David Bond's Outputs (56)

A palynological investigation of the Early-Middle Devonian transition and associated Choteč Event in Northern Spain (2024)
Journal Article
Lopes, G., Blanco-Ferrera, S., Bond, D. P., Greene, S. E., Hilton, J., Marshall, J. E., Sanz-López, J., & Wellman, C. H. (2025). A palynological investigation of the Early-Middle Devonian transition and associated Choteč Event in Northern Spain. Review of palaeobotany and palynology, 332, Article 105222. https://doi.org/10.1016/j.revpalbo.2024.105222

In Northern Spain there is a near complete sequence of Devonian rocks that accumulated around a relatively isolated land mass, the Armorican Terrane Assemblage, which was separated from Gondwana to the south and Laurussia to the north. The Lower to M... Read More about A palynological investigation of the Early-Middle Devonian transition and associated Choteč Event in Northern Spain.

Re-evaluating Water Column Reoxygenation during the End Permian Mass Extinction (2024)
Journal Article
Yang, F., Li, S., An, K. Y., Bond, D. P., Ao, R., Wu, X. B., Ma, L. L., & Sun, Y. D. (2024). Re-evaluating Water Column Reoxygenation during the End Permian Mass Extinction. Geochemistry, geophysics, geosystems G³, 25(10), Article e2024GC011779. https://doi.org/10.1029/2024GC011779

Ocean anoxia is considered a key driver of the end-Permian mass extinction (EPME). However, it is much debated whether there was an ocean reoxygenation phase during, and in the aftermath, of the EPME. Evidence for ocean reoxygenation is often inferre... Read More about Re-evaluating Water Column Reoxygenation during the End Permian Mass Extinction.

Mega El Niño instigated the end-Permian mass extinction (2024)
Journal Article
Sun, Y., Farnsworth, A., Joachimski, M. M., Wignall, P. B., Krystyn, L., Bond, D. P., Ravidà, D. C., & Valdes, P. J. (2024). Mega El Niño instigated the end-Permian mass extinction. Science, 385(6714), 1189-1195. https://doi.org/10.1126/science.ado2030

The ultimate driver of the end-Permian mass extinction is a topic of much debate. Here, we used a multiproxy and paleoclimate modeling approach to establish a unifying theory elucidating the heightened susceptibility of the Pangean world to the prolo... Read More about Mega El Niño instigated the end-Permian mass extinction.

The impact of frequent wildfires during the Permian–Triassic transition: Floral change and terrestrial crisis in southwestern China (2024)
Journal Article
Hua, F., Shao, L., Wang, X., Jones, T., Jones, T. P., Zhang, T., Bond, D. P., Yan, Z., & Hilton, J. (2024). The impact of frequent wildfires during the Permian–Triassic transition: Floral change and terrestrial crisis in southwestern China. Palaeogeography, palaeoclimatology, palaeoecology, 641, Article 112129. https://doi.org/10.1016/j.palaeo.2024.112129

Wildfires are considered to have played an important role in the land plants crisis during the Permian–Triassic (P–T) transition. However, the nature and impact of wildfires in the P–T terrestrial crisis remains unclear. Organic petrology data from a... Read More about The impact of frequent wildfires during the Permian–Triassic transition: Floral change and terrestrial crisis in southwestern China.

Marine snowstorm during the Permian-Triassic mass extinction (2023)
Journal Article
Grasby, S. E., Ardakani, O. H., Liu, X., Bond, D. P. G., Wignall, P. B., & Strachan, L. J. (2024). Marine snowstorm during the Permian-Triassic mass extinction. Geology, 52(2), 120-124. https://doi.org/10.1130/G51497.1

The Permian-Triassic mass extinction (PTME) interval is marked by major excursions in both inorganic and organic carbon (C) isotopes. Carbon cycle models predict that these trends were driven by large increases in productivity, yet organic C-rich roc... Read More about Marine snowstorm during the Permian-Triassic mass extinction.

