# Cave KNI-51, Western Australia 8,800 Year Stalagmite d18O Data #---------------------------------------------------- # World Data Service for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program # National Centers for Environmental Information (NCEI) #---------------------------------------------------- # Template Version 4.0 # Encoding: UTF-8 # NOTE: Please cite original publication, NOAA Landing Page URL, dataset and publication DOIs (where available), and date accessed when using downloaded data. If there is no publication information, please cite investigator, study title, NOAA Landing Page URL, and date accessed. # # Description/Documentation lines begin with # # Data lines have no # # # NOAA_Landing_Page: https://www.ncei.noaa.gov/access/paleo-search/study/20530 # Landing_Page_Description: NOAA Landing Page of this file's parent study, which includes all study metadata. # # Study_Level_JSON_Metadata: https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/json/noaa-cave-20530.json # Study_Level_JSON_Description: JSON metadata of this data file's parent study, which includes all study metadata. # # Data_Type: Speleothems # # Dataset_DOI: 10.25921/htg9-m613 # # Science_Keywords: Monsoon #-------------------- # Resource_Links # # Data_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/speleothem/australia/kni-51-0-2016d18o-noaa.txt # Data_Download_Description: NOAA Template File; Stalagmite KNI-51-0 d18O Data # #-------------------- # Contribution_Date # Date: 2016-09-29 #-------------------- # File_Last_Modified_Date # Date: 2025-03-20 #-------------------- # Title # Study_Name: Cave KNI-51, Western Australia 8,800 Year Stalagmite d18O Data #-------------------- # Investigators # Investigators: Denniston, R.F.(https://orcid.org/0000-0002-6346-1221); Ummenhofer, C.C.(https://orcid.org/0000-0002-9163-3967); Wanamaker, A.D.(https://orcid.org/0000-0002-6560-6420); Lachniet, M.S.(https://orcid.org/0000-0001-5250-0144); Villarini, G.(https://orcid.org/0000-0001-9566-2370); Asmerom, Y.(https://orcid.org/0000-0003-3440-1294); Polyak, V.J.(https://orcid.org/0000-0002-2010-1066); Passaro, K.J.; Cugley, J.(https://orcid.org/0000-0002-6827-875X); Woods, D.(https://orcid.org/0000-0001-6264-2218); Humphreys, W.F. #-------------------- # Description_Notes_and_Keywords # Description: Stalagmite oxygen isotope (d18O) data for 18 calcite and aragonite stalagmites collected in Cave KNI-51, tropical Western Australia, providing a paleomonsoon record for the past 8,800 years. Note: d18O values for stalagmite KNI-51-10 have been decreased by 1 per mil. Provided Keywords: stalagmite, oxygen isotope, Australia, monsoon, tropical rain belt. # # Data file updated 7/26/2017. In the data section of the file, ages were corrected for the stable isotope data of stalagmites KNI-51-10, KNI-51-A2-side 1, and KNI-51-A2-side 2. Stalagmite labels were corrected for stalagmites KNI-51-A2-side 1 and KNI-51-A2-side 2 (previously were mistakenly labelled as KNI-51-A1-side 1 and KNI-51-A1-side 2). In the Chronology section, distances for U-Th dates in stalagmite KNI-51-A2-side 1 and KNI-51-A2-side 2 were corrected, and ages for U-Th dates in stalagmite KNI-51-A2-side 1 and KNI-51-A2-side 2 were corrected. # # Additional assigned age corrections were made to this file 7-February-2018. #-------------------- # Publication # Authors: Denniston, R.F., Wyrwoll, K.