# Eastern Coastal Adriatic 48 Year Bivalve Growth Increment Data #----------------------------------------------------------------------- # World Data Service for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program # National Centers for Environmental Information (NCEI) #----------------------------------------------------------------------- # Template Version 3.0 # Encoding: UTF-8 # NOTE: Please cite Publication, and Online_Resource and date accessed when using these data. # If there is no publication information, please cite Investigators, Title, and Online_Resource and date accessed. # # Online_Resource: https://www.ncdc.noaa.gov/paleo/study/27250 # Description: NOAA Landing Page # Online_Resource: https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/peharda2019/peharda2019zivogosce.txt # Description: NOAA location of the template # # Original_Source_URL: # Description: # # Description/Documentation lines begin with # # Data lines have no # # # Archive: Paleoceanography # # Dataset DOI: # # Parameter_Keywords: other #-------------------- # Contribution_Date # Date: 2019-07-22 #-------------------- # File_Last_Modified_Date # Date: 2019-07-22 #-------------------- # Title # Study_Name: Eastern Coastal Adriatic 48 Year Bivalve Growth Increment Data #-------------------- # Investigators # Investigators: Peharda, M.; Vilibic, I.; Black, B.; Uvanovic, H.; Markulin, K.; Mihanovic, H. #-------------------- # Description_Notes_and_Keywords # Description: Growth increment data and standardized growth chronologies for the bivalve Glycymeris pilosa from 4 locations along the Croatian coast in the eastern Adriatic. #-------------------- # Publication # Authors: Melita Peharda, Ivica Vilibic, Bryan Black, Hana Uvanovic, Kresimir Markulin, Hrvoje Mihanovic # Published_Date_or_Year: 2019-07-30 # Published_Title: A network of bivalve chronologies from semi-enclosed seas # Journal_Name: Plos ONE # Volume: 14 # Edition: e0220520 # Issue: 7 # Pages: # Report_Number: # DOI: 10.1371/journal.pone.0220520 # Online_Resource: # Full_Citation: # Abstract: Four chronologies of the bivalve species Glycymeris pilosa have been constructed along a 300 km gradient of the eastern coastal Adriatic Sea, all of which span the common period of 1982-2015. The chronologies are compared to local and remote environmental drivers suspected to influence the biology of the system, including air and seawater temperature, precipitation and freshwater discharge. The Adriatic-Ionian Bimodal Oscillating System (BiOS), a key oceanographic feature quantified by satellite-derived absolute dynamic topography, is also compared to the chronologies. The chronologies at the two southern sites are more strongly influenced by local river discharge, while the two northern chronologies are more strongly influenced by BiOS. These results highlight the broadscale importance of BiOS to the Adriatic system as well as the heterogeneity of nearshore environmental and drivers of growth. These G. pilosa chronologies provide unique multidecadal, continuous, biological time series to better understand the ecology and fine-scale variability of the Adriatic with potential for other shallow, semi-enclosed seas. #------------------ # Publication # Authors: M. Peharda, I. Vilibic, B.A. Black, K. Markulin, N. Dunic, T. Dzoic, H. Mihanovic, M. Gacic, S. Puljas, R. Waldman # Published_Date_or_Year: 2018-04-03 # Published_Title: Using bivalve chronologies for quantifying environmental drivers in a semi-enclosed temperate sea # Journal_Name: Scientific Reports # Volume: 8 # Edition: 5559 # Issue: # Pages: # Report_Number: # DOI: 10.1038/s41598-018-23773-w # Online_Resource: https://www.nature.com/articles/s41598-018-23773-w # Full_Citation: # Abstract: Annual growth increments formed in bivalve shells are increasingly used as proxies of environmental variability and change in marine ecosystems, especially at higher latitudes. Here, we document that well-replicated and exactly dated chronologies can also be developed to capture oceanographic processes in temperate and semi-enclosed seas, such as the Mediterranean. A chronology is constructed for Glycymeris pilosa from a shallow embayment of the northern Adriatic and extends from 1979 to 2016. The chronology significantly (p < 0.05) and positively correlates to winter sea surface temperatures, but negatively correlates to summer temperatures, which suggests that extreme winter lows and extreme summer highs may be limiting to growth. However, the strongest and most consistent relationships are negative correlations with an index of the Adriatic-Ionian Bimodal Oscillating System (BiOS) for which positive values indicate the inflow of the ultraoligotrophic Eastern Mediterranean waters to the Adriatic. In contrast, the substantial freshwater flows that discharge into the Adriatic do not correlate to the bivalve chronology, emphasizing the importance of remote oceanographic processes to growth at this highly coastal site. Overall, this study underscores the potential of bivalve chronologies to capture biologically relevant, local- to regional-scale patterns of ocean circulation in mid-latitude, temperate systems. #------------------ # Publication # Authors: Melita Peharda, Bryan A. Black, Ariadna Purroy, Hrvoje Mihanovic # Published_Date_or_Year: 2016-08-01 # Published_Title: The bivalve Glycymeris pilosa as a multidecadal environmental archive for the Adriatic and Mediterranean Seas # Journal_Name: Marine Environmental Research # Volume: 119 # Edition: # Issue: # Pages: 79-87 # Report_Number: # DOI: 10.1016/j.marenvres.2016.05.022 # Online_Resource: https://www.sciencedirect.com/science/article/pii/S0141113616300915 # Full_Citation: # Abstract: We evaluated the potential of Glycymeris pilosa as an environmental indicator for the Mediterranean region by applying sclerochronological techniques on a sample set collected from Pasman Channel in the middle Adriatic Sea. Maximal longevity of analyzed shells was 69 years. Growth increments in acetate peels of the hinge region had clear boundaries, and there was a strongly synchronous signal in growth-increment width among individuals. The final, replicated chronology spanned 1969 to 2013. Shell growth negatively correlated with local summer sea temperatures and positively with November precipitation. High correlation between shell growth and circulation patterns in the northern Ionian was also observed, with slower growth occurring during cyclonic regimes. Given its broad distribution in the region and the ability to crossdate, generate annually-resolved chronologies, and of a length that substantially overlaps with observational records, G. pilosa has considerable potential to test hypotheses relating to environmental variability and biological response in the Mediterranean. #------------------ # Funding_Agency # Funding_Agency_Name: Croatian Science Foundation # Grant: IP-2014-09-5747 #------------------ # Site_Information # Site_Name: Zivogosce # Location: Ocean>Atlantic Ocean>North Atlantic Ocean>Mediterranean Sea # Country: Croatia # Northernmost_Latitude: 43.1825 # Southernmost_Latitude: 43.1825 # Easternmost_Longitude: 