M Fernández-García
Biographic Data
| ID | 148545 |
|---|---|
| NAME | M Fernández-García |
| GIVEN NAMES | M |
| FAMILY NAME | Fernández-García |
| SIGNATURE | FERNÁNDEZ-GARCÍA M |
| AFFILIATIONS | Universidad de Cantabria |
| ORCID | 0000-0001-9301-6877 |
| VERIFIED | Yes |
| TOTAL WORKS | 8 |
| TOTAL CITATIONS | 21 |
| AUTHOR COUNT | 8 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2020 |
| LATEST PUBLICATION YEAR | 2026 |
| H-INDEX | 3 |
Bone collagen hydrogen isotopes as tracers of local palaeoclimate
Hydrogen stable isotopes (δ 2 H) preserved in bone collagen have been proposed as a promising proxy for palaeoclimatic reconstruction, though empirical applications remain limited. To evaluate the reliability and scope of this approach, we performed a multiisotopic analysis (δ 13 C, δ 15 N, δ 34 S, and δ 2 H) on 50 herbivore bone samples collected from three archaeostratigraphic layers spanning the Aurignacian sequence of Isturitz Cave (France). …
Neanderthal landscapes in southern Europe
Synanthropy of the Isturitz foxes during the Aurignacian is not proven
Aurignacian groups at Isturitz (France) adapted to a shifting environment upon their arrival in Western Europe ∼42,000 years ago
The Marine Isotope Stage 3 is a context of considerable climatic instability. Establishing the link between global climate changes and their impact on the local ecological contexts and prey exploited by human populations is challenging. Still, it is necessary to understand better the local conditions where humans lived to unravel how they adapted to fluctuating environmental conditions. Here, we address this question by studying 250 osteodental e…
Ecological evolution in northern Iberia (SW Europe) during the Late Pleistocene through isotopic analysis on ungulate teeth
During the Late Pleistocene, stadial and interstadial fluctuations affected vegetation, fauna, and human groups that were forced to cope with these pronounced climatic and environmental changes in time and space. These changes were especially abrupt during the Marine Isotopic Stage (MIS) 3. However, little is still known about the local and regional climatic conditions experienced by hominins in Europe. Here we reconstruct the climatic trends in …
New insights in Neanderthal palaeoecology using stable oxygen isotopes preserved in small mammals as palaeoclimatic tracers in Teixoneres Cave (Moià, northeastern Iberia)
The northeastern region of Iberia constitutes a natural pass-area for arriving populations into the peninsula and becomes a key area to understand Neanderthal resilience to changing environmental conditions experienced during Marine Isotope Stage 3 (MIS 3; 60-30 ka). Short-term but repeated occupations by Neanderthal groups occurred in Teixoneres Cave (Moià, Barcelona) in alternation with large and small carnivores during MIS3. Abundant small-mam…
Elucidating anuran accumulations
The Koskobilo (Olazti, Navarre, Northern Iberian Peninsula) paleontological collection
New insights in Neanderthal palaeoecology using stable oxygen isotopes preserved in small mammals as palaeoclimatic tracers in Teixoneres Cave (Moià, northeastern Iberia)
The northeastern region of Iberia constitutes a natural pass-area for arriving populations into the peninsula and becomes a key area to understand Neanderthal resilience to changing environmental conditions experienced during Marine Isotope Stage 3 (MIS 3; 60-30 ka). Short-term but repeated occupations by Neanderthal groups occurred in Teixoneres Cave (Moià, Barcelona) in alternation with large and small carnivores during MIS3. Abundant small-mam…
The Koskobilo (Olazti, Navarre, Northern Iberian Peninsula) paleontological collection
Aurignacian groups at Isturitz (France) adapted to a shifting environment upon their arrival in Western Europe ∼42,000 years ago
The Marine Isotope Stage 3 is a context of considerable climatic instability. Establishing the link between global climate changes and their impact on the local ecological contexts and prey exploited by human populations is challenging. Still, it is necessary to understand better the local conditions where humans lived to unravel how they adapted to fluctuating environmental conditions. Here, we address this question by studying 250 osteodental e…
Elucidating anuran accumulations
The Koskobilo (Olazti, Navarre, Northern Iberian Peninsula) paleontological collection
New insights in Neanderthal palaeoecology using stable oxygen isotopes preserved in small mammals as palaeoclimatic tracers in Teixoneres Cave (Moià, northeastern Iberia)
The northeastern region of Iberia constitutes a natural pass-area for arriving populations into the peninsula and becomes a key area to understand Neanderthal resilience to changing environmental conditions experienced during Marine Isotope Stage 3 (MIS 3; 60-30 ka). Short-term but repeated occupations by Neanderthal groups occurred in Teixoneres Cave (Moià, Barcelona) in alternation with large and small carnivores during MIS3. Abundant small-mam…
Ecological evolution in northern Iberia (SW Europe) during the Late Pleistocene through isotopic analysis on ungulate teeth
During the Late Pleistocene, stadial and interstadial fluctuations affected vegetation, fauna, and human groups that were forced to cope with these pronounced climatic and environmental changes in time and space. These changes were especially abrupt during the Marine Isotopic Stage (MIS) 3. However, little is still known about the local and regional climatic conditions experienced by hominins in Europe. Here we reconstruct the climatic trends in …
Synanthropy of the Isturitz foxes during the Aurignacian is not proven
Aurignacian groups at Isturitz (France) adapted to a shifting environment upon their arrival in Western Europe ∼42,000 years ago
The Marine Isotope Stage 3 is a context of considerable climatic instability. Establishing the link between global climate changes and their impact on the local ecological contexts and prey exploited by human populations is challenging. Still, it is necessary to understand better the local conditions where humans lived to unravel how they adapted to fluctuating environmental conditions. Here, we address this question by studying 250 osteodental e…
Bone collagen hydrogen isotopes as tracers of local palaeoclimate
Hydrogen stable isotopes (δ 2 H) preserved in bone collagen have been proposed as a promising proxy for palaeoclimatic reconstruction, though empirical applications remain limited. To evaluate the reliability and scope of this approach, we performed a multiisotopic analysis (δ 13 C, δ 15 N, δ 34 S, and δ 2 H) on 50 herbivore bone samples collected from three archaeostratigraphic layers spanning the Aurignacian sequence of Isturitz Cave (France). …
Neanderthal landscapes in southern Europe
Cave (6 works) · Pleistocene-Era Hominins and Archaeology (6 works) · Geography (5 works) · Archaeology (4 works) · Aurignacian (4 works) · Biology (4 works) · Ecology (4 works) · Evolution and Paleontology Studies (4 works) · Geology and Paleoclimatology Research (4 works) · Archaeology and ancient environmental studies (3 works)