about
Devonian rise in atmospheric oxygen correlated to the radiations of terrestrial plants and large predatory fishInteractions between Ediacaran animals and microbial mats: Insights from Lamonte trevallis, a new trace fossil from the Dengying Formation of South ChinaStatistical analysis of iron geochemical data suggests limited late Proterozoic oxygenation.Proterozoic ocean redox and biogeochemical stasis.Pulse of atmospheric oxygen during the late Cambrian.Uranium isotopes distinguish two geochemically distinct stages during the later Cambrian SPICE event.Sulfur isotopes track the global extent and dynamics of euxinia during Cretaceous Oceanic Anoxic Event 2.Evidence for rapid weathering response to climatic warming during the Toarcian Oceanic Anoxic Event.A geochemical study of the Ediacaran discoidal fossil Aspidella preserved in limestones: Implications for its taphonomy and paleoecology.Placing an upper limit on cryptic marine sulphur cycling.Geochemical evidence for widespread euxinia in the later Cambrian ocean.Evolution of the global phosphorus cycle.Uncovering the Neoproterozoic carbon cycle.Thallium isotopes reveal protracted anoxia during the Toarcian (Early Jurassic) associated with volcanism, carbon burial, and mass extinctionTracking the rise of eukaryotes to ecological dominance with zinc isotopesSulphur and carbon cycling in the subduction zone mélangeLate inception of a resiliently oxygenated upper oceanEvidence for the development of local anoxia during the Cambrian SPICE event in eastern North AmericaAtmosphere-ocean oxygen and productivity dynamics during early animal radiations
P50
Q24624525-4BE26C80-7438-432E-AC1C-83C048FBDE54Q29012168-216AF547-F642-427B-B5E4-F18236FC47F6Q30982109-AFB3CFC9-F5D4-482B-B8C0-EFEFC0B2F662Q34334288-CF20DE4B-03C7-4BDB-B884-B0B5982FD842Q34652078-583B53CF-4262-4478-8056-FE85A796D8F8Q35079855-A2E5657D-9FE8-4ED0-A0D1-8FCE72860CCDQ37319572-BD45D208-F058-4B52-931D-3F2C4357677DQ38685337-A316066A-E288-4E7C-BF02-5687978D9FA7Q38843106-11A337F1-B62E-4A2F-B428-6E1A5AC3CA35Q42681429-CEB3C80B-50E7-4B84-9267-9373343A1B79Q44442073-4285F9AF-6960-4F2A-8FC8-8BA18861F4C9Q45049399-D9785093-8193-42E4-A049-305D0F905297Q46552573-AA495872-5F08-4843-A2A6-A357CDEBEF0AQ56221438-0C0E97B0-99D8-4A7D-A64E-3D17FDEC09EAQ56594167-E9AAA132-70CB-4CA6-8006-766BE03CEAD1Q57811592-D9337DB5-F491-4E80-A0C3-F5BB2EBEDDF0Q58074628-32D2B4E3-93DE-435B-84B0-B5E9230971F0Q63388923-2068D4B1-2881-4ABE-B951-2564FE4AC0F0Q90001615-11CD967A-7D1C-4755-845D-460A28141AF6
P50
description
hulumtues
@sq
researcher
@en
wetenschapper
@nl
հետազոտող
@hy
name
Benjamin Gill
@ast
Benjamin Gill
@en
Benjamin Gill
@es
Benjamin Gill
@nl
Benjamin Gill
@sl
type
label
Benjamin Gill
@ast
Benjamin Gill
@en
Benjamin Gill
@es
Benjamin Gill
@nl
Benjamin Gill
@sl
prefLabel
Benjamin Gill
@ast
Benjamin Gill
@en
Benjamin Gill
@es
Benjamin Gill
@nl
Benjamin Gill
@sl
P1053
B-8047-2012
P106
P1153
15132002500
P21
P31
P3829
P4450
benjamin-gilles
P496
0000-0001-7402-0811