-H., Polyak, Brown, J. Asmerom, Y., Wanamaker, A. Jr., LaPointe, Z., Ellerbroek, R., Barthelmes, M., Cleary, D., Cugley, J., Woods, D., Humphreys, W. # Journal_Name: Quaternary Science Reviews # Published_Title: A Stalagmite Record of Holocene Indonesian-Australian Summer Monsoon Variability from the Australian Tropics # Published_Date_or_Year: 2013 # Volume: 78 # Pages: 155-168 # Issue: # Report_Number: # DOI: 10.1016/j.quascirev.2013.08.004 # Full_Citation: # Abstract: Oxygen isotopic data from a suite of calcite and aragonite stalagmites from cave KNI-51, located in the eastern Kimberley region of tropical Western Australia, represent the first absolute-dated, high-resolution speleothem record of the Holocene Indonesian-Australian summer monsoon (IASM) from the Australian tropics. Stalagmite oxygen isotopic values track monsoon intensity via amount effects in precipitation and reveal a dynamic Holocene IASM which strengthened in the early Holocene, decreased in strength by 4 ka, with a further decrease from 2 to 1 ka, before strengthening again at 1 ka to years to levels similar to those between 4 and 2 ka. The relationships between the KNI-51 IASM reconstruction and those from published speleothem time series from Flores and Borneo, in combination with other data sets, appear largely inconsistent with changes in the position and/or organization of the Intertropical Convergence Zone (ITCZ). Instead, we argue that the El Nino/Southern Oscillation (ENSO) may have played a dominant role in driving IASM variability since at least the middle Holocene. Given the muted modern monsoon rainfall responses to most El Nino events in the Kimberley, an impact of ENSO on regional monsoon precipitation over northwestern Australia would suggest non-stationarity in the long-term relationship between ENSO forcing and IASM rainfall, possibly due to changes in the mean state of the tropical Pacific over the Holocene. #-------------------- # Authors: Rhawn F. Denniston, Caroline C. Ummenhofer, Alan D. Wanamaker, Matthew S. Lachniet, Gabriele Villarini, Yemane Asmerom, Victor J. Polyak, Kristian J. Passaro, John Cugley, David Woods, and William F. Humphreys # Journal_Name: Scientific Reports # Published_Title: Expansion and Contraction of the Indo-Pacific Tropical Rain Belt over the Last Three Millennia # Published_Date_or_Year: 2016 # Volume: 6 # Pages: # Issue: # Report_Number: # DOI: 10.1038/srep34485 # Full_Citation: # Abstract: The seasonal north-south migration of the intertropical convergence zone (ITCZ) defines the tropical rain belt (TRB), a region of enormous terrestrial and marine biodiversity and home to 40% of