Zobrazeno 1 - 10
of 288
pro vyhledávání: '"Noah J. Planavsky"'
Publikováno v:
Frontiers in Climate, Vol 6 (2024)
In an effort to mitigate anthropogenic climate impacts the U.S. has established ambitious Nationally Determined Contribution (NDC) targets, aiming to reduce greenhouse gas emissions by 50% before 2030 and achieving net-zero emissions by 2050. Enhance
Externí odkaz:
https://doaj.org/article/8fd62523d2594ae5a7e35b06cb965573
Autor:
Judith A. Rosentreter, Lewis Alcott, Taylor Maavara, Xin Sun, Yong Zhou, Noah J. Planavsky, Peter A. Raymond
Publikováno v:
Earth's Future, Vol 12, Iss 6, Pp n/a-n/a (2024)
Abstract An accurate quantification of global methane sources and sinks is imperative for assessing realistic pathways to mitigate climate change. A key challenge of quantifying the Global Methane Budget (Saunois et al., 2020, https://doi.org/10.5194
Externí odkaz:
https://doaj.org/article/8243813883494b0ab6ffae2608edf436
Autor:
Tim Jesper Suhrhoff, Tom Reershemius, Jiuyuan Wang, Jacob S. Jordan, Christopher T. Reinhard, Noah J. Planavsky
Publikováno v:
Frontiers in Climate, Vol 6 (2024)
Enhanced weathering (EW) of silicate rocks spread onto managed lands as agricultural amendments is a promising carbon dioxide removal (CDR) approach. However, there is an obvious need for the development of tools for Measurement, Reporting, and Verif
Externí odkaz:
https://doaj.org/article/f056dcfbd8ce4d58913c2ab51786c42b
Autor:
Isabella Chiaravalloti, Nicolas Theunissen, Shuang Zhang, Jiuyuan Wang, Fengchao Sun, Ayesha A. Ahmed, Evelin Pihlap, Christopher T. Reinhard, Noah J. Planavsky
Publikováno v:
Frontiers in Climate, Vol 5 (2023)
Nitrous oxide (N2O) is a potent and long-lived greenhouse gas that accounts for roughly 6% of global anthropogenic greenhouse gas emissions, and it has risen from its preindustrial concentration of 270 ppb N2O to 332 ppb N2O as a result of human acti
Externí odkaz:
https://doaj.org/article/d933fcd5bb9145138852f4ef96526749
Autor:
Terry T. Isson, Shuang Zhang, Kimberly V. Lau, Sofia Rauzi, Nicholas J. Tosca, Donald E. Penman, Noah J. Planavsky
Publikováno v:
Nature Communications, Vol 13, Iss 1, Pp 1-12 (2022)
The widespread disappearance of siliceous life sustained extreme temperatures in the wake of Earth’s most severe mass extinction event.
Externí odkaz:
https://doaj.org/article/a1de382962a54e4aa8d5fdea3658dc57
Publikováno v:
Scientific Reports, Vol 12, Iss 1, Pp 1-9 (2022)
Abstract Earth’s earliest fossils of complex macroscopic life are recorded in Ediacaran-aged siliciclastic deposits as exceptionally well-preserved three-dimensional casts and molds, known as “Ediacara-style” preservation. Ediacara-style fossil
Externí odkaz:
https://doaj.org/article/b6033ef3a71845bf88574bedd7e9096f
Autor:
Jun Shen, Runsheng Yin, Shuang Zhang, Thomas J. Algeo, David J. Bottjer, Jianxin Yu, Guozhen Xu, Donald Penman, Yongdong Wang, Liqin Li, Xiao Shi, Noah J. Planavsky, Qinglai Feng, Shucheng Xie
Publikováno v:
Nature Communications, Vol 13, Iss 1, Pp 1-10 (2022)
The work shows that volcanic-related elevated continental chemical weathering could have played a significant role in global environmental perturbations during the Triassic-Jurassic mass extinction.
Externí odkaz:
https://doaj.org/article/b6599170de6d461f97dcee4ee1fb31aa
Publikováno v:
Scientific Reports, Vol 13, Iss 1, Pp 1-2 (2023)
Externí odkaz:
https://doaj.org/article/a5ee67c1823d41a0933e1a5e060f59c0
Autor:
Weiduo Hao, Kaarel Mänd, Yuhao Li, Daniel S. Alessi, Peeter Somelar, Mathieu Moussavou, Alexander E. Romashkin, Aivo Lepland, Kalle Kirsimäe, Noah J. Planavsky, Kurt O. Konhauser
Publikováno v:
Nature Communications, Vol 12, Iss 1, Pp 1-6 (2021)
Expanded phosphorus availability possibly triggered a marine bioproduction boom after 2.3 billion years ago, but its delivery mechanisms remain unclear. Here we propose a kaolinite shuttle which efficiently adsorbs phosphorus in continental weatherin
Externí odkaz:
https://doaj.org/article/cd36d9f5edad498a876bcb1e49ccae2b
Autor:
Richard G. Stockey, Devon B. Cole, Noah J. Planavsky, David K. Loydell, Jiří Frýda, Erik A. Sperling
Publikováno v:
Nature Communications, Vol 11, Iss 1, Pp 1-10 (2020)
The Late Ordovician mass extinction has been attributed to extended marine anoxia. Here, the authors use a metal isotope mass balance model and find the marine anoxic event lasted over 3 million years, notably longer than the anoxic event associated
Externí odkaz:
https://doaj.org/article/cb6814aa30384c9a9eca2d509be1855f