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Home , Ireviken event, Telychian

Cyclo and chemostratigraphic characteristics of the Middle in Gotland, Sweden M.C.M. Arts1, B. Cramer2, M. Calner3, C. M.Ø. Rasmussen4 5, A. M. Bancroft5, S. C. Oborny2, E. Hartke2, E. Biebesheimer2, A.C. Da Silva1 3Lithosphere and Biosphere Science, Lund University, Sweden 1 Sedimentary Petrology, Geology Department, Liège University, Belgium 4Natural History Museum of Denmark, University of Copenhagen, Denmark corresponding author: [email protected] 5GLOBE Institute, University of Copenhagen, Denmark 2 Earth and Environmental Sciences, University of Iowa, U.S.A. 6Indiana Geological Survey, University of Indiana, U.S.A Introduction The cumulative work of geoscientists over the past decades has shown that the Silurian Period which was once thought as warm and climatically stable time interval is in fact punctuated by numerous paleoenvironmental perturbations or events. These Silurian events follow a similar pattern where a minor event precedes a substantial carbon isotope excursion (Jeppsen 2000 &1997). Many theories have been brought forward to explain these events ranging from glaciations, to changes in precipitations patterns, ocean currents, volcanism induced ocean anoxia and SEDEX deposit formation. Constraints on the duration and timing of these extinction events and subsequent positive carbon isotope excursions are weak, which hampers a full understanding of the processes at play. The Altajme well drilled in South Central Gotland in Sweden in 2015 spans the latest to succession of Gotland. The data from theAltajme core provides us with a unique opportunity to look at two of these climatic perturbations during the Silurian. The Altajme core spans both the event and the Homerian Mulde event. The Altajme core dataset includes a litholog, high-resolution δ13C data, correlated bentonites with U-Pb dates and a highresolution XRF core scan: important data required for and integrated stratigraphic study. A new high resolution (0.5-1cm resolution) XRF-dataset was gathered in December 2019 constituting of the elements: Al, Si, P, S, Cl, Ar, K, Ca, Ti, V, Cr, Mn, Fe, Co, Ni, Cu, Zn, Ge, As, Se, Br, Rb, Sr, Y, Zr, Nb, Mo, Pd, Ag, Cd, In, Ba, Nd, Eu, Pb and U. The U-Pb-dated bentonites give us age constraints. The δ13C data in combination with the high resolution XRF scan XRF Aluminiun gives us insights into the changes in the ocean before during and after the events, while the XRF data is 800 also used to give cyclostratigraphic age constraints for the events and for the whole core. This stratigraphic 600 study will provide us with a palaeoclimatological insights to explain these two events and provide us with a cyclostratigraphy based age model for the Middle Silurian. 400

58°N Hangvar Fm. 200 Al (ppm) A B Tofta Fm. N ELLESMERIAN Högklint Fm. 0 50 100 150 200 250 300 350 10o depth (metres) Lower Visby Fm. oup 6 Upper Visby Fm. r 4 Mulde Excursion Visby Slite G N Halla Fm. 2 13C Ireviken

δ 0 20 km Excursion EDONIAN B Altajme -2 L Fröjel Fm. Fröjel Han./Tof. U. & L Visby CAL 19°E o g Fm. Klinteberg Fm. Halla Fm. Slite Group 20 Fm. Hög. Fm. Strat. Fm. Klinteber C ALACHIAN P P A Gotland 60°N Litho. o 0 50 100 150 200 250 300 350 40 57°N Gotland depth (metres) Modified after Cramer et, al. 2012 18°E 20°E Investigated section A. Silurian paleogeography Homerian ? Sheinwoodian Rh. Hir. B. Geological map of Gotland, with the Altajme well location as red dot Wenlock Llandovery Up. C. Map of Northern Europe with Gotland Silurian Ord. Chemostratigraphy Cyclostratigraphy To provide insights into the paleoclimatological To asses the presence of orbital cycles the Wavelet spectrum role of different elements a Principle Component XRF Aluminium record was analyzed using C. the R Astrochron and Biwavelet packages 3.3e4 Analysis was conducted using the FactoMineR spectral power

