Wildfires affect 40% of the earth's terrestrial biome, but much of our knowledge of wildfire
activity is limited to the satellite era. Improved understanding of past fires is necessary to …

There is limited understanding of temperature and atmospheric circulation changes that
accompany an Atlantic Meridional Overturning Circulation (AMOC) slowdown beyond the …

Palaeoclimate information on multiple climate variables at different spatiotemporal scales is
becoming increasingly important to understand environmental and societal responses to …

The Last Interglacial (LIG,~ 130–116 ka) was one of the warmest interglacials of the past
800,000 years and an important test bed for future climate conditions warmer than today. LIG …

This study utilizes speleothem trace elements as climate proxies to reconstruct hydroclimate
variability over approximately 350 years in the Southern Cook Islands. Stalagmites Pu17 …

Annually laminated stalagmites ER77 and ER78 from Grotta di Ernesto provide an accurate
annual record of environmental and anthropogenic signals for the last~ 200 years. Two …

Abstract In the European Alps, the Last Interglacial (LIG,~ 129–116 ka) has been primarily
studied using pollen preserved in mires and lake sediments. These records document the …

Rationale Suites of trace elements are routinely used in speleothems as proxies to
understand periods of past climate change. Laser ablation techniques are regularly …

The landscape reconstruction in the Jebel El Mida area during the Late Pleistocene was
based on the continental carbonate record, particularly on the clastic tufa deposits. Four …

1 Le dernier interglaciaire (LIG,~ 130-116 ka) a été l'un des interglaciaires les plus chauds
des 800 000 dernières années. Bien que le forçage climatique ait été différent de celui de …