people on Earth. The TRB is dynamic and has been shown to shift south as a coherent system during periods of Northern Hemisphere cooling. However, recent studies of Indo-Pacific hydroclimate suggest that during the Little Ice Age (LIA; AD 1400-1850), the TRB in this region contracted rather than being displaced uniformly southward. This behaviour is not well understood, particularly during climatic fluctuations less pronounced than those of the LIA, the largest centennial-scale cool period of the last millennium. Here we show that the Indo-Pacific TRB expanded and contracted numerous times over multi-decadal to centennial scales during the last 3,000 yr. By integrating precisely-dated stalagmite records of tropical hydroclimate from southern China with a newly enhanced stalagmite time series from northern Australia, our study reveals a previously unidentified coherence between the austral and boreal summer monsoon. State-of-the-art climate model simulations of the last millennium suggest these are linked to changes in the structure of the regional manifestation of the atmosphere's meridional circulation. #-------------------- # Authors: Rhawn F. Denniston, Gabriele Villarini, Angelique N. Gonzales, Karl-Heinz Wyrwoll, Victor J. Polyak, Caroline C. Ummenhofer, Matthew S. Lachniet, Alan D. Wanamaker, Jr, William F. Humphreys, David Woods, and John Cugley # Journal_Name: Proceedings of the National Academy of Sciences # Published_Title: Extreme rainfall activity in the Australian tropics reflects changes in the El Niño/Southern Oscillation over the last two millennia # Published_Date_or_Year: 2015 # Volume: 112 # Pages: 4576-4581 # Issue: 15 # Report_Number: # DOI: 10.1073/pnas.1422270112 # Full_Citation: # Abstract: Assessing temporal variability in extreme rainfall events before the historical era is complicated by the sparsity of long-term "direct" storm proxies. Here we present a 2,200-y-long, accurate, and precisely dated record of cave flooding events from the northwest Australian tropics that we interpret, based on an integrated analysis of meteorological data and sediment layers within stalagmites, as representing a proxy for extreme rainfall events derived primarily from tropical cyclones (TCs) and secondarily from the regional summer monsoon. This time series reveals substantial multicentennial variability in extreme rainfall, with elevated occurrence rates characterizing the twentieth century, 850-1450 CE (Common Era), and 50-400 CE; reduced activity marks 1450-1650 CE and 500-850 CE. These trends are similar to reconstructed numbers of TCs in the North Atlantic and Caribbean basins, and they form temporal and spatial patterns best explained by secular changes in the dominant mode of the El Niño/Southern Oscillation (ENSO), the primary driver of modern TC variability. We thus attribute long-term shifts in cyclogenesis in both the central Australian and North Atlantic sectors over the past two millennia to entrenched El Niño or La Niña states of the tropical