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1

Gabdullin, R. R., N. V. Badulina, and A. V. Ivanov. "Astroclimatic benchmarks of stratigraphic correlation for Neogene-Quaternary deposits." Moscow University Bulletin Series 4 Geology, no. 6, 2024 (2024): 61–71. https://doi.org/10.55959/msu0579-9406-4-2024-63-6-61-71.

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An astrochronological (cyclostratigraphic) binding of the lithological and geochemical characteristics of the Neogene-Quaternary sediments of the sections to the Milankovich cycles (eccentricity, inclination of the ecliptic, precession) was carried out, an analysis of the relationship between the established variations of climate and paleotemperature with the moments of coincidence of different Milankovich cycles was given, a possible limit of the method of high-precision planetary correlation was determined. Correlation markers for the method of high-precision planetary correlation of precipi
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2

Pomortsev, O. A., V. R. Filippov, and S. S. Rozhin. "Transgressive Pleistocene Cycles and Their Place on the Milankovich Scale." IOP Conference Series: Earth and Environmental Science 666, no. 3 (2021): 032068. http://dx.doi.org/10.1088/1755-1315/666/3/032068.

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3

Michael Oldfield Jonas. "The inter-glacial cycle is not a 100,000-year cycle, it is a shorter cycle with missing beats." World Journal of Advanced Research and Reviews 13, no. 3 (2022): 388–92. http://dx.doi.org/10.30574/wjarr.2022.13.3.0259.

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The "100,000-year problem" refers to an apparent unexplained change in the frequency of inter-glacial periods which occurred about a million years ago. Before that, inter-glacial periods seemed to occur about every 41,000 years, in line with the obliquity Milankovich cycle. But after that, they seemed to occur about every 100,000 years, in line with the orbital inclination Milankovich cycle. Examination of the data shows that there never was a 41,000-year cycle, and that there is no 100,000-year cycle, but that the most influential cycle is the approx 21,000-year precession cycle which is the
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4

Michael, Oldfield Jonas. "The inter-glacial cycle is not a 100,000-year cycle, it is a shorter cycle with missing beats." World Journal of Advanced Research and Reviews 13, no. 3 (2022): 388–92. https://doi.org/10.5281/zenodo.6413979.

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The "100,000-year problem" refers to an apparent unexplained change in the frequency of inter-glacial periods which occurred about a million years ago. Before that, inter-glacial periods seemed to occur about every 41,000 years, in line with the obliquity Milankovich cycle. But after that, they seemed to occur about every 100,000 years, in line with the orbital inclination Milankovich cycle. Examination of the data shows that there never was a 41,000-year cycle, and that there is no 100,000-year cycle, but that the most influential cycle is the approx 21,000-year precession cycle whi
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5

Pomortsev, O. A. "The response of rhythmically forming processes to the latitudinal position of the zones of their implementation." Vestnik of North-Eastern Federal University Series "Earth Sciences", no. 3 (September 21, 2023): 35–41. http://dx.doi.org/10.25587/svfu.2023.31.3.005.

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The problem of variability of the Milankovich scale and cyclic oscillations in the troposphere circulation mode depending on the geographical latitude of the area is investigated. Parallels in the dynamics of multi-thousand-year and intra-century climate cycles in different latitudinal zones and possible causes of this phenomenon are considered. New data on the influence of axial rotation and the shape of the Earth on the structure of rhythm-forming processes are presented. It is established that the zone with a high frequency of pulsations of climatic phases is confined to low latitudes with
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6

Gabdullin, R. R., K. V. Syromyatnikov, N. V. Badulina, S. I. Merenkova, A. V. Ivanov, and I. R. Migranov. "High-precision cyclic correlation as a basis for detailed paleoclimatic reconstructions for the Pliocene-Quartenary sections of Eurasia." Moscow University Bulletin Series 4 Geology, no. 4 (2024) (October 4, 2024): 116–24. http://dx.doi.org/10.55959/msu0579-9406-4-2024-63-4-116-124.