Period (metres) 1 (Le et al., 2008) function from R. The results (A) (Meyers 2014 and Gouhier T.C. et al.,). 1.0e3 show that Dim 1 and 2 cover almost 50% of the precession 4 3.2e2 variance and that 3 clusters can be defined: As indicated by Barnes. et al. (2019) the obliquity 1 Cluster 1: detrital elements core contains 3 U/Pb dated bentonites: 100ky eccentricity 16 Cluster 2: carbonate associated elements Ireviken 281.5m 431.83Ma +/- 0.23, 3.1e-2 Grotlingbo: 134m 428.45 Ma +/- 0.35 405ky eccentricity Cluster 3: Chalcophile/low oxygen elements 9.8e-4 and Djupvik: 62.9m 428.06Ma +/- 0.35. 64 The 281.5-134m interval has an average 3.1e-5 Aluminium a detrital element is selected for the 256 tuning. Gotland was located In mid to lower sedimenation rate of ~4cm/kyr and the 0 50 100 150 200 250 300 latitudes during the Silurian. Higher summer 134-62.9m interval has an average depth (metres) insolation should lead to higher precipitation sedimentation rate of ~19cm/kyr. The bentonite data supports

and thus higher aluminium values thus a maxima EHA: EHA: EHA: spectral power normalized in the 405-kyr filtered aluminium record should our identification of D. Harmonic F-test (1) Harmonic F-test (2) Harmonic F-test (3) correspond to a 405-kyr eccentrcity maxima. precession, obliquity, 1 1 320 1 long and short depth (metres) 280 eccentricity in the 200 The XRF chemostratigraphic record also 0.8 260 0.8300 0.8 shows enrichments in P, Mn, Zn, S, Ba wavelet spectra (C). 0.6 240 0.6 and Pb at and and during the onset of the 280 0.6 A. 150 220 carbon isotope excursions (B). Elemental The stable 405kyr 0.4 200 0.4 0.4 enrichments before carbon isotope excursions could be associated with volcanic events but as indicated in eccentrcity cycle can 260 100 0.2 Emsbo. (2017) the elemental enrichment of P, Mn, Zn, S, Ba and Pb could also be indicative of the formation of be used to create a 0.2 180 0.2 floating time scale for 240 Sedimentary exhalative deposits (SEDEX). The pre-excursion extinction and excursion could be due to a release 0 160 0 0 of SEDEX brines into the ocean. the (Laskar et Mn Zn S Ba Pb 0.008 0.02 0.02 0.12 0.5 P al., 2004). The 405kyr 0.15 10000 20000 30000 40000 50000 10000 15000 20000 25000 (ppm) 10000 (ppm) (ppm) 10000 (ppm)20000 30000 (ppm) Frequency (cycles/metre) 2000 4000 6000 8000 (ppm) 1000 2000 3000 4000 cycle was traced in the Black dotted lines are 405-kyr cycle traced in spectra 20 40 60

-2 δ13C Litholog 0 2 4 6 EHA windowed spectra (D). Three different sized y

0 0 0 0 0 0 0 windows with overlap in the depth domain were used k Sedimentation rate from EHA / 30

to account for the large changes in sedimenation rate m

c 25

in the Altajme core and provide a complete trace of e

t 20

the 405-kyr cycle in the depht domain. The traced a r 50 50 50 50 50 50 50 15 EHA results are combined and converted to a n Mulde o i 10 EHA based composite sedimentation rate (E). t Excursion a

t 5

The sedimentation rate is used to convert from the n

e 0 100 100 100 100 100 100 100 depth to the time domain (F). m 0 50 100 150 200 250 300 350 i