17.29525 # Westernmost_Longitude: 17.29525 # Elevation: #------------------ # Data_Collection # Collection_Name: Peharda2019Zivogosce # Earliest_Year: 1969 # Most_Recent_Year: 2013 # Time_Unit: CE # Core_Length: # Notes: #------------------ # Chronology_Information # Chronology: # #---------------- # Variables # # Data variables follow are preceded by "##" in columns one and two. # Data line variables format: one per line, shortname-tab-variable components (what, material, error, units, seasonality, data type,detail, method, C or N for Character or Numeric data, free text) # ## age_CE age, , , year Common Era, ,paleoceanography,,,N, ## sgi growth rate,bivalve, ,dimensionless, ,paleoceanography,composited,,N,standardized growth index; annually resolved Glycymeris pilosa growth increment width chronology ## giw1 growth rate,bivalve, , micrometer, ,paleoceanography,,,N,growth increment width; Glycymeris pilosa sample 1; acetate peels of shell sections ## giw2 growth rate,bivalve, , micrometer, ,paleoceanography,,,N,growth increment width; Glycymeris pilosa sample 2; acetate peels of shell sections ## giw3 growth rate,bivalve, , micrometer, ,paleoceanography,,,N,growth increment width; Glycymeris pilosa sample 3; acetate peels of shell sections ## giw4 growth rate,bivalve, , micrometer, ,paleoceanography,,,N,growth increment width; Glycymeris pilosa sample 4; acetate peels of shell sections ## giw5 growth rate,bivalve, , micrometer, ,paleoceanography,,,N,growth increment width; Glycymeris pilosa sample 5; acetate peels of shell sections ## giw6 growth rate,bivalve, , micrometer, ,paleoceanography,,,N,growth increment width; Glycymeris pilosa sample 6; acetate peels of shell sections ## giw7 growth rate,bivalve, , micrometer, ,paleoceanography,,,N,growth increment width; Glycymeris pilosa sample 7; acetate peels of shell sections ## giw8 growth rate,bivalve, , micrometer, ,paleoceanography,,,N,growth increment width; Glycymeris pilosa sample 8; acetate peels of shell sections ## giw9 growth rate,bivalve, , micrometer, ,paleoceanography,,,N,growth increment width; Glycymeris pilosa sample 9; acetate peels of shell sections ## giw10 growth rate,bivalve, , micrometer, ,paleoceanography,,,N,growth increment width; Glycymeris pilosa sample 10; acetate peels of shell sections ## giw11 growth rate,bivalve, , micrometer, ,paleoceanography,,,N,growth increment width; Glycymeris pilosa sample 11; acetate peels of shell sections ## giw12 growth rate,bivalve, , micrometer, ,paleoceanography,,,N,growth increment width; Glycymeris pilosa sample 12; acetate peels of shell sections ## giw13 growth rate,bivalve, , micrometer, ,paleoceanography,,,N,growth increment width; Glycymeris pilosa sample 13; acetate peels of shell sections ## giw14 growth rate,bivalve, , micrometer, ,paleoceanography,,,N,growth increment width; Glycymeris pilosa sample 14; acetate peels of shell sections ## giw15 growth rate,bivalve, , micrometer, ,paleoceanography,,,N,growth increment width; Glycymeris pilosa sample 15; acetate peels of shell sections ## giw16 growth rate,bivalve, , micrometer, ,paleoceanography,,,N,growth increment width; Glycymeris pilosa sample 16; acetate peels of shell sections ## giw17 growth rate,bivalve, , micrometer, ,paleoceanography,,,N,growth increment width; Glycymeris pilosa sample 17; acetate peels of shell sections ## giw18 growth rate,bivalve, , micrometer, ,paleoceanography,,,N,growth increment width; Glycymeris pilosa sample 18; acetate peels of shell sections ## giw19 growth rate,bivalve, , micrometer, ,paleoceanography,,,N,growth