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An astrochronological (cyclostratigraphic) binding of the lithological and geochemical characteristics of Pliocene-Quaternary sediments of the Eurasian sections to the Milankovich cycles (eccentricity, obliquity of the ecliptic, precession) was carried out, an analysis of the relationship between the established variations in climate and paleotemperature with the moments of coincidence of different-order cycles of eccentricity and their paleoclimatic characteristics was given. The results of the implementation of the results obtained during the practice in geology at the Moscow State Universit
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7

Solé, J., A. Turiel, and J. E. Llebot. "Using empirical mode decomposition to correlate paleoclimatic time-series." Natural Hazards and Earth System Sciences 7, no. 2 (2007): 299–307. http://dx.doi.org/10.5194/nhess-7-299-2007.

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Abstract. Determination of the timing and duration of paleoclimatic events is a challenging task. Classical techniques for time-series analysis rely too strongly on having a constant sampling rate, which poorly adapts to the uneven time recording of paleoclimatic variables; new, more flexible methods issued from Non-Linear Physics are hence required. In this paper, we have used Huang's Empirical Mode Decomposition (EMD) for the analysis of paleoclimatic series. We have studied three different time series of temperature proxies, characterizing oscillation patterns by using EMD. To measure the d
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8

Salamatin, Andrey N., and Catherine Ritz. "A simplified multi-scale model for predicting climatic variations of the ice-sheet surface elevation in central Antarctica." Annals of Glaciology 23 (1996): 28–35. http://dx.doi.org/10.3189/s0260305500013227.

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The equation describing the surface evolution of a large ice sheet is examined on the basis of a scale analysis applied to Antarctic conditions. Changes in the surface elevation are mainly driven by mass-balance fluctuations which approximately follow global atmospheric temperature variations. The essential spatial non-uniformity of the accumulation rate and the resultant difference between central and coastal regions in reaction time-scales are taken into account. The dynamic interaction of the time-lagging interior with the quasi-stationary margin is described. As a result, a simplified mode
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9

Salamatin, Andrey N., and Catherine Ritz. "A simplified multi-scale model for predicting climatic variations of the ice-sheet surface elevation in central Antarctica." Annals of Glaciology 23 (1996): 28–35. http://dx.doi.org/10.1017/s0260305500013227.

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The equation describing the surface evolution of a large ice sheet is examined on the basis of a scale analysis applied to Antarctic conditions. Changes in the surface elevation are mainly driven by mass-balance fluctuations which approximately follow global atmospheric temperature variations. The essential spatial non-uniformity of the accumulation rate and the resultant difference between central and coastal regions in reaction time-scales are taken into account. The dynamic interaction of the time-lagging interior with the quasi-stationary margin is described. As a result, a simplified mode
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10

Lopes, Fernando, Vincent Courtillot, Dominique Gibert, and Jean-Louis Le Mouël. "Extending the Range of Milankovic Cycles and Resulting Global Temperature Variations to Shorter Periods (1–100 Year Range)." Geosciences 12, no. 12 (2022): 448. http://dx.doi.org/10.3390/geosciences12120448.

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The Earth’s revolution is modified by changes in inclination of its rotation axis. Its trajectory is not closed and the equinoxes drift. Changes in polar motion and revolution are coupled through the Liouville–Euler equations. Milanković (1920) argued that the shortest precession period of solstices is 20,700 years: the summer solstice in one hemisphere takes place alternately every 11,000 year at perihelion and at aphelion. Milanković assumed that the planetary distances to the Sun and the solar ephemerids are constant. There are now observations that allow one to drop these assumptions. We h
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11

Smirnov, Boris M. "Physics of the Earth’s Glacial Cycle." Foundations 2, no. 4 (2022): 1114–28. http://dx.doi.org/10.3390/foundations2040073.

