FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4311409708> ?p ?o ?g. }

• W4311409708 abstract "<p indent=0mm>Water circulation plays a crucial role in the Earth’s systems, linking the atmosphere, hydrosphere, lithosphere, and biosphere. During the Paleozoic-Mesozoic transition, climatic and environmental conditions turned into crises, caused by a sudden and serious global warming, accompanied by the largest known extinction event of all time. Several studies have been conducted to discover the causes of this notable climate change. Nevertheless, the evolution of water circulation processes during the Paleozoic-Mesozoic transition is still unclear. Several lithologic indicators present in paleoclimate records have been described over the last few decades. Based on these data, we defined climate zones and calculated their area values using Thiessen polygons and Geographic Information System technology to visualize climate evolution during the Paleozoic-Mesozoic transition. Results of a few of the climate simulations showed changes in precipitation and the amplitudes of the inter-tropical convergence zone (ITCZ) seasonal migration. The results showed several changes in water circulation during the late Paleozoic to early Mesozoic. (1) The climate zones reconstructed by sedimentary and paleontological records showed a remarkable arid expansion. The distribution area of evaporites began to expand in the Middle to Late Permian and reached a peak in the Early Triassic, returned to Middle-Late Permian levels in the Middle Triassic, and thereafter continued to narrow during the Late Triassic to Early Jurassic. (2) Global precipitation was higher during the Late Carboniferous and Early Jurassic and lower in the Middle to Late Permian and Early Triassic. Such a “V” shape represents considerable swing. (3) The assembly of Pangea might have led to “giant land surface winds” in Pangaea and “trans-equatorial winds” in the Tethys region, resulting in a global “megamonsoon”. (4) Seasonal movements of the ITCZ were located at lower latitudes from the Silurian to Carboniferous and from the Jurassic to the present, while reaching higher latitudes with large seasonal oscillations during the Permian-Triassic. Depending on the timing of events, these major changes in water circulation coincided with the assembly of Pangaea, the Variscan or Hercynian orogeny, the end of the late Paleozoic ice age, major carbon emissions, and global warming. These factors are closely related to the changes in atmospheric and water circulation during the Paleozoic-Mesozoic transition. The assembly of Pangea redistributed water storage and altered atmospheric circulation and the “megamonsoon”, while the elevation reduction of mountains traversing middle Pangea weakened the resistance of north and south winds. These factors promoted the evolution of a “megamonsoon” with strong seasonal swings of the ITCZ, which led to the expansion of arid zones and reduced precipitation during the Middle and Late Permian. Meanwhile, large carbon emissions and dramatic global warming altered the energy transition within global systems, which influenced atmospheric circulation. In addition, transformations of global plant clades affected the carbon budget and altered water circulation. In summary, strong fluctuations in water circulation were present during the Paleozoic-Mesozoic transition, especially as observed through climate zones, precipitation and runoff, the “monsoon”, and ITCZ. These crucial processes reflect the interaction between the lithosphere, atmosphere, hydrosphere, and biosphere. However, we have limited knowledge of the complete process of water circulation because geological records and climate simulations are extremely imprecise for the Paleozoic-Mesozoic transition. Future research could focus on other water circulation processes, such as the evolution of underground water, reserves, and fluxes of lakes, rather than only precipitation and “monsoons”. Moreover, the upgrade and extension of big data platforms and a larger number of climate simulations should be considered in future studies." @default.
• W4311409708 created "2022-12-26" @default.
• W4311409708 creator A5014347484 @default.
• W4311409708 creator A5019280357 @default.
• W4311409708 creator A5020516263 @default.
• W4311409708 creator A5022521479 @default.
• W4311409708 creator A5034216471 @default.
• W4311409708 creator A5065303096 @default.
• W4311409708 date "2022-12-01" @default.
• W4311409708 modified "2023-09-25" @default.
• W4311409708 title "Evolution and driving mechanisms of water circulation during the late Paleozoic to early Mesozoic" @default.
• W4311409708 cites W1544616175 @default.
• W4311409708 cites W1711607069 @default.
• W4311409708 cites W1922855605 @default.
• W4311409708 cites W1966572506 @default.
• W4311409708 cites W1968621442 @default.