The great catastrophe: causes of the Permo-Triassic marine mass extinction (2023)
Journal Article
Wignall, P. B., & Bond, D. P. G. (2024). The great catastrophe: causes of the Permo-Triassic marine mass extinction. National Science Review, 11(1), Article nwad273. https://doi.org/10.1093/nsr/nwad273

The marine losses during the Permo-Triassic mass extinction were the worst ever experienced. All groups were badly affected, especially amongst the benthos (e.g. brachiopods, corals, bryozoans, foraminifers, ostracods). Planktonic populations underwe... Read More about The great catastrophe: causes of the Permo-Triassic marine mass extinction.

How Large Igneous Provinces Have Killed Most Life on Earth—Numerous Times (2023)
Journal Article
Grasby, S. E., & Bond, D. P. (2023). How Large Igneous Provinces Have Killed Most Life on Earth—Numerous Times. Elements: An International Magazine of Mineralogy, Geochemistry, and Petrology, 19(5), 276-281. https://doi.org/10.2138/gselements.19.5.276

Evolution has not been a simple path. Since the first appearance of complex life, there have been several mass extinctions on Earth. This was exemplified by the most severe event during the Phanerozoic, the end-Permian mass extinction that occurred 2... Read More about How Large Igneous Provinces Have Killed Most Life on Earth—Numerous Times.

Global oceanic anoxia linked with the Capitanian (Middle Permian) marine mass extinction (2023)
Journal Article
Song, H., Algeo, T., Song, H., Tong, J., Wignall, P., Bond, D. P., Zheng, W., Chen, X., Romaniello, S., Wei, H., & Anbar, A. (2023). Global oceanic anoxia linked with the Capitanian (Middle Permian) marine mass extinction. Earth and planetary science letters, 610, Article 118128. https://doi.org/10.1016/j.epsl.2023.118128

The timing and causation of the Capitanian (late Middle Permian) biocrisis remain controversial. Here, a detailed uranium-isotopic (δ238U) profile was generated for the mid-Capitanian to lower Wuchiapingian of the Penglaitan section (the Guadalupian/... Read More about Global oceanic anoxia linked with the Capitanian (Middle Permian) marine mass extinction.

Middle Jurassic terrestrial environmental and floral changes linked to volcanism: Evidence from the Qinghai-Tibet Plateau, China (2023)
Journal Article
Zhang, P., Yang, M., Lu, J., Jiang, Z., Zhou, K., Liu, H., He, Z., Wang, Y., Bian, X., Shao, L., Hilton, J., & Bond, D. P. (2023). Middle Jurassic terrestrial environmental and floral changes linked to volcanism: Evidence from the Qinghai-Tibet Plateau, China. Global and planetary change, 223, Article 104094. https://doi.org/10.1016/j.gloplacha.2023.104094

The breakup of Pangaea and the rapid opening of the Ligurian and Central Atlantic oceans during the Middle Jurassic resulted in widespread volcanism accompanied by significant shifts in global environments, climates, and floras. Although major volcan... Read More about Middle Jurassic terrestrial environmental and floral changes linked to volcanism: Evidence from the Qinghai-Tibet Plateau, China.

End-Permian terrestrial ecosystem collapse in North China: evidence from palynology and geochemistry (2023)
Journal Article
Zhang, P., Yang, M., Lu, J., Bond, D. P., Shao, L., Zhou, K., Xu, X., Xua, X., Wang, Y., He, Z., Bian, X., & Hilton, J. (2023). End-Permian terrestrial ecosystem collapse in North China: evidence from palynology and geochemistry. Global and planetary change, 222, Article 104070. https://doi.org/10.1016/j.gloplacha.2023.104070

The Permian-Triassic Mass Extinction (ca. 252 Ma; PTME) is the most severe biocrisis of the Phanerozoic in both the oceans and on land. The crisis saw the collapse of terrestrial ecosystems in low, mid and high latitudes. Although terrestrial plant l... Read More about End-Permian terrestrial ecosystem collapse in North China: evidence from palynology and geochemistry.