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The evolution of the atmospheric temperature in the past, resulted from the EPICA project (European Project for Ice Coring in Antarctica) for the analysis of air bubbles in ice deposits near three weather stations in Antarctica, includes several glacial cycles. According to these studies, the glacial cycle consists of a slow cooling of the Earth’s surface at a rate of about 10−4∘C per year for almost the entire time of a single cycle (about 100 thousand years) and of a fast process of heating the planet, similar to a thermal explosion. The observed cooling of the planet follows from the imbala
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12

Gabdullin, R. R., A. Yu Puzik, S. I. Merenkova, et al. "Lithological and geochemical characteristics and paleoclimatic conditions of the origin of Upper Cretaceous deposits of the epicontinental basin of the Russian plate in the region of the Ulyanovsk-Saratov foredeep." Moscow University Bulletin. Series 4. Geology 1, no. 2 (2022): 20–33. http://dx.doi.org/10.33623/0579-9406-2021-2-20-33.

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The results of a geochemical study and paleogeographic, paleoclimatic interpretation for a cyclically constructed section of upper Cretaceous deposits near Volsk city, Saratov region, are presented. Elementary formation cyclites and cyclic variations of a number of certain parameters were associated with the Milankovich astronomical-climatic cycles. The curves of changes of paleotemperature, humidity, paleobathymetry were compiled. The results obtained give an idea of the migration of the arid belt boundaries in the upper Cretaceous and the overall climatic zonation, which is important for reg
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13

Posmentier, E. S. "Response of an ocean-atmosphere climate model to Milankovic forcing." Nonlinear Processes in Geophysics 1, no. 1 (1994): 26–30. http://dx.doi.org/10.5194/npg-1-26-1994.

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Abstract. There is considerable evidence in support of Milankovic's theory that variations in high-latitude summer insolation caused by Earth orbital variations are the cause of the Pleistocene ice cycles. The enigmatic discrepancy between the spectra of Milankovic forcing and of Pleistocene climate variations is believed to be resolved by the slow, nonlinear response of ice sheets to changes in solar seasonality. An experiment with a preliminary version of a 14-region atmosphere/snow/upper ocean climate model demonstrates that the response of the ocean-atmosphere system alone to Milankovic fo
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14

Salamatin, Andrey N., Elena A. Tsyganova, Vladimir Ya Lipenkov, and Jean Robert Petit. "Vostok (Antarctica) ice-core time-scale from datings of different origins." Annals of Glaciology 39 (2004): 283–92. http://dx.doi.org/10.3189/172756404781814023.

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AbstractThree different approaches to ice-core age dating are employed to develop a depth–age relationship at Vostok, Antarctica: (1) correlating the ice-core isotope record to the geophysical metronome (Milankovich surface temperature cycles) inferred from the borehole temperature profile, (2) importing a known chronology from another (Devils Hole, Nevada, USA) paleoclimatic signal, and (3) direct ice-sheet flow modeling. Inverse Monte Carlo sampling is used to constrain the accumulation-rate reconstruction and ice-flow simulations in order to find the best-fit glaciological time-scale matche
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15

Abdussamatov, H. I., Ye V. Lapovok, and S. I. Khankov. "Decrease in temperatures of the ocean and the atmosphere and approach of big Ice Age in the conditions of establishment of cycles of Milankovich." Journal International Academy of Refrigeration 16, no. 3 (2017): 62–66. http://dx.doi.org/10.21047/1606-4313-2017-16-3-62-66.

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16

Prokopenko, Alexander A., Eugene B. Karabanov, Douglas F. Williams, et al. "Biogenic Silica Record of the Lake Baikal Response to Climatic Forcing during the Brunhes." Quaternary Research 55, no. 2 (2001): 123–32. http://dx.doi.org/10.1006/qres.2000.2212.

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AbstractThis work presents a detailed, orbitally tuned biogenic silica record of continental paleoclimate change during the Brunhes chron. The Brunhes/Matuyama boundary lies within the warm isotopic stage 19 in Baikal, and the boundaries between eight lithological cycles correspond to terminations in the marine oxygen isotope record. The high amplitude and resolution of climatically driven changes in BioSi content in Lake Baikal sediments permits tuning of almost every precessional cycle during the Brunhes and reveals the structure of interglacial stages. For example, the last three interglaci
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17

Yuan, Rui, Rui Zhu, Shiwen Xie, Wei Hu, Fengjuan Zhou, and Ye Yu. "Utilizing Maximum Entropy Spectral Analysis (MESA) to identify Milankovitch cycles in Lower Member of Miocene Zhujiang Formation in north slope of Baiyun Sag, Pearl River Mouth Basin, South China Sea." Open Geosciences 11, no. 1 (2019): 877–87. http://dx.doi.org/10.1515/geo-2019-0068.

