OOIR: Observatory of International Research

Papers

(The H4-Index of Global and Planetary Change is 29. The table below lists those papers that are above that threshold based on CrossRef citation counts [max. 250 papers]. The publications cover those that have been published in the past four years, i.e., from 2021-05-01 to 2025-05-01.)

Article	Citations
Warming and drying increased the interspecies consistency of tree-ring lignin methoxy δ2H variability at the alpine treeline	77
Dual carbon isotopes constrain the sources and age variations of terrestrial organic carbon in the middle Okinawa Trough since the last deglaciation	60
Improved geometry of the subducting Philippine Sea plate beneath the Suruga Trough	57
Constraints on Earth-Moon dynamical parameters from Eocene cyclostratigraphy	52
Assessment of Indian Ocean upwelling changes and its relationship with the Indian monsoon	51
Growing at the limit: Reef growth sensitivity to climate and oceanographic changes in the South Western Atlantic	49
Change of global land extreme temperature in the future	45
Coastal submersions in the north-eastern Adriatic during the last 5200 years	42
Ichnology, sedimentology, and orbital cycles in the hemipelagic Early Jurassic Laurasian Seaway (Pliensbachian, Cardigan Bay Basin, UK)	41
A link between the paleoenvironment and PETM via trace element proxies in Southwest Atlantic sediments	40
Permafrost controls the displacement rates of large unstable rock-slopes in subarctic environments	39
ITCZ precipitation and cloud cover excursions control Cedrela nebulosa tree-ring oxygen and carbon isotopes in the northwestern Amazon	38
Regional landscape change triggered by Andean uplift: The extinction of Sparassodonta (Mammalia, Metatheria) in South America	38
Editorial Board	37
Nature of Devonian anoxic events based on multiproxy records from Panthalassa, NW Canada	37
Mid-Piacenzian and future changes in South Asian precipitation under global warming	33
Coupled feedback between the tropics and subtropics of the Indian Ocean with emphasis on the coupled interaction between IOD and SIOD	33
Climate or tectonics? What controls the spatial-temporal variations in erosion rates across the Eastern Cordillera of Colombia? [Global and planetary change, volume 203, August 2021, 103,541]: Comment	33
Tracking magmatism and oceanic change through the early Aptian Anoxic Event (OAE 1a) to the late Aptian: Insights from osmium isotopes from the westernmost Tethys (SE Spain) Cau Core	32
Orbital eccentricity and inclination metronomes in Middle Miocene lacustrine mudstones of Jiuxi Basin, Tibet: Closing an astrochronology time gap and calibrating global cooling events	31
Early post-rift confined turbidite systems in a supra-detachment basin: Implications for the early to middle Miocene basin evolution and hydrocarbon exploration of the Pannonian Basin	31
Anaerobic oxidation of methane and greigite formation: Evidence of isotopically heavy pyrite in Pleistocene coastal sediments from the South Yellow Sea	31
Spatio-temporal characteristics and driving factors of flash drought in northern China from 1978 to 2020	31
Population migration with improved productivity caused a heterogeneity pattern of Holocene vegetation succession in typical areas of the lower Yangtze region	31
Temperature variability revealed by lacustrine brGDGTs in northeastern China since the Last Glacial Maximum	31

Impact of the 1994–1997 temporary decrease in Northern Hemisphere stratospheric methane on the 1990s methane trend	30
Benzo[ghi]fluoranthene and benz[a]anthracene as potentially useful wildfire temperature indicators	30
The Central Paratethys Sea – Part of the tropical eastern Atlantic rather than gate into the Indian Ocean	30
Resolving Cenozoic climate pattern debate in East Asia: Insights from orbital-scale oscillations	29
Anthropogenic modification of phosphorus sequestration in lake sediments during the Holocene: A global perspective	29
Precipitation dynamics and its interactions with possible drivers over global highlands	29
Response of calcareous nannoplankton to the Paleocene–Eocene Thermal Maximum in the Paratethys Seaway (Tarim Basin, West China)	29