Pacific. The influence of ENSO on monsoon precipitation in this region of northwest Australia is muted, but ENSO-driven changes to the monsoon may have complemented changes to TC activity. #-------------------- # Funding_Agency # Funding_Agency_Name: US National Science Foundation # Grant: AGS-1103413 #-------------------- # Site_Information # Site_Name: Cave KNI-51 # Location: Western Australia # Northernmost_Latitude: -15.18 # Southernmost_Latitude: -15.18 # Easternmost_Longitude: 128.37 # Westernmost_Longitude: 128.37 # Elevation_m: 100 #-------------------- # Data_Collection # Collection_Name: KNI-51-0-2016d18O # First_Year: 8806 # Last_Year: 304 # Time_Unit: cal yr BP # Core_Length_m: # Parameter_Keywords: oxygen isotopes # Notes: #-------------------- # Chronology_Information # Chronology: Uranium-Thorium # Chronology_Download_Resource: https://www.ncei.noaa.gov/pub/data/paleo/templates/noaa-wds-paleo-uth-terms.csv # Chronology_Download_Description: Uranium-Thorium terms and definitions. # Chronology_Notes: Samples with asterisks were published in Denniston et al. (2015); all others reported in Denniston et al. (2013) # Rejection_Rationale: # 238U_Decay_Constant: Cheng et al., 2000 # 234U_Decay_Constant: Cheng et al., 2000 # 230Th_Decay_Constant: Cheng et al., 2000 # Initial_230Th/232Th: 4.4 × 10−6 ± 4.4 × 10−6 # Initial_230Th/232Th_Method: Average crustal silicate ratio # Age_Model_Method: # Missing_Values: na # Chronology_Table: # core_id material_dated depth_bot_mm 238U_ppm 232Th_ppb d234U_init_permil d234U_init_2s_permil 230Th_238U_act 230Th_238U_act_2s 230Th_232Th_atom_ppm 230Th_232Th_atom_2s_ppm age_uncorr_BM age_uncorr_2s_yr age_corr_BP1950 age_corr_2s_yr date_type # KNI-51-0 calcite 1920 422 15569 409.7 2.0 0.014 0.00034 6 0.2 1109 27 285 764 MC-ICP-MS # Hiatus NA 1901.5 NA NA NA NA NA NA NA NA NA NA NA NA hiatus # KNI-51-0 calcite 1808 84 3988 450.3 5.0 0.065 0.00241 23 0.9 5006 191 3994 972 MC-ICP-MS # KNI-51-0 calcite 1730 183 3261 444.2 2.0 0.061 0.00073 57 0.9 4752 58 4332 365 MC-ICP-MS # KNI-51-0 calcite 1563 452 5793 424.3 1.3 0.067 0.00055 87 1.1 5297 45 4974 266 MC-ICP-MS # KNI-51-0 calcite 1484 106 2196 460.0 2.4 0.070 0.00133 56 1.5 5360 105 4885 428 MC-ICP-MS # KNI-51-0 calcite 1412 122 1113 446.0 2.6 0.070 0.00139 126 6.1 5426 111 5182 215 MC-ICP-MS # KNI-51-0 calcite 1075 100 2518 474.8 1.9 0.079 0.00110 51 1.5 6003 86 5442 508 MC-ICP-MS # KNI-51-0 calcite 1064 112 1207 480.4 1.8 0.079 0.00110 122 3.9 6021 86 5749 229 MC-ICP-MS # KNI-51-0 calcite 973 72 1427 441.5 2.2 0.080 0.00180 66 2.4 6250 144 5787 427 MC-ICP-MS # KNI-51-0 calcite 771 136 579 506.0 2.0 0.108 0.00076 418 15.4 8130 60 7988 102 MC-ICP-MS # KNI-51-0 calcite 640 82 2020 445.7 2.9 0.098 0.00220 66 2.5 7664 179 7107 528 MC-ICP-MS # KNI-51-0 calcite 538 84 429 457.5 2.4 0.114 0.00168 366 32.4 8889 138 8727 172 MC-ICP-MS # KNI-51-0 calcite 441 89 2222 458.3 2.3 0.111 0.00149 73 1.7 8663 122 8104 514 MC-ICP-MS # KNI-51-0 calcite 356 136 579 506.0 2.0 0.108 0.00076 418 15.4 8130 60 