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Abstract Logs in the petroleum boreholes indirectly records the sedimentary cycles in the deep burial formation. In order to extract and understand the periodicity and cyclicity, it is necessary to process the data by digital signal analysis method. Taking the gamma ray (GR) log as the primary material, an identification approach of Milankovitch cycles in boreholes is proposed in this paper, which is based on the Maximum Entropy Spectral Analysis (MESA). The first stage chooses the appropriate windows for calculating the frequency spectral properties in a short section of the data. In each dep
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18

ADAMS, J. M., H. FAURE, and N. PETIT-MAIRE. "Methane and Milankovitch cycles." Nature 355, no. 6357 (1992): 214. http://dx.doi.org/10.1038/355214a0.

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19

Bennett, K. D. "Milankovitch cycles and their effects on species in ecological and evolutionary time." Paleobiology 16, no. 1 (1990): 11–21. http://dx.doi.org/10.1017/s0094837300009684.

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The Quaternary ice ages were paced by astronomical cycles with periodicities of 20–100 k.y. (Milankovitch cycles). These cycles have been present throughout earth history. The Quaternary fossil record, marine and terrestrial, near to and remote from centers of glaciation, shows that communities of plants and animals are temporary, lasting only a few thousand years at the most. Response of populations to the climatic changes of Quaternary Milankovitch cycles can be taken as typical of the way populations have behaved throughout earth history. Milankovitch cycles thus force an instability of cli
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20

Crowley, Thomas J., Kuor-Jier Joseph Yip, and Steven K. Baum. "Milankovitch cycles and carboniferous climate." Geophysical Research Letters 20, no. 12 (1993): 1175–78. http://dx.doi.org/10.1029/93gl01119.

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21

Ganopolski, Andrey. "Toward generalized Milankovitch theory (GMT)." Climate of the Past 20, no. 1 (2024): 151–85. http://dx.doi.org/10.5194/cp-20-151-2024.

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Abstract. In recent decades, numerous paleoclimate records and results of model simulations have provided strong support for the astronomical theory of Quaternary glacial cycles formulated in its modern form by Milutin Milankovitch. At the same time, new findings have revealed that the classical Milankovitch theory is unable to explain a number of important facts, such as the change in the dominant periodicity of glacial cycles from 41 to 100 kyr about 1 million years ago. This transition was also accompanied by an increase in the amplitude and asymmetry of the glacial cycles. Here, based on t
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22

Abdussamatov, H. I., Ye V. Lapovok, and S. I. Khankov. "Planetary temperature calculations under Milankovitch cycles." Journal International Academy of Refrigeration 15, no. 3 (2016): 82–86. http://dx.doi.org/10.21047/1606-4313-2016-15-3-82-86.

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23

de Winter, N. J., C. Zeeden, and F. J. Hilgen. "Low-latitude climate variability in the Heinrich frequency band of the Late Cretaceous greenhouse world." Climate of the Past 10, no. 3 (2014): 1001–15. http://dx.doi.org/10.5194/cp-10-1001-2014.

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Abstract. Deep marine successions of early Campanian age from DSDP (Deep Sea Drilling Project) site 516F drilled at low paleolatitudes in the South Atlantic reveal distinct sub-Milankovitch variability in addition to precession, obliquity and eccentricity-related variations. Elemental abundance ratios point to a similar climatic origin for these variations and exclude a quadripartite structure as an explanation for the inferred semi-precession cyclicity in the magnetic susceptibility (MS) signal as observed in the Mediterranean Neogene for precession-related cycles. However, semi-precession cy
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Chen, Panpan, Nianqiao Fang, Cunlei Li, and Jianmei Liu. "A method for the division of the conglomerate depositional cycle under Milankovitch cycles." Journal of Geophysics and Engineering 14, no. 3 (2017): 611–20. http://dx.doi.org/10.1088/1742-2140/aa6168.

