Orbital-to-millennial scale climate variability during Marine Isotope Stages 5 to 3 in northeast Iberia

Orbital-to-millennial scale climate variability during Marine Isotope Stages 5 to 3 in northeast Iberia

The climate during the last glacial cycle was characterized by abrupt millennial-scale changes superimposed on long-term orbital control. This study examines this climate variability for northeast Iberia for the time interval 118.9 to 36.9 kyr using a multi-proxy approach (δ18O, δ13C and Mg/Ca) appl...

Full description

Bibliographic Details
Main Authors: Cacho, I. (Author), Cheng, H. (Author), Edwards, R.L (Author), Martín-García, R. (Author), Moreno, A. (Author), Pérez-Mejías, C. (Author), Sancho, C. (Author), Spötl, C. (Author)
Format: Article
Language:English
Published: Elsevier Ltd 2019
Subjects:
Atlantic Ocean
Atlantic Ocean (North)
carbon isotope
Catchments
climate variation
Climatology
foraminifera
Foraminifera
Glacial geology
humid tropics
Iberian Peninsula
Isotopes
Last glacial period
Last Interglacial
marine isotope stage
microbial activity
Oceanography
Orbital-millennial scale
oxygen isotope
precipitation (climatology)
Productivity
proxy climate record
reinforcement
sea level change
Stable isotopes
stalagmite
Stalagmite
Surface discharges
Surface waters
Western mediterranean
Western Mediterranean
Online Access:View Fulltext in Publisher

Internet

View Fulltext in Publisher

Similar Items