7988 102 MC-ICP-MS #-------------------- # Variables # PaST_Thesaurus_Download_Resource: https://www.ncei.noaa.gov/access/paleo-search/skos/past-thesaurus.rdf # PaST_Thesaurus_Download_Description: Paleoenvironmental Standard Terms (PaST) Thesaurus terms, definitions, and relationships in SKOS format. # # Data variables follow that are preceded by '##' in columns one and two. # Variables list, one per line, shortname-tab-var components: what, material, error, units, seasonality, data type, detail, method, C or N for Character or Numeric data) # ## sampleID sample identification,,,,,speleothems,,,C,Stalagmite ID ## depth_mm depth,,,millimeter,,speleothems,,,N,distance from base ## mineral notes,,,,,speleothems,,,C,calcite or aragonite ## age_calBP age,,,calendar year before present,,speleothems,,,N, ## d18OcarbVPDB delta 18O,calcium carbonate,,per mil VPDB,,speleothems,raw,isotope ratio mass spectrometry,N, #-------------------- # Data: # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing_Values: sampleID depth_mm mineral age_calBP d18OcarbVPDB KNI-51-0 1933 calcite 304 -8.63 KNI-51-0 1930 calcite 314 -9.45 KNI-51-0 1927 calcite 324 -8.34 KNI-51-0 1924 calcite 333 -8.67 KNI-51-0 1921 calcite 343 -8.93 KNI-51-0 1918 calcite 352 -8.17 KNI-51-0 1915 calcite 362 -9.03 KNI-51-0 1912 calcite 372 -8.67 KNI-51-0 1909 calcite 381 -8.01 KNI-51-0 1906 calcite 391 -8.10 KNI-51-0 1903 calcite 400 -8.47 KNI-51-0 1900 calcite 4028 -9.97 KNI-51-0 1897 calcite 4033 -8.78 KNI-51-0 1894 calcite 4038 -9.55 KNI-51-0 1891 calcite 4043 -8.20 KNI-51-0 1888 calcite 4048 -8.76 KNI-51-0 1885 calcite 4054 -7.35 KNI-51-0 1882 calcite 4059 -9.70 KNI-51-0 1879 calcite 4064 -7.68 KNI-51-0 1876 calcite 4069 -8.60 KNI-51-0 1873 calcite 4075 -9.93 KNI-51-0 1870 calcite 4080 -8.28 KNI-51-0 1867 calcite 4085 -10.09 KNI-51-0 1864 calcite 4090 -10.21 KNI-51-0 1861 calcite 4096 -9.16 KNI-51-0 1858 calcite 4101 -9.69 KNI-51-0 1855 calcite 4106 -9.22 KNI-51-0 1852 calcite 4112 -8.85 KNI-51-0 1849 calcite 4117 -11.15 KNI-51-0 1846 calcite 4123 -9.49 KNI-51-0 1843 calcite 4128 -7.94 KNI-51-0 1840 calcite 4133 -9.44 KNI-51-0 1837 calcite 4139 -9.70 KNI-51-0 1834 calcite 4144 -8.86 KNI-51-0 1831 calcite 4150 -8.74 KNI-51-0 1828 calcite 4155 -7.78 KNI-51-0 1825 calcite 4161 -9.15 KNI-51-0 1822 calcite 4166 -8.91 KNI-51-0 1819 calcite 4172 -8.58 KNI-51-0 1813 calcite 4183 -9.40 KNI-51-0 1807 calcite 4194 -9.58 KNI-51-0 1801 calcite 4205 -8.63 KNI-51-0 1795 calcite 4217 -8.32 KNI-51-0 1789 calcite 4228 -10.10 KNI-51-0 1783 calcite 4240 -7.96 KNI-51-0 1777 calcite 4251 -9.02 KNI-51-0 1771 calcite 4263 -9.55 KNI-51-0 1765 calcite 4274 -8.60 KNI-51-0 1759 calcite 4286 -8.88 KNI-51-0 1753 calcite 4298 -8.31 KNI-51-0 1747 calcite 4310 -9.48 KNI-51-0 1741 calcite 4322 -9.57 KNI-51-0 1735 calcite 4334 -8.72 KNI-51-0 1729 calcite 4346 -8.57 KNI-51-0 1723 calcite 4358 -8.95 KNI-51-0 1717 calcite 4370 -9.03 KNI-51-0 1711 calcite 4382 -8.08 KNI-51-0 1705 calcite 4395 -8.15 KNI-51-0 1699 calcite 4407 -8.11 KNI-51-0 1693 