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25

Kostadinov, T. S., and R. Gilb. "Earth Orbit v2.1: a 3-D visualization and analysis model of Earth's orbit, Milankovitch cycles and insolation." Geoscientific Model Development 7, no. 3 (2014): 1051–68. http://dx.doi.org/10.5194/gmd-7-1051-2014.

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Abstract. Milankovitch theory postulates that periodic variability of Earth's orbital elements is a major climate forcing mechanism, causing, for example, the contemporary glacial–interglacial cycles. There are three Milankovitch orbital parameters: orbital eccentricity, precession and obliquity. The interaction of the amplitudes, periods and phases of these parameters controls the spatio-temporal patterns of incoming solar radiation (insolation) and the timing and duration of the seasons. This complexity makes Earth–Sun geometry and Milankovitch theory difficult to teach effectively. Here, we
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Kostadinov, T. S., and R. Gilb. "Earth Orbit v2.1: a 3-D visualization and analysis model of Earth's orbit, Milankovitch cycles and insolation." Geoscientific Model Development Discussions 6, no. 4 (2013): 5947–80. http://dx.doi.org/10.5194/gmdd-6-5947-2013.

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Abstract. Milankovitch theory postulates that periodic variability of Earth's orbital elements is a major climate forcing mechanism, causing, for example, the contemporary glacial-interglacial cycles. There are three Milankovitch orbital parameters: orbital eccentricity, precession and obliquity. The interaction of the amplitudes, periods and phases of these parameters controls the spatio-temporal patterns of incoming solar radiation (insolation) and the timing of the seasons with respect to perihelion. This complexity makes Earth–Sun geometry and Milankovitch theory difficult to teach effecti
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27

Alam, Syaiful, Ahmad Helman Hamdani, Mohamad Sapari Dwi Hadian, and Noorzamzarina Sulaiman. "Stratigraphic stacking patterns and basin filling efficiency: Impacts of Milankovitch Cycles and spatial facies variability." IOP Conference Series: Earth and Environmental Science 1486, no. 1 (2025): 012011. https://doi.org/10.1088/1755-1315/1486/1/012011.

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Abstract Sedimentation dynamics are significantly influenced by Milankovitch cycles, which govern long-term climate variations through changes in Earth’s orbit, axial tilting, and precession. This study aims to analyse the spatial variability in sedimentation by quantifying the compensation index, which measures basin filling efficiency regulation across different depositional environments. The study uses stratigraphic data from Sumedang-Majalengka section, including non-marine facies of the fluvial Citalang Formation and marine facies of the Halang Formation. The compensation index evaluation
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28

de Winter, N. J., C. Zeeden, and F. J. Hilgen. "Low-latitude climate variability in the Heinrich frequency band of the Late Cretaceous Greenhouse world." Climate of the Past Discussions 9, no. 4 (2013): 4475–98. http://dx.doi.org/10.5194/cpd-9-4475-2013.

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Abstract. Deep marine successions of early Campanian age from DSDP site 516F drilled at low paleolatitudes in the South Atlantic reveal distinct sub-Milankovitch variability in addition to precession and eccentricity related variations. Elemental abundance ratios point to a similar climatic origin for these variations and exclude a quadripartite structure – as observed in the Mediterranean Neogene – of the precession related cycles as an explanation for the inferred semi-precession cyclicity in MS. However, the semi-precession cycle itself is likely an artifact, reflecting the first harmonic o
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29

Hinnov, Linda A., and Richard J. Diecchio. "Milankovitch cycles in the Juniata Formation, Late Ordovician, Central Appalachian Basin, USA." Stratigraphy 12, no. 3-4 (2016): 287–96. http://dx.doi.org/10.29041/strat.12.4.07.

