A stratigrapher’s reflecions on climate change and energy transition

Abstract This article consists of two well-differentiated parts. The first, based on a bibliographic analysis, tries to position this current episode of global warming within the framework of the geological history of climate change. The conclusion is clear and in line with the scientific consensus. Greenhouse gas emissions linked to human actions are the main cause of global warming. Given this situation, we can speculate about the future climate evolution of the “Anthropocene”. Unfortunately, such projections in the scientific literature paint a bleak picture. Paradoxically, future predictions take us back millions of years in geological history, placing humanity in unknown territory. Accordingly, we must ask ourselves what we can do to adjust the global thermostat. A first optimistic reflection is that the very fact that humans are the cause of the problem opens a window of hope. If global warming were due to natural causes linked to astronomical phenomena, to the internal dynamics of the planet, or to its evolution, we could do little or nothing to remedy our current climate situation. However, if we are the main cause of the crisis, we have the capacity to resolve it. This consideration, in turn, leads us to the second part of this article which comprises a series of personal reflections on the nature of the so-called energy transition and its main lines of action.

Authors

Institutions

Publication Details

Journal
Journal of Iberian Geology
Published
2025-02-10
DOI
https://doi.org/10.1007/s41513-025-00282-0
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
0.00

Funders

Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

A stratigrapher’s reflecions on climate change and energy transition

Manuel Carpio
Journal of Iberian Geology
Geology and Paleoclimatology Research
article

A stratigrapher’s reflecions on climate change and energy transition

Manuel Carpio
article en

Abstract

Abstract This article consists of two well-differentiated parts. The first, based on a bibliographic analysis, tries to position this current episode of global warming within the framework of the geological history of climate change. The conclusion is clear and in line with the scientific consensus. Greenhouse gas emissions linked to human actions are the main cause of global warming. Given this situation, we can speculate about the future climate evolution of the “Anthropocene”. Unfortunately, such projections in the scientific literature paint a bleak picture. Paradoxically, future predictions take us back millions of years in geological history, placing humanity in unknown territory. Accordingly, we must ask ourselves what we can do to adjust the global thermostat. A first optimistic reflection is that the very fact that humans are the cause of the problem opens a window of hope. If global warming were due to natural causes linked to astronomical phenomena, to the internal dynamics of the planet, or to its evolution, we could do little or nothing to remedy our current climate situation. However, if we are the main cause of the crisis, we have the capacity to resolve it. This consideration, in turn, leads us to the second part of this article which comprises a series of personal reflections on the nature of the so-called energy transition and its main lines of action.

Journal of Iberian Geology
Universitat de Barcelona (ES)
Universitat de Barcelona
Climate action
Openalex Percentile: Top 98%
Geology and Paleoclimatology Research
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.