• W4311409708 cites W1971012657 @default.
• W4311409708 cites W1978209045 @default.
• W4311409708 cites W1981316911 @default.
• W4311409708 cites W1982446415 @default.
• W4311409708 cites W1984823613 @default.
• W4311409708 cites W1986500300 @default.
• W4311409708 cites W1988528439 @default.
• W4311409708 cites W2012870613 @default.
• W4311409708 cites W2015681184 @default.
• W4311409708 cites W2020116131 @default.
• W4311409708 cites W2025729644 @default.
• W4311409708 cites W2037013396 @default.
• W4311409708 cites W2037223408 @default.
• W4311409708 cites W2043165162 @default.
• W4311409708 cites W2043746679 @default.
• W4311409708 cites W2049610925 @default.
• W4311409708 cites W2051426779 @default.
• W4311409708 cites W2054593957 @default.
• W4311409708 cites W2073560578 @default.
• W4311409708 cites W2078542443 @default.
• W4311409708 cites W2081829616 @default.
• W4311409708 cites W2082356805 @default.
• W4311409708 cites W2088157811 @default.
• W4311409708 cites W2091143358 @default.
• W4311409708 cites W2091574685 @default.
• W4311409708 cites W2091805937 @default.
• W4311409708 cites W2110714265 @default.
• W4311409708 cites W2127170577 @default.
• W4311409708 cites W2127603986 @default.
• W4311409708 cites W2134131574 @default.
• W4311409708 cites W2138019909 @default.
• W4311409708 cites W2153235590 @default.
• W4311409708 cites W2171789383 @default.
• W4311409708 cites W2181436777 @default.
• W4311409708 cites W2312226480 @default.
• W4311409708 cites W2313928225 @default.
• W4311409708 cites W2480521994 @default.
• W4311409708 cites W2606932046 @default.
• W4311409708 cites W2756470701 @default.
• W4311409708 cites W2775151642 @default.
• W4311409708 cites W2791051032 @default.
• W4311409708 cites W2900974949 @default.
• W4311409708 cites W2903416363 @default.
• W4311409708 cites W2914155918 @default.
• W4311409708 cites W2942555673 @default.
• W4311409708 cites W2965548895 @default.
• W4311409708 cites W2995086571 @default.
• W4311409708 cites W2999219571 @default.
• W4311409708 cites W2999234322 @default.
• W4311409708 cites W3010949495 @default.
• W4311409708 cites W3015313699 @default.
• W4311409708 cites W3044243879 @default.
• W4311409708 cites W3092321905 @default.
• W4311409708 cites W3113176128 @default.
• W4311409708 cites W3120450552 @default.
• W4311409708 cites W3139147700 @default.
• W4311409708 cites W3148203179 @default.
• W4311409708 cites W3161872040 @default.
• W4311409708 cites W3190873826 @default.
• W4311409708 cites W3211851622 @default.
• W4311409708 cites W3214945316 @default.
• W4311409708 cites W3216530127 @default.
• W4311409708 cites W355482922 @default.
• W4311409708 cites W4213045350 @default.
• W4311409708 cites W4232538116 @default.
• W4311409708 cites W4233173901 @default.
• W4311409708 cites W4238409933 @default.
• W4311409708 cites W4239491302 @default.
• W4311409708 cites W4249312230 @default.
• W4311409708 cites W4253461774 @default.
• W4311409708 cites W4255526753 @default.
• W4311409708 cites W4289745731 @default.
• W4311409708 doi "https://doi.org/10.1360/tb-2022-0896" @default.
• W4311409708 hasPublicationYear "2022" @default.
• W4311409708 type Work @default.
• W4311409708 citedByCount "0" @default.
• W4311409708 crossrefType "journal-article" @default.
• W4311409708 hasAuthorship W4311409708A5014347484 @default.
• W4311409708 hasAuthorship W4311409708A5019280357 @default.
• W4311409708 hasAuthorship W4311409708A5020516263 @default.
• W4311409708 hasAuthorship W4311409708A5022521479 @default.
• W4311409708 hasAuthorship W4311409708A5034216471 @default.
• W4311409708 hasAuthorship W4311409708A5065303096 @default.
• W4311409708 hasConcept C109007969 @default.

• next