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The Juniata Formation is a thick succession of prevalently red, cyclically bedded arenites, wackes, and mudrocks found in the Upper Ordovician of the Central Appalachian Basin, USA. In outcrops close to the study area, the Juniata cycles predominantly have the characteristics of regressive tidal flat deposits. Long and continuous well logs of the subsurface Juniata provide an unparalleled opportunity to investigate Milankovitch controls on the cyclic deposition. In the Preston 119 well, northern West Virginia, a 2700-ft long gamma-ray well log provides a high-resolution proxy of terrigenous si
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30

Dean, Walter E., and James V. Gardner. "Milankovitch cycles in Neocene deep-sea sediment." Paleoceanography 1, no. 4 (1986): 539–53. http://dx.doi.org/10.1029/pa001i004p00539.

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31

Schwarzacher, W. "Milankovitch cycles and the measurement of time." Terra Nova 1, no. 5 (1989): 405–8. http://dx.doi.org/10.1111/j.1365-3121.1989.tb00400.x.

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32

Short, David A., John G. Mengel, Thomas J. Crowley, William T. Hyde, and Gerald R. North. "Filtering of Milankovitch Cycles by Earth's Geography." Quaternary Research 35, no. 2 (1991): 157–73. http://dx.doi.org/10.1016/0033-5894(91)90064-c.

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AbstractEarth's land-sea distribution modifies the temperature response to orbitally induced perturbations of the seasonal insolation. We examine this modification in the frequency domain by generating 800,000-yr time series of maximum summer temperature in selected regions with a linear, two-dimensional, seasonal energy balance climate model. Previous studies have demonstrated that this model has a sensitivity comparable to general circulation models for the seasonal temperature response to orbital forcing on land. Although the observed response in the geologic record is sometimes significant
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33

Crampton, James S., Stephen R. Meyers, Roger A. Cooper, Peter M. Sadler, Michael Foote, and David Harte. "Pacing of Paleozoic macroevolutionary rates by Milankovitch grand cycles." Proceedings of the National Academy of Sciences 115, no. 22 (2018): 5686–91. http://dx.doi.org/10.1073/pnas.1714342115.

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Periodic fluctuations in past biodiversity, speciation, and extinction have been proposed, with extremely long periods ranging from 26 to 62 million years, although forcing mechanisms remain speculative. In contrast, well-understood periodic Milankovitch climate forcing represents a viable driver for macroevolutionary fluctuations, although little evidence for such fluctuation exists except during the Late Cenozoic. The reality, magnitude, and drivers of periodic fluctuations in macroevolutionary rates are of interest given long-standing debate surrounding the relative roles of intrinsic bioti
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Cvijanovic, Ivana, Jelena Lukovic, and James D. Begg. "One hundred years of Milanković cycles." Nature Geoscience 13, no. 8 (2020): 524–25. http://dx.doi.org/10.1038/s41561-020-0621-2.

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35

Deitrick, Russell, Rory Barnes, Thomas R. Quinn, John Armstrong, Benjamin Charnay, and Caitlyn Wilhelm. "Exo-Milankovitch Cycles. I. Orbits and Rotation States." Astronomical Journal 155, no. 2 (2018): 60. http://dx.doi.org/10.3847/1538-3881/aaa301.

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36

Marsh, Gerald E. "Interglacials, Milankovitch Cycles, Solar Activity, and Carbon Dioxide." Journal of Climatology 2014 (September 8, 2014): 1–7. http://dx.doi.org/10.1155/2014/345482.

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The existing understanding of interglacial periods is that they are initiated by Milankovitch cycles enhanced by rising atmospheric carbon dioxide concentrations. During interglacials, global temperature is also believed to be primarily controlled by carbon dioxide concentrations, modulated by internal processes such as the Pacific Decadal Oscillation and the North Atlantic Oscillation. Recent work challenges the fundamental basis of these conceptions.
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Brickman, David, D. G. Wright, and William Hyde. "Filtering of Milankovitch Cycles by the Thermohaline Circulation." Journal of Climate 12, no. 6 (1999): 1644–58. http://dx.doi.org/10.1175/1520-0442(1999)012<1644:fomcbt>2.0.co;2.

