about
Subtropical Arctic Ocean temperatures during the Palaeocene/Eocene thermal maximumStable carbon isotope analyses of nanogram quantities of particulate organic carbon (pollen) with laser ablation nano combustion gas chromatography/isotope ratio mass spectrometryUnexpected biotic resilience on the Japanese seafloor caused by the 2011 Tōhoku-Oki tsunami.Ocean acidification reduces growth and calcification in a marine dinoflagellateNiche segregation of ammonia-oxidizing archaea and anammox bacteria in the Arabian Sea oxygen minimum zoneFossilized glycolipids reveal past oceanic N2 fixation by heterocystous cyanobacteriaAustralian tropical cyclone activity lower than at any time over the past 550-1,500 years.Proton pumping accompanies calcification in foraminifera.Detection, isolation, and characterization of acidophilic methanotrophs from Sphagnum mosses.Atmospheric carbon injection linked to end-Triassic mass extinction.Temperature-induced increase in methane release from peat bogs: a mesocosm experimentEnvironmental precursors to rapid light carbon injection at the Palaeocene/Eocene boundary.The Eocene Arctic Azolla bloom: environmental conditions, productivity and carbon drawdown.Effect of different seawater Mg2 + concentrations on calcification in two benthic foraminifers.Sedimentation Pulse in the NE Gulf of Mexico following the 2010 DWH Blowout.Combined Effects of Ocean Acidification and Light or Nitrogen Availabilities on 13C Fractionation in Marine Dinoflagellates.CO2-dependent carbon isotope fractionation in dinoflagellates relates to their inorganic carbon fluxes.Extreme warmth and heat-stressed plankton in the tropics during the Paleocene-Eocene Thermal Maximum.Metabolic Adaptation, a Specialized Leaf Organ Structure and Vascular Responses to Diurnal N2 Fixation by Nostoc azollae Sustain the Astonishing Productivity of Azolla Ferns without Nitrogen Fertilizer.Astronomical age constraints and extinction mechanisms of the Late Triassic Carnian crisis.Early Palaeogene temperature evolution of the southwest Pacific Ocean.Anammox bacterial populations in deep marine hypersaline gradient systems.Is there foul play in the leaf pocket? The metagenome of floating fern Azolla reveals endophytes that do not fix N2 but may denitrify.Evidence for active El Niño Southern Oscillation variability in the Late Miocene greenhouse climatePaleocene–Eocene warming and biotic response in the epicontinental West Siberian SeaWarm and wet conditions in the Arctic region during Eocene Thermal Maximum 2Transient Middle Eocene Atmospheric CO2 and Temperature VariationsGlobal prevalence of methane oxidation by symbiotic bacteria in peat-moss ecosystemsHigh resolution geochemical and grain-size analysis of the AD 1755 tsunami deposit: Insights into the inland extent and inundation phasesMultiple water isotope proxy reconstruction of extremely low last glacial temperatures in Eastern Beringia (Western Arctic)Large effect of irradiance on hydrogen isotope fractionation of alkenones in Emiliania huxleyiAn interlaboratory study of TEX86and BIT