d depth (m) e

The duration of the is 5*405-kyr S Red lines are mayor formation/lithological boundaries Left to right shale ->marl ->carbonate Depth (metres) eccentricity cycles giving a duration of 2.025Myr E. 150 150 150 150 150 150 150 for the whole event. The steep rise in δ13C values at the onset of both events shows us that the largest rise in δ13C occured in a only very short interval. The short timespan indicates that the processes which lead to the environmental pertubation which created the Mulde and Ireviken excursions was formed by a pulse like short event. 200 200 200 200 200 200 200 1.5 Al based Tuning Altajme core F. 6 1.0 250 250 4 250 Ireviken 250 250 250 250 Excursion 0.5 2

300 300 300 300 300 300 300 δ13C (promille) -1000 0 1000 2000 3000 4000 5000 6000 7000 8000 9000 Al Al 405ky -0.5 -2 d13C Normalized Al. values 350 350 350 350 350 350 350 B. (filtered and unfiltered) floating age (in kyrs) Conclusions References

A new cyclostratigraphy based age model for the Telychian to Homerian of Gotland is presented. The duration Barnes. L., Trayler R. B., Cramer B. D., Calner M., Bancroft A. M., Oborny S.C., Jeppsson, Lennart & Calner, Mikael. (2002). The Silurian Mulde Event and a (2019) A Bayesian Age-Depth Model for the Silurian Altajme Core, Gotland, Sweden. scenario for secundo–secundo events. Earth and Environmental Science of the Ireviken event is 2.025Myrs eg. 5*405-kyr eccentricity cycle. The steep rises in δ13C values indicate that 10.1130/abs/2019AM-337871. Transactions of the Royal Society of Edinburgh. 93. 135 - 154. 10.1017/S0263593300000377. the largest rise in δ13C occured in a event like paced timespan. Cramer, & Condon, Daniel & Söderlund, Ulf & Marshall, & Worton, & Thomas, Alan & Calner, Mikael & Ray, David & Perrier, Vincent & Boomer, & Patchett, & Jeppsson,. Laskar J., Robutel P., Joutel F., Gastineau M., Correia A. C. M., and Levrard B. The enrichments of P, Mn, Zn, S, Ba and Pb before and during the excursions indicate that the δ13C (2012). U-Pb (zircon) age constraints on the timing and duration of Wenlock (Silurian) A&A, 428 1 (2004) A long-term numerical solution for the insolation quantities of the paleocommunity collapse and recovery during the ‘Big Crisis’. Geological Society of Earth, 261-285 DOI: https://doi.org/10.1051/0004-6361:20041335 excursions might be the result of a sudden release of SEDEX brines into the ocean. America Bulletin. 124. 1841-1857. 10.1130/B30642.1. Le, S., Josse, J. & Husson, F. (2008). FactoMineR: An R Package for Multivariate Emsbo P., (2017). Sedex brine expulsions to Paleozoic basins may have changed Analysis. Journal of Statistical Software. 25(1). pp. 1-18. global marine 87Sr/86Sr values, triggered anoxia, and initiated mass , 86. http://www.jstatsoft.org/v25/i01/ 474-486. https://doi.org/10.1016/j.oregeorev.2017.02.031 \. Acknowledgments Meyers, S.R. (2014). Astrochron: An R Package for Astrochronology. https://cran.r- Gouhier T. C., Grinsted. A., Viliam S., https://CRAN.R-project.org/package=biwavelet project.org/package=astrochron Jeppsson, L (1997). "The anatomy of the Mid-Early Silurian Ireviken Event and a scenario for P-S events". In Brett, C.E.; Baird, G.C. (eds.). Paleontological Events: This poster is made with support of FNRS grant FNRS.PDRT.T.0051.19. Stratigraphic, Ecological, and Evolutionary Implications. New York: Columbia This poster is a contribution to IGCP-652 “Reading Geologic time in Paleozoic Sedimentary rocks” University Press. pp. 451–492.