calcite 4419 -9.76 KNI-51-0 1687 calcite 4432 -9.42 KNI-51-0 1681 calcite 4444 -8.99 KNI-51-0 1675 calcite 4457 -8.88 KNI-51-0 1669 calcite 4470 -8.58 KNI-51-0 1663 calcite 4482 -9.09 KNI-51-0 1657 calcite 4495 -8.36 KNI-51-0 1651 calcite 4508 -10.11 KNI-51-0 1645 calcite 4521 -9.76 KNI-51-0 1639 calcite 4534 -9.20 KNI-51-0 1633 calcite 4547 -9.39 KNI-51-0 1627 calcite 4560 -8.48 KNI-51-0 1621 calcite 4574 -7.91 KNI-51-0 1615 calcite 4587 -7.86 KNI-51-0 1610 calcite 4598 -9.22 KNI-51-0 1604 calcite 4611 -10.08 KNI-51-0 1598 calcite 4625 -10.24 KNI-51-0 1592 calcite 4638 -9.43 KNI-51-0 1586 calcite 4652 -9.89 KNI-51-0 1583 calcite 4659 -8.11 KNI-51-0 1580 calcite 4666 -9.97 KNI-51-0 1574 calcite 4679 -8.09 KNI-51-0 1568 calcite 4693 -8.84 KNI-51-0 1562 calcite 4707 -8.40 KNI-51-0 1559 calcite 4714 -7.99 KNI-51-0 1556 calcite 4721 -9.44 KNI-51-0 1550 calcite 4735 -8.09 KNI-51-0 1544 calcite 4749 -7.88 KNI-51-0 1538 calcite 4763 -8.37 KNI-51-0 1532 calcite 4777 -8.22 KNI-51-0 1529 calcite 4784 -8.48 KNI-51-0 1523 calcite 4799 -9.79 KNI-51-0 1517 calcite 4813 -8.27 KNI-51-0 1511 calcite 4827 -8.22 KNI-51-0 1505 calcite 4842 -10.50 KNI-51-0 1499 calcite 4856 -7.67 KNI-51-0 1493 calcite 4871 -8.66 KNI-51-0 1487 calcite 4885 -9.46 KNI-51-0 1481 calcite 4900 -8.62 KNI-51-0 1475 calcite 4915 -9.79 KNI-51-0 1469 calcite 4930 -8.35 KNI-51-0 1463 calcite 4945 -8.47 KNI-51-0 1457 calcite 4960 -7.52 KNI-51-0 1451 calcite 4975 -10.43 KNI-51-0 1439 calcite 5005 -8.80 KNI-51-0 1433 calcite 5020 -8.55 KNI-51-0 1427 calcite 5036 -8.93 KNI-51-0 1415 calcite 5066 -8.44 KNI-51-0 1409 calcite 5082 -7.66 KNI-51-0 1403 calcite 5097 -7.53 KNI-51-0 1397 calcite 5113 -9.18 KNI-51-0 1391 calcite 5129 -9.29 KNI-51-0 1385 calcite 5145 -6.85 KNI-51-0 1379 calcite 5160 -9.06 KNI-51-0 1373 calcite 5176 -7.00 KNI-51-0 1367 calcite 5192 -8.97 KNI-51-0 1361 calcite 5208 -8.12 KNI-51-0 1355 calcite 5224 -8.97 KNI-51-0 1349 calcite 5240 -8.14 KNI-51-0 1343 calcite 5257 -6.67 KNI-51-0 1337 calcite 5273 -6.80 KNI-51-0 1331 calcite 5289 -7.37 KNI-51-0 1325 calcite 5306 -9.42 KNI-51-0 1319 calcite 5322 -8.49 KNI-51-0 1313 calcite 5339 -7.66 KNI-51-0 1307 calcite 5355 -7.32 KNI-51-0 1301 calcite 5372 -9.10 KNI-51-0 1295 calcite 5389 -9.01 KNI-51-0 1289 calcite 5406 -8.43 KNI-51-0 1283 calcite 5422 -8.51 KNI-51-0 1277 calcite 5439 -9.14 KNI-51-0 1271 calcite 5456 -9.44 KNI-51-0 1265 calcite 5473 -8.26 KNI-51-0 1259 calcite 5490 -7.30 KNI-51-0 1253 calcite 5508 -7.57 KNI-51-0 1247 calcite 5525 -7.29 KNI-51-0 1241 calcite 5542 -8.48 KNI-51-0 1235 calcite 5560 -7.94 KNI-51-0 1229 calcite 5577 -7.96 KNI-51-0 1223 calcite 5595 -10.10 KNI-51-0 1217 calcite 5612 -10.43 KNI-51-0 1211 calcite 5630 -7.68 KNI-51-0 1205 calcite 5647 -8.03 KNI-51-0 1199 calcite 5665 -9.16 KNI-51-0 1193 calcite 5683 -9.94 KNI-51-0 1187 calcite 5701 -8.55 KNI-51-0 1181 calcite 5719 -6.56 KNI-51-0 1175 calcite 5737 -9.10 KNI-51-0 1169 calcite 5755 -6.64 KNI-51-0 1163 calcite 5773 -7.73 KNI-51-0 1157 calcite 5791 -8.14 KNI-51-0 1151 calcite 5810 -9.79 KNI-51-0 1145 calcite 5828 -7.47 KNI-51-0 1139 calcite 5846 -8.02 KNI-51-0 1133 calcite 5865 -8.44 KNI-51-0 1127 calcite 5883 -7.22 KNI-51-0 1121 calcite 5902 -9.76 KNI-51-0 1115 calcite 5921 -9.53 KNI-51-0 1109 calcite 5939 -6.94 KNI-51-0 1103 calcite 5958 -9.18 KNI-51-0 1100 calcite 5968 -8.76 KNI-51-0 1097 calcite 5977 -8.28 KNI-51-0 1094 calcite 5987 -10.10 KNI-51-0 1091 calcite 5996 -7.85 KNI-51-0 1088 calcite 6006 -7.19 KNI-51-0 1085 calcite 6015 -7.33 KNI-51-0 1082 calcite 6025 -7.91 KNI-51-0 1079 calcite 6034 -8.06 KNI-51-0 1076 calcite 6044 -8.29 KNI-51-0 1073 calcite 6053 -9.60 KNI-51-0 1070 calcite 6063 -8.07 KNI-51-0 1067 calcite 6072 -8.76 KNI-51-0 1064 calcite 6082 -8.64 KNI-51-0 1061 calcite 6092 -8.86 KNI-51-0 1058 calcite 6101 -9.24 KNI-51-0 1055 calcite 6111 -8.38 KNI-51-0 1052 calcite 6121 -7.13 KNI-51-0 1049 calcite 6130 -8.67 KNI-51-0 1046 calcite 6140 -7.17 KNI-51-0 1043 calcite 6150 -7.88 KNI-51-0 1040 calcite 6160 -8.60 KNI-51-0 1037 calcite 6169 -8.24 KNI-51-0 1031 calcite 6189 -7.44 KNI-51-0 1028 calcite 6199 -7.90 KNI-51-0 1025 calcite 6209 -9.01 KNI-51-0 1019 calcite 6228 -9.75 KNI-51-0 1016 calcite 6238 -8.93 KNI-51-0 1013 calcite 6248 -8.47 KNI-51-0 1010 calcite 6258 -7.95 KNI-51-0 1007 calcite 6268 -9.80 KNI-51-0 1004 calcite 6278 -9.49 KNI-51-0 1001 calcite 6288 -8.38 KNI-51-0 998 calcite 6298 -9.60 KNI-51-0 995 calcite 6308 -7.86 KNI-51-0 992 calcite 6318 -8.85 KNI-51-0 989 calcite 6328 -8.83 KNI-51-0 986 calcite 6338 -8.98 KNI-51-0 983 calcite 6348 -9.50 KNI-51-0 980 calcite 6358 -9.38 KNI-51-0 977 calcite 6368 -8.20 KNI-51-0 974 calcite 6378 -8.77 KNI-51-0 971 calcite 6388 -8.33 KNI-51-0 968 calcite 6399 -8.35 KNI-51-0 965 calcite 6409 -8.93 KNI-51-0 959 calcite 6429 -7.50 KNI-51-0 953 calcite 6449 -9.23 KNI-51-0 947 calcite 6470 -8.70 KNI-51-0 944 calcite 6480 -8.81 KNI-51-0 941 calcite 6490 -8.80 KNI-51-0 938 calcite 6501 -7.99 KNI-51-0 935 calcite 6511 -6.83 KNI-51-0 932 calcite 6521 -7.74 KNI-51-0 929 calcite 6532 -8.30 KNI-51-0 926 calcite 6542 -9.54 KNI-51-0 923 calcite 6553 -8.25 KNI-51-0 920 calcite 6563 -8.21 KNI-51-0 917 calcite 6573 -7.98 KNI-51-0 914 calcite 6584 -8.32 KNI-51-0 913 calcite 6587 -9.13 KNI-51-0 910 calcite 6598 -8.45 KNI-51-0 907 calcite 6608 -9.56 KNI-51-0 904 calcite 6619 -8.00 KNI-51-0 901 calcite 6629 -9.49 KNI-51-0 898 calcite 6640 -7.12 KNI-51-0 895 calcite 6650 -9.79 KNI-51-0 892 calcite 6661 -8.52 KNI-51-0 889 calcite 6671 -8.26 KNI-51-0 883 calcite 6693 -8.42 KNI-51-0 877 calcite 6714 -8.42 KNI-51-0 871 calcite 6735 -8.94 KNI-51-0 865 calcite 6756 -9.25 KNI-51-0 859 calcite 6778 -9.05 KNI-51-0 853 calcite 6799 -8.04 KNI-51-0 851 calcite 6807 -9.59 KNI-51-0 848 calcite 6817 -9.96 KNI-51-0 845 calcite 6828 -8.99 KNI-51-0 842 calcite 6839 -9.50 KNI-51-0 839 calcite 6850 -9.78 KNI-51-0 836 calcite 6861 -8.32 KNI-51-0 833 calcite 6872 -9.32 KNI-51-0 830 calcite 6882 -7.44 KNI-51-0 827 calcite 6893 -8.59 KNI-51-0 824 calcite 6904 -8.17 KNI-51-0 821 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