Nitrogen‐based symbioses, phosphorus availability, and accounting for a modern world more productive than the Paleozoic. Issue 1 (10th August 2022)

• Record Type: Journal Article
• Authors: Boyce, C. Kevin; Ibarra, Daniel E.; Nelsen, Matthew P.; D'Antonio, Michael P.
• Is Part Of: Geobiology. Volume 21:Issue 1(2023)
• Page Start: 86
• Page End: 101
• Publication Date: 2022-08-10
• Subjects: angiosperms -- carbon cycle -- coal -- ectomycorrhizae -- lichens -- rock cycle -- symbiosis -- weathering; Geobiology -- Periodicals; Biogeochemistry -- Periodicals; Ecology -- Periodicals; 551
• DOI: 10.1111/gbi.12519
• Languages: English
• ISSNs: 1472-4677

Abstract

Abstract: Evolution of high‐productivity angiosperms has been regarded as a driver of Mesozoic ecosystem restructuring. However, terrestrial productivity is limited by availability of rock‐derived nutrients such as phosphorus for which permanent increases in weathering would violate mass balance requirements of the long‐term carbon cycle. The potential reality of productivity increases sustained since the Mesozoic is supported here with documentation of a dramatic increase in the evolution of nitrogen‐fixing or nitrogen‐scavenging symbioses, including more than 100 lineages of ectomycorrhizal and lichen‐forming fungi and plants with specialized microbial associations. Given this evidence of broadly increased nitrogen availability, we explore via carbon cycle modeling how enhanced phosphorus availability might be sustained without violating mass balance requirements. Volcanism is the dominant carbon input, dictating peaks in weathering outputs up to twice modern values. However, times of weathering rate suppression may be more important for setting system behavior, and the late Paleozoic was the only extended period over which rates are expected to have remained lower than modern. Modeling results are consistent with terrestrial organic matter deposition that accompanied Paleozoic vascular plant evolution having suppressed weathering fluxes by providing an alternative sink of atmospheric CO2 . Suppression would have then been progressively lifted as the crustal reservoir's holding capacity for terrestrial organic matter saturated back toward steady state with deposition of new organic matter balanced by erosion of older organic deposits. Although not an absolute increase, weathering fluxes returning to early Paleozoic conditions would represent a novel regime for the complex land biota that evolved in the interim. Volcanism‐based peaks in Mesozoic weathering far surpass the modern rates that sustain a complex diversity of nitrogen‐based symbioses; only in the late Paleozoic might these ecologies have been suppressed by significantly lower rates. Thus, angiosperms are posited to be another effect rather than proximal cause of Mesozoic upheaval.