An astronomical timescale for the Permian-Triassic mass extinction reveals a two-step, million-year-long terrestrial crisis in South China (2023)
Journal Article
Hua, F., Shao, L., Zhang, T., Bond, D. P., Wang, X., Wang, J., Yan, Z., Lu, J., & Hilton, J. (2023). An astronomical timescale for the Permian-Triassic mass extinction reveals a two-step, million-year-long terrestrial crisis in South China. Earth and planetary science letters, 605, Article 118035. https://doi.org/10.1016/j.epsl.2023.118035

The Permian-Triassic Mass Extinction (PTME) is the greatest biotic crisis of the Phanerozoic. In terrestrial settings, the PTME appears to have been diachronous and it has been suggested that losses initiated before the marine crisis. We examine orga... Read More about An astronomical timescale for the Permian-Triassic mass extinction reveals a two-step, million-year-long terrestrial crisis in South China.

Rapid marine oxygen variability: Driver of the Late Ordovician mass extinction (2022)
Journal Article
Kozik, N. P., Young, S. A., Newby, S. M., Liu, M., Chen, D., Hammarlund, E., Bond, D. P., Them, T. R., & Owens, J. D. (2022). Rapid marine oxygen variability: Driver of the Late Ordovician mass extinction. Science Advances, 8(46), eabn8345. https://doi.org/10.1126/sciadv.abn8345

The timing and connections between global cooling, marine redox conditions, and biotic turnover are underconstrained for the Late Ordovician. The second most severe mass extinction occurred at the end of the Ordovician period, resulting in ~85% loss... Read More about Rapid marine oxygen variability: Driver of the Late Ordovician mass extinction.

Dynamic ocean redox conditions during the end-Triassic mass extinction: Evidence from pyrite framboids (2022)
Journal Article
Li, J., Song, H., Tian, L., Bond, D. P., Song, H., Du, Y., Zhang, C., Chu, D., Wignall, P. B., & Tong, J. (2022). Dynamic ocean redox conditions during the end-Triassic mass extinction: Evidence from pyrite framboids. Global and planetary change, 218, Article 103981. https://doi.org/10.1016/j.gloplacha.2022.103981

The end-Triassic (∼201 Mya) records one of the five largest mass extinction events of the Phanerozoic. Extinction losses were coincident with large igneous province volcanism in the form of the Central Atlantic Magmatic Province (CAMP) and major carb... Read More about Dynamic ocean redox conditions during the end-Triassic mass extinction: Evidence from pyrite framboids.

Two deep marine oxygenation events during the Permian-Triassic boundary interval in South China: relationship with ocean circulation and marine primary productivity (2022)
Journal Article
Ge, Y., & Bond, D. P. (2022). Two deep marine oxygenation events during the Permian-Triassic boundary interval in South China: relationship with ocean circulation and marine primary productivity. Earth-Science Reviews, 234, Article 104220. https://doi.org/10.1016/j.earscirev.2022.104220

Marine redox conditions through the Permian-Triassic (P-T) boundary interval have been intensively studied in South China with different redox proxies and from different sections. However, the resultant interpretations are inconsistent and sometimes... Read More about Two deep marine oxygenation events during the Permian-Triassic boundary interval in South China: relationship with ocean circulation and marine primary productivity.

Ecological Responses to Climate Change: Using the Common Ragworm (Hediste diversicolor) as an Indicator for Benthic Ecosystems (2022)
Thesis
James, J. Ecological Responses to Climate Change: Using the Common Ragworm (Hediste diversicolor) as an Indicator for Benthic Ecosystems. (Thesis). University of Hull. https://hull-repository.worktribe.com/output/4192688

Climate change is projected to have a negative impact on biodiversity over the next century. Similar drivers of change have been observed in the geological past and were also associated with loss of species, particularly in the marine environment. Th... Read More about Ecological Responses to Climate Change: Using the Common Ragworm (Hediste diversicolor) as an Indicator for Benthic Ecosystems.