analysis of sediments, extracts, and standard mixturesTrends in element incorporation in hyaline and porcelaneous foraminifera as a function of <i>p</i>CO<sub>2</sub>Benthic foraminiferal Mn / Ca ratios reflect microhabitat preferencesBa incorporation in benthic foraminiferaSingle-species dinoflagellate cyst carbon isotope ecology across the Paleocene-Eocene Thermal MaximumGlendonites track methane seepage in Mesozoic polar seasStable carbon isotope fractionation of organic cyst-forming dinoflagellates: Evaluating the potential for a CO 2 proxyEustatic variations during the Paleocene-Eocene greenhouse worldClimate-controlled multidecadal variability in North African dust transport to the Mediterranean
P50
Q28244186-6C4BB57C-DB36-418B-91BE-30917528A03CQ28591016-85005729-2996-47A5-ACFD-6AEA5E5D2D2FQ28649654-0CD1738E-5646-4F8D-BBA5-D4EB5B0FEBFAQ28681563-692DC3B9-0EF2-4443-AE66-FE89DDBC7256Q28742300-82037107-F8FF-40B3-AD5D-6B554455A5CAQ28748315-6E3AF28E-5C08-4072-8B55-85FFAC0697EDQ30745060-383CABF2-1C40-4C36-A681-9BDEC2A9B041Q30837316-70116397-F92D-4BB6-BF25-B4F99F666D41Q33949391-ED63C2DD-5F83-4853-8BED-82C94480DDC7Q33967759-831EEF8F-D69B-4437-A8C1-0F1482585D6EQ34328222-CE6841F0-BECA-4153-B7EB-EAE5F9AF7AFCQ34728416-C70E36D9-B741-4AEF-BECF-F6B1679DC6ECQ34969415-1DB75361-EF61-40F0-B8E1-480418542B13Q35668129-82EBBF90-A27A-45D3-891E-D5EBC8DE1BB8Q35690844-588FF926-9D17-4AD4-9DB5-54FBBAED61C3Q36010903-FF79D58F-4049-4D90-B0AA-3CD7C732E6DFQ37608601-8400E048-BA77-4662-AD26-68C4A899E0B8Q37679845-3F2B1ADE-64D8-42C7-ABC9-362FF0881328Q37731049-B9DB538F-B4C6-42B8-ADE8-03B65D9F3AF1Q38752509-D5FCD7D3-D5A2-4B9D-9705-F7BFCCF15BC2Q38908995-B8FDAFBA-C41E-440D-A8D0-B0A0EDB4C3D3Q43017533-AB7D8F25-C98D-4970-8758-D2EC23B8A9D5Q46272269-C0EE372B-58F8-4386-BE34-12B877B441A0Q56225508-437E9373-31FC-4C02-B853-6C150BDD5314Q56638805-48E3D54C-5F2D-4101-8A4C-7ACCE640332AQ56680924-ECBB509D-AFFA-46E9-B1E9-C987832BF839Q56854440-9D34F762-34EC-4143-8BA0-D7BF7CE3F078Q57273415-2A6F5A3C-29D9-4DBB-9963-C14D4877872AQ57529534-2F18E94B-1404-4F3B-9889-EA1BB1C23EBDQ57637864-286CAEDC-CAC1-4A30-B875-80BF02D5AC5DQ57873607-2C751C97-FCDA-49C2-9EF1-B649B88FAD55Q57881020-6BEA8669-20B5-405C-9028-346E28B634ACQ57890298-5CF1BFCD-5D4F-41E8-B19E-8CF8FCF3B636Q57890483-B161DE84-17B7-455D-B8B7-C80D1366230BQ57891583-2BA78B49-BB7D-4319-9B1E-D1C93643D068Q57967950-642F10F9-8845-4E15-B76D-43C8E3D64286Q57978522-1AA21DC7-6A3D-480D-9D19-4030DFA9DCBBQ58074255-393DAC20-4360-4BF7-A2DC-82A0127AF2A3Q58074315-72C8114F-89D2-40D6-8F2D-F56038F53C19Q58079968-1E1C68EF-2599-446A-B637-617FAB939C80
P50
description
hulumtues
@sq
researcher
@en
wetenschapper
@nl
հետազոտող
@hy
name
Gert-Jan Reichart
@ast
Gert-Jan Reichart
@en
Gert-Jan Reichart
@es
Gert-Jan Reichart
@nl
Gert-Jan Reichart
@sl
type
label
Gert-Jan Reichart
@ast
Gert-Jan Reichart
@en
Gert-Jan Reichart
@es
Gert-Jan Reichart
@nl
Gert-Jan Reichart
@sl
prefLabel
Gert-Jan Reichart
@ast
Gert-Jan Reichart
@en
Gert-Jan Reichart
@es
Gert-Jan Reichart
@nl
Gert-Jan Reichart
@sl
P1053
N-6308-2018
P106
P1153
7004045376
P21
P2798
P31
P3191
P3829
P496
0000-0002-7256-2243