Climate-forced Hg-remobilization driving mutagenesis in ferns in the aftermath of the end-Triassic extinction DOI Creative Commons
Remco Bos, Wang Zheng, Sofie Lindström

et al.

Research Square (Research Square), Journal Year: 2023, Volume and Issue: unknown

Published: Oct. 16, 2023

Abstract The long-term effects of the Central Atlantic Magmatic Province (CAMP), a large igneous province connected to end-Triassic mass-extinction (201.5 Ma), remain largely elusive. Here, we document persistence volcanic-induced mercury pollution and its on biosphere for 2 million years after extinction event. In sediments recovered in Germany (Schandelah-1 core), record not only high abundances malformed fern spores at Triassic-Jurassic boundary, but also during Hettangian, indicating repeated vegetation disturbance environmental stress that was eccentricity forced. Crucially, these correspond spikes sedimentary Hg concentrations. Hg-isotope ratios (δ202Hg, Δ199Hg) indicate volcanic source boundary terrestrial early Jurassic peaks. We conclude injected by CAMP across repeatedly remobilized from coastal wetlands hinterland areas eccentricity-forced phases severe hydrological upheaval erosion, focusing Hg-pollution shallow marine basins.

Language: Английский

The terrestrial end-Permian mass extinction in the paleotropics postdates the marine extinction DOI Creative Commons
Qiong Wu, Hua Zhang, Jahandar Ramezani

et al.

Science Advances, Journal Year: 2024, Volume and Issue: 10(5)

Published: Jan. 31, 2024

The end-Permian mass extinction was the most severe ecological event during Phanerozoic and has long been presumed contemporaneous across terrestrial marine realms with global environmental deterioration triggered by Siberian Traps Large Igneous Province. We present high-precision zircon U-Pb geochronology chemical abrasion-isotope dilution-thermal ionization spectrometry technique on tuffs from to transitional coastal settings in Southwest China, which reveals a protracted collapse of Cathaysian rainforest beginning after onset extinction. Integrated high-resolution coeval successions, our results suggest that occurred diachronously latitude, at high latitudes late Changhsingian progressing tropics early Induan, spanning duration nearly 1 million years. This latitudinal age gradient may have related variations surface warming more degraded conditions higher contributing rates.

Language: Английский

Citations

13

Sixteen mass extinctions of the past 541 My correlated with 15 pulses of Large Igneous Province (LIP) volcanism and the 4 largest extraterrestrial impacts DOI
Michael R. Rampino,

K. Caldeira,

Sedelia Rodriguez

et al.

Global and Planetary Change, Journal Year: 2024, Volume and Issue: 234, P. 104369 - 104369

Published: Feb. 8, 2024

Language: Английский

Citations

9

Functional traits of fossil plants DOI Creative Commons
Jennifer C. McElwain, William J. Matthaeus, Catarina Barbosa

et al.

New Phytologist, Journal Year: 2024, Volume and Issue: 242(2), P. 392 - 423

Published: Feb. 26, 2024

A minuscule fraction of the Earth's paleobiological diversity is preserved in geological record as fossils. What plant remnants have withstood taphonomic filtering, fragmentation, and alteration their journey to become part fossil provide unique information on how plants functioned paleo-ecosystems through traits. Plant traits are measurable morphological, anatomical, physiological, biochemical, or phenological characteristics that potentially affect environment fitness. Here, we review rich literature paleobotany, lens contemporary trait-based ecology, evaluate which well-established extant hold greatest promise for application In particular, focus functional traits, those properties leaf, stem, reproductive, whole fossils offer insights into functioning when alive. The limitations a approach paleobotany considerable. However, our critical assessment over 30 present an initial, semi-quantitative ranking 26 paleo-functional based methodological criteria potential impact Earth system processes, be quantifiable. We demonstrate valuable inferences paleo-ecosystem processes (pollination biology, herbivory), past nutrient cycles, paleobiogeography, paleo-demography (life history), history can derived plants.

Language: Английский

Citations

9

How Large Igneous Provinces Have Killed Most Life on Earth—Numerous Times DOI Open Access
Stephen E. Grasby, David P.G. Bond

Elements, Journal Year: 2023, Volume and Issue: 19(5), P. 276 - 281

Published: Oct. 1, 2023

Evolution has not been a simple path. Since the first appearance of complex life, there have several mass extinctions on Earth. This was exemplified by most severe event during Phanerozoic, end-Permian extinction that occurred 252 million years ago and saw loss 90% 70% all marine terrestrial species, respectively. Such entirely reset ecosystems. Increasing evidence points to massive eruption crustal emplacement magmas associated with large igneous provinces (LIPs) as key drivers these events. Understanding how LIP events disrupted global biogeochemical cycles is prime importance, especially humans alter atmosphere biosphere today. We explore cascading impacts climate, oceans, land—including runaway greenhouses, release toxic metals environment, destruction ozone layer, oceans are driven anoxic acidic states—all which parallels in consequences modern industrialisation.

Language: Английский

Citations

20

Climate-forced Hg-remobilization associated with fern mutagenesis in the aftermath of the end-Triassic extinction DOI Creative Commons
Remco Bos, Wang Zheng, Sofie Lindström

et al.