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38

Spiegel, David S., Sean N. Raymond, Courtney D. Dressing, Caleb A. Scharf, and Jonathan L. Mitchell. "GENERALIZED MILANKOVITCH CYCLES AND LONG-TERM CLIMATIC HABITABILITY." Astrophysical Journal 721, no. 2 (2010): 1308–18. http://dx.doi.org/10.1088/0004-637x/721/2/1308.

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39

Ainsworth, R. Bruce, Adam J. Vonk, Paul Wellington, and Victorien Paumard. "Out-of-phase cyclical sediment supply: A potential causal mechanism for generating stratigraphic asymmetry and explaining sequence stratigraphic spatial variability." Journal of Sedimentary Research 90, no. 12 (2020): 1706–33. http://dx.doi.org/10.2110/jsr.2020.012.

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ABSTRACTAlthough acknowledged to be a simplification, the rate of sediment supply is usually assumed to be constant in sequence stratigraphic interpretations of clastic shelf systems. The simplified assumption taken in this work is that sediment supply can be represented by sine curves linked to climate changes driven by Milankovitch cycles. Three orders of sediment supply sine curves (amplitude and frequency scaled to order) are convolved with three orders of Milankovitch-forced eustatic sea-level sine curves and a constant rate of subsidence to generate curves for the ratio of rate of accomm
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Anderson, R. Y. "Enhanced climate variability in the tropics: a 200 000 yr annual record of monsoon variability from Pangea's equator." Climate of the Past 7, no. 3 (2011): 757–70. http://dx.doi.org/10.5194/cp-7-757-2011.

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Abstract. A continuous series of 209 000 evaporite varves from the equator of arid western Pangea (age = −255 ma), as a proxy for surface temperature, has a complete suite of Milankovitch cycles and harmonics as expected for a rectified reaction to precession-modulated insolation at the equator. Included are modes of precession (23.4 kyr, 18.2 kyr), semi-precession (11.7 kyr, 9.4 kyr), and harmonics at ~7 kyr and 5.4 kyr. An oscillation of ~100 kyr, with 35 % of total variance, originates as an amplitude modulation of precession cycles. An exceptionally strong 2.3 kyr quasi-bi-millennial oscil
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41

Lewis, David F. V., and Jean-Lou C. M. Dorne. "The Astronomical Pulse of Global Extinction Events." Scientific World JOURNAL 6 (2006): 718–26. http://dx.doi.org/10.1100/tsw.2006.156.

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The linkage between astronomical cycles and the periodicity of mass extinctions is reviewed and discussed. In particular, the apparent 26 million year cycle of global extinctions may be related to the motion of the solar system around the galaxy, especially perpendicular to the galactic plane. The potential relevance of Milankovitch cycles is also explored in the light of current evidence for the possible causes of extinction events over a geological timescale.
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42

Meyers, Stephen R., and Alberto Malinverno. "Proterozoic Milankovitch cycles and the history of the solar system." Proceedings of the National Academy of Sciences 115, no. 25 (2018): 6363–68. http://dx.doi.org/10.1073/pnas.1717689115.

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The geologic record of Milankovitch climate cycles provides a rich conceptual and temporal framework for evaluating Earth system evolution, bestowing a sharp lens through which to view our planet’s history. However, the utility of these cycles for constraining the early Earth system is hindered by seemingly insurmountable uncertainties in our knowledge of solar system behavior (including Earth–Moon history), and poor temporal control for validation of cycle periods (e.g., from radioisotopic dates). Here we address these problems using a Bayesian inversion approach to quantitatively link astron
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43

Forgan, Duncan. "Milankovitch cycles of terrestrial planets in binary star systems." Monthly Notices of the Royal Astronomical Society 463, no. 3 (2016): 2768–80. http://dx.doi.org/10.1093/mnras/stw2098.

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44

Radivojevic, Dejan. "A hundred years of Milutin Milankovic's climate change theory-geological implications." Annales g?ologiques de la Peninsule balkanique 81, no. 2 (2020): 87–98. http://dx.doi.org/10.2298/gabp201125011r.

