quaternary
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upper Holocene (4)
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Pleistocene
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middle Pleistocene (1)
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upper Pleistocene (3)
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upper Quaternary (1)
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-
Tertiary
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Neogene
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Miocene
-
Guantao Formation (1)
-
-
Pliocene (2)
-
-
-
-
Chordata
-
Vertebrata
-
Tetrapoda
-
Mammalia
-
Theria
-
Eutheria
-
Proboscidea
-
Elephantoidea
-
Elephantidae
-
Mammuthus
-
Mammuthus columbi (1)
-
-
-
-
-
-
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-
-
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clay mineralogy (1)
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ecology (22)
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Donets Basin (1)
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hydrogen
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deuterium (1)
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Chondrites ichnofossils (1)
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igneous rocks
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plutonic rocks
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diorites
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tonalite (1)
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granites (1)
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granodiorites (1)
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monzonites (1)
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ultramafics
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pyroxenite
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garnet pyroxenite (1)
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-
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volcanic rocks
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basalts (1)
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glasses
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perlite (1)
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pyroclastics
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pumice (1)
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tuff (1)
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inclusions (1)
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Invertebrata
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Chelicerata
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Arachnida (1)
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Mandibulata
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Insecta (1)
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Myriapoda (1)
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isostasy (1)
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isotopes
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radioactive isotopes
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stable isotopes
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Ca-44/Ca-40 (1)
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deuterium (1)
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Fe-54 (1)
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Fe-56/Fe-54 (1)
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Sr-87/Sr-86 (1)
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Mesozoic
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roots
The Devonian landscape factory: plant–sediment interactions in the Old Red Sandstone of Svalbard and the rise of vegetation as a biogeomorphic agent
Impact of acidic volcanic emissions on ash leaching and on the bioavailability and mobility of trace metals in soils of Mt. Etna
Land plant evolution decreased, rather than increased, weathering rates
Breaking it Down: Mechanical Processes in the Weathering Engine
How Plants Enhance Weathering and How Weathering is Important to Plants
Addressing time-scale–dependent erosion rates from measurement methods with censorship
Backarc origin for Neoarchean ultrahigh-temperature metamorphism, eclogitization, and orogenic root growth
A Simple Representation of Plant Water Storage Effects in Coupled Soil Water Flow and Transpiration Stream Modeling
Reply to Discussion on ‘Tectonic and environmental controls on Palaeozoic fluvial environments: reassessing the impacts of early land plants on sedimentation’ Journal of the Geological Society, London , https://doi.org/10.1144/jgs2016-063
Evaluation of Simulated Transpiration from Maize Plants on Lysimeters
THE WACO MAMMOTH NATIONAL MONUMENT MAY REPRESENT A DIMINISHED WATERING-HOLE SCENARIO BASED ON PRELIMINARY EVIDENCE OF POST-MORTEM SCAVENGING
Gneiss domes, vertical and horizontal mass transfer, and the initiation of extension in the hot lower-crustal root of a continental arc, Fiordland, New Zealand
Monitoring of Stem Water Content of Native and Invasive Trees in Arid Environments Using GS3 Soil Moisture Sensors
Experimental Evaluation of Earthworm and Plant Root Soil Penetration–Cavity Expansion Models Using Cone Penetrometer Analogs
Spatio-temporal Scaling of Vegetation Growth and Soil Formation from Percolation Theory
Water for Carbon, Carbon for Water
Mechanisms of Early Microbial Establishment on Growing Root Surfaces
Structured Heterogeneity in a Marine Terrace Chronosequence: Upland Mottling
Abstract A siliceous permineralized peat block recovered from Hopen in the Svalbard archipelago hosts a low-diversity Late Triassic flora dominated by autochthonous roots and stems of bennettitaleans and lycophytes, and parautochthonous leaves, sporangia, spores and pollen from a small range of pteridophytes and gymnosperms. Some parenchymatous bennettitalean root cells show interactions with chytrid fungi and bacteria; the remains of other fungi and fungi-like organisms are dispersed within the peat’s detrital matrix. Cavities excavated through some roots and compacted detritus contain abundant coprolites probably derived from sapro-xylophagous oribatid mites, although no body fossils have yet been identified. Sparse larger coprolites containing leaf fragments attest to the presence of invertebrate folivores in the ancient ecosystem. The low-diversity flora, relatively few trophic levels and simple nutritional web, together with sedimentological aspects of the host formation and the peat structure, collectively favour accumulation of the organic mass as a fibric (root-dominated) peat within a temperate (high middle-latitude), well-aerated mire.