Diachronous end-Permian terrestrial ecosystem collapse with its origin in wildfires (2022)
Journal Article
Lu, J., Wang, Y., Yang, M., Zhang, P., Bond, D. P., Shao, L., & Hilton, J. (2022). Diachronous end-Permian terrestrial ecosystem collapse with its origin in wildfires. Palaeogeography, palaeoclimatology, palaeoecology, 594, Article 110960. https://doi.org/10.1016/j.palaeo.2022.110960

The Permian-Triassic Mass Extinction (PTME) is the greatest biodiversity crisis in Earth history and while the marine crisis is increasingly well constrained, the timing and cause(s) of terrestrial losses remain poorly understood. There have been sug... Read More about Diachronous end-Permian terrestrial ecosystem collapse with its origin in wildfires.

Volcanically-Induced Environmental and Floral Changes Across the Triassic-Jurassic (T-J) Transition (2022)
Journal Article
Zhang, P., Lu, J., Yang, M., Bond, D. P., Greene, S. E., Liu, L., Zhang, Y., Wang, Y., Wang, Z., Li, S., Shao, L., & Hilton, J. (2022). Volcanically-Induced Environmental and Floral Changes Across the Triassic-Jurassic (T-J) Transition. Frontiers in ecology and evolution, 10, Article 853404. https://doi.org/10.3389/fevo.2022.853404

The End-Triassic Mass Extinction (ETME) saw the catastrophic loss of ca. 50% of marine genera temporally associated with emplacement of the Central Atlantic Magmatic Province (CAMP). However, the effects of the ETME on land is a controversial topic.... Read More about Volcanically-Induced Environmental and Floral Changes Across the Triassic-Jurassic (T-J) Transition.

Sulfidic anoxia in the oceans during the Late Ordovician mass extinctions – insights from molybdenum and uranium isotopic global redox proxies (2021)
Journal Article
Dahl, T. W., Hammarlund, E. U., Rasmussen, C. M. Ø., Bond, D. P., & Canfield, D. E. (2021). Sulfidic anoxia in the oceans during the Late Ordovician mass extinctions – insights from molybdenum and uranium isotopic global redox proxies. Earth-Science Reviews, 220, Article 103748. https://doi.org/10.1016/j.earscirev.2021.103748

The Late Ordovician Mass Extinction wiped out 85% of animal species in two phases (LOME1 and LOME2). The kill mechanisms for the extinction phases are debated, but deteriorating climate and the expansion of marine anoxia appear to have been important... Read More about Sulfidic anoxia in the oceans during the Late Ordovician mass extinctions – insights from molybdenum and uranium isotopic global redox proxies.

Transient Permian-Triassic euxinia in the southern Panthalassa deep ocean (2021)
Journal Article
Takahashi, S., Strachan, L. J., Yin, R., Wignall, P. B., Bond, D. P., & Grasby, S. E. (in press). Transient Permian-Triassic euxinia in the southern Panthalassa deep ocean. Geology, 49(8), 889-893. https://doi.org/10.1130/G48928.1

Both the duration and severity of deep-water anoxic conditions across the Permian-Triassic mass extinction (PTME) are controversial. Panthalassa Ocean circulation models yield varying results, ranging from a well-ventilated deep ocean to rapidly deve... Read More about Transient Permian-Triassic euxinia in the southern Panthalassa deep ocean.

Global warming and mass extinctions associated with large igneous province volcanism (2021)
Book Chapter
Bond, D. P., & Sun, Y. (2021). Global warming and mass extinctions associated with large igneous province volcanism. In R. E. Ernst, A. J. Dickson, & A. Bekker (Eds.), Large Igneous Provinces: A Driver of Global Environmental and Biotic Changes (83-102). American Geophysical Union. https://doi.org/10.1002/9781119507444.ch3

The coincidence of large igneous province (LIP) eruptions with at least three, if not all, of the Big Five biotic crises of the Phanerozoic implies that volcanism is a key driver of mass extinctions. Many LIP-induced extinction scenarios invoke globa... Read More about Global warming and mass extinctions associated with large igneous province volcanism.