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Milankovic?s cycles theory published hundred years ago is the most important theory in climate science and had great influence on Earth disciplines. Nevertheless, his work waited for more than fifty years for confirmation. It could be said that Milankovic?s work had most influence in creation of Astronomic Time Scale, supporting of continental drift hypothesis and palaeoclimatology implications. Positive results of the implementation of the astronomic time scale to the Neogene stratigraphy initiated the application of this method within the Mesozoic, and lately also to the Paleozoic sediments.
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45

Hágen, András. "Astronomical causes of climate change. Milanković–Bacsák cycle and the last ice age." Acta climatologica et chorologica 55, no. 1 (2021): 5–16. http://dx.doi.org/10.14232/acta.clim.2021.55.1.

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György Bacsák, a Hungarian polyhistor, was born 150 years ago and died 50 years ago. He played an important role in refining and further developing the Milanković cycle. Milanković's theory describes the effect of changes in Earth's movements on the climate. The theory came from its creator, Milutin Milanković, a Serbian geophysicist and astronomer. The Serbian scientist was imprisoned in the Austro-Hungarian Monarchy during World War I as a citizen of a hostile state. He developed his theory in the library of the Hungarian Academy of Sciences. Understanding the essence of the theory, György B
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46

Hágen, András. "Astronomical causes of climate change. Milanković–Bacsák cycle and the last ice age." Acta climatologica et chorologica 55, no. 1 (2021): 5–16. http://dx.doi.org/10.14232/acta.clim.2020.55.1.

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György Bacsák, a Hungarian polyhistor, was born 150 years ago and died 50 years ago. He played an important role in refining and further developing the Milanković cycle. Milanković's theory describes the effect of changes in Earth's movements on the climate. The theory came from its creator, Milutin Milanković, a Serbian geophysicist and astronomer. The Serbian scientist was imprisoned in the Austro-Hungarian Monarchy during World War I as a citizen of a hostile state. He developed his theory in the library of the Hungarian Academy of Sciences. Understanding the essence of the theory, György B
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47

Jovanovic, Gordana. "The Influence of Natural Cycles on Climate Change." Modern Environmental Science and Engineering 8, no. 9 (2022): 477–82. http://dx.doi.org/10.15341/mese(2333-2581)/09.08.2022/004.

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The influence of natural cycles on the climate of our planet was very successfully and in detail examined by Milutin Milankovitch. He described mathematically precisely how the movement of the Earth around the Sun over long periods of time is reflected in its climate at different latitudes. Modern researches show the existence of some other natural cycles — astronomical, related to the activity of the Sun and its cycles, and terrestrial, related to periodic processes on Earth such as El Niño and La Niña, which also affect the climate. This paper will discuss all these impacts as well as scient
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48

Soua, Mohamed. "Time series analysis (orbital cycles) of the uppermost Cenomanian-Lower Turonian sequence on the southern Tethyan margin using foraminifera." Geologica Carpathica 61, no. 2 (2010): 111–20. http://dx.doi.org/10.2478/v10096-010-0004-5.

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Time series analysis (orbital cycles) of the uppermost Cenomanian-Lower Turonian sequence on the southern Tethyan margin using foraminiferaTime series analysis has been performed for the first time on the Cenomanian-Turonian sequence in Central Tunisia in order to shed light on its Milankovitch-like cyclicity. This analysis was applied to two foraminiferal genera: the biserialHeterohelix, an oxygen-minimum zone (OMZ) dweller, and the triserialGuembelitria, a eutrophic surface dweller. Average sedimentary rates and the duration of the oceanic anoxic event (OAE2) in each studied section were est
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Schwarzacher, Walther. "Milankovitch cycles in the pre-Pleistocene stratigraphic record: a review." Geological Society, London, Special Publications 70, no. 1 (1993): 187–94. http://dx.doi.org/10.1144/gsl.sp.1993.070.01.13.

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Niggemann, Stefan, Augusto Mangini, Manfred Mudelsee, Detlev K. Richter, and Georg Wurth. "Sub-Milankovitch climatic cycles in Holocene stalagmites from Sauerland, Germany." Earth and Planetary Science Letters 216, no. 4 (2003): 539–47. http://dx.doi.org/10.1016/s0012-821x(03)00513-2.

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