Nature Communications, Journal Year: 2024, Volume and Issue: 15(1)

Published: April 27, 2024

Abstract The long-term effects of the Central Atlantic Magmatic Province, a large igneous province connected to end-Triassic mass-extinction (201.5 Ma), remain largely elusive. Here, we document persistence volcanic-induced mercury (Hg) pollution and its on biosphere for ~1.3 million years after extinction event. In sediments recovered in Germany (Schandelah-1 core), record not only high abundances malformed fern spores at Triassic-Jurassic boundary, but also during lower Jurassic Hettangian, indicating repeated vegetation disturbance stress that was eccentricity-forced. Crucially, these correspond increases sedimentary Hg-concentrations. Hg-isotope ratios (δ 202 Hg, Δ 199 Hg) suggest volcanic source Hg-enrichment boundary terrestrial early peaks. We conclude volcanically injected Hg across repeatedly remobilized from coastal wetlands hinterland areas eccentricity-forced phases severe hydrological upheaval erosion, focusing Hg-pollution European Basin.

Language: Английский

Citations

7

Mega El Niño instigated the end-Permian mass extinction DOI
Yadong Sun,

Alexander Farnsworth,

Michael M. Joachimski

et al.

Science, Journal Year: 2024, Volume and Issue: 385(6714), P. 1189 - 1195

Published: Sept. 12, 2024

The ultimate driver of the end-Permian mass extinction is a topic much debate. Here, we used multiproxy and paleoclimate modeling approach to establish unifying theory elucidating heightened susceptibility Pangean world prolonged intensified El Niño events leading an state. As atmospheric partial pressure carbon dioxide doubled from about 410 860 ppm (parts per million) in latest Permian, meridional overturning circulation collapsed, Hadley cell contracted, Niños intensified. resultant deforestation, reef demise, plankton crisis marked start cascading environmental disaster. Reduced sequestration initiated positive feedback, producing warmer hothouse and, consequently, stronger Niños. compounding effects elevated climate variability mean state warming led catastrophic but diachronous terrestrial marine losses.

Language: Английский

Citations

7

Platinum-group elements (PGEs) and rhenium in Permian-Triassic boundary sediments from southern China and Japan linked to concurrent eruptions of the Siberian Traps DOI

Monika Misztela,

Michael R. Rampino, I. H. Campbell

et al.

Chemical Geology, Journal Year: 2025, Volume and Issue: unknown, P. 122715 - 122715

Published: March 1, 2025

Language: Английский

Citations

0

Environmental & health impacts of ultraviolet radiation: current trends and mitigation strategies DOI Creative Commons
Gideon Sadikiel Mmbando, Kelvin Ngongolo

Discover Sustainability, Journal Year: 2024, Volume and Issue: 5(1)

Published: Nov. 26, 2024

Contrary to the conventional wisdom and practices moderate non-burning ultraviolet (UV) radiation may be beneficial our existence, but ecosystems human health are seriously threatened by rise in UV from ozone layer loss climate change. Nevertheless, there is less current information on environmental effects of elevated stress. This review looks at patterns levels today emphasizes causes, which include anthropogenic activities ozone. With a focus physiological, cellular, ecological mechanisms, environment, wildlife, aquatic terrestrial ecosystems, thoroughly discussed. Various mitigation tactics, such as technological ones like UV-protective materials, biological breeding UV-resistant species, policy public education international agreements, discussed here. provides thorough understanding potential techniques combining these various strategies. study crucial that will help protect against harmful environment health.

Language: Английский

Citations

3

Atmospheric ozone destruction and the end-Permian crisis: Evidence from multiple sulfur isotopes DOI
Rucao Li, Shu‐zhong Shen, Xiaoping Xia

et al.

Chemical Geology, Journal Year: 2024, Volume and Issue: 647, P. 121936 - 121936

Published: Jan. 11, 2024

Language: Английский

Citations

3

A Fossil Record of Spores before Sporophytes DOI Creative Commons
Paul K. Strother,

Wilson A. Taylor

Diversity, Journal Year: 2024, Volume and Issue: 16(7), P. 428 - 428

Published: July 22, 2024

Because their resistant, sporopolleninous walls preserve a record of morphogenetic change during spore formation, fossil cryptospores provide direct physical the evolution sporogenesis algal–plant transition. That transition itself is story development—it not about phylogeny. Here, we review terrestrially derived spore/cryptospore assemblages and attempt to place these microfossils in evolutionary context with respect origin complex multicellularity plants. Cambrian show features related karyokinesis seen extant charophytes, but they also possess ultrastructure similar that liverworts today. Dyadospora, cryptospore dyad recovered from sporangia Devonian embryophytes, first occurs earliest Ordovician. Tetrahedraletes, likely precursor trilete spore, Middle These fossils correspond novelties were acquired period genome assembly prior existence upright, axial sporophytes. The cryptospore/spore provides temporal scaffold for acquisition novel characters relating plant Cambrian–Silurian interval.

Language: Английский

Citations

2