increment width; Glycymeris pilosa sample 19; acetate peels of shell sections ## giw20 growth rate,bivalve, , micrometer, ,paleoceanography,,,N,growth increment width; Glycymeris pilosa sample 20; acetate peels of shell sections ## EPS growth rate,bivalve,expressed population signal , , ,paleoceanography,,,N,Glycymeris pilosa ## samp depth,bivalve, , micrometer, ,paleoceanography,,,N,sample depth; Glycymeris pilosa # #---------------- # Data: # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing_Values: NaN # age_CE sgi giw1 giw2 giw3 giw4 giw5 giw6 giw7 giw8 giw9 giw10 giw11 giw12 giw13 giw14 giw15 giw16 giw17 giw18 giw19 giw20 EPS samp 1968 NaN NaN NaN NaN 0.727 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 1 1969 NaN NaN NaN NaN 1.1345 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 1 1970 NaN NaN NaN NaN 1.107 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 1 1971 NaN NaN NaN NaN 0.816 NaN NaN 0.94 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 2 1972 NaN NaN NaN NaN 1.1529 NaN NaN 1.0415 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 2 1973 NaN NaN NaN NaN 1.0333 NaN NaN 0.8078 NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN NaN 2 1974 NaN NaN NaN NaN 1.3525 NaN NaN 1.2169 NaN NaN NaN NaN NaN NaN 1.2116 NaN NaN NaN NaN NaN NaN 0.9178 3 1975 NaN NaN NaN NaN 0.889 NaN NaN 0.7725 NaN NaN NaN NaN NaN NaN 0.8213 NaN NaN NaN NaN NaN NaN 0.8769 3 1976 NaN NaN NaN NaN 1.2288 NaN NaN 1.0643 NaN NaN NaN NaN NaN NaN 1.1361 NaN NaN NaN NaN NaN NaN 0.791 3 1977 NaN NaN NaN NaN 1.1131 NaN NaN 1.0013 NaN NaN NaN NaN NaN NaN 1.015 NaN NaN NaN NaN NaN NaN 0.7907 3 1978 NaN NaN NaN NaN 1.0336 NaN NaN 1.1913 NaN NaN NaN NaN NaN NaN 1.2766 NaN NaN NaN NaN NaN NaN 0.6329 3 1979 NaN NaN NaN NaN 0.6414 NaN NaN 0.9521 NaN 0.7674 NaN NaN NaN NaN 0.8517 NaN NaN NaN NaN NaN NaN 0.6601 4 1980 NaN NaN 0.8188 NaN 1.1231 NaN NaN 1.3174 1.1542 1.4127 NaN NaN NaN NaN 0.7848 NaN NaN NaN NaN NaN 1.6805 0.7126 7 1981 NaN NaN 0.7904 NaN 1.1204 0.7115 NaN 1.2133 0.6641 1.2409 NaN NaN NaN NaN 0.7161 NaN NaN NaN NaN NaN 0.654 0.8747 8 1982 0.904 NaN 0.9836 NaN 0.8647 0.9004 0.9651 0.8046 1.0553 0.6797 NaN NaN 1.0211 NaN 0.8774 NaN 0.8693 NaN 0.9304 NaN 0.8669 0.9141 12 1983 1.173 NaN 1.2254 NaN 1.0396 1.062 1.2997 1.1236 1.2466 1.0112 NaN NaN 1.2019 1.1924 1.1335 NaN 1.1247 NaN 1.2651 NaN 1.2376 0.8888 13 1984 0.807 NaN 0.8763 NaN 0.5412 1.0728 0.7786 0.8423 0.929 0.5857 NaN NaN 0.8115 0.9025 0.7287 NaN 0.8761 NaN 0.762 NaN 0.7148 0.9276 13 1985 0.745 NaN 1.0116 NaN 0.6965 0.9824 0.5815 0.6638 0.746 0.6766 NaN NaN 0.7224 0.5998 0.7438 NaN 1.042 NaN 0.9075 NaN 0.6685 0.9699 13 1986 1.052 NaN 1.3385 1.1967 0.7693 1.1142 0.8527 1.0674 1.0407 1.292 NaN NaN 1.1636 0.7069 1.0854 NaN 0.99 NaN 1.0128 NaN 1.0177 0.9632 14 1987 1.15 0.9476 1.2044 0.8652 1.002 1.3399 1.3424 1.0287 1.4637 1.3293 NaN 1.0318 1.1481 1.1903 1.2114 NaN 1.3548 NaN 0.95 NaN 0.9777 0.9606 16 1988 0.821 0.7137 0.8708 0.8953 0.6982 0.8137 0.7846 0.7502 0.821 0.7289 0.8172 0.9556 0.7545 0.843 0.8696 0.74 0.6046 0.8751 0.9452 NaN 0.9749 0.9634 19 1989 1.012 0.9438 1.0726 0.8529 1.121 1.2145 1.2158 0.8533 0.615 0.9889 0.911 1.0606 0.938 1.103 1.0784 0.9259 1.0091 0.9736 0.9893 NaN 1.1156 0.9356 19 1990 1.194 1.2124 1.2506 1.0377 0.9878 0.8778 1.2143 1.0504 1.4208 1.4286 1.2873 0.8964 1.2947 1.3442 1.2945 1.2642 0.9766 1.1996 1.1142 NaN 1.2599 0.9293 19 1991 1.153 0.874 1.0776 1.1305 1.143 1.2738 1.3233 1.1173 1.0895 1.1752 0.739 1.099 1.1673 1.2889 1.0417 1.1098 1.2414 0.7231 1.1274 NaN 1.1636 0.9229 19 1992 1.032 0.9717 0.9509 0.9723 0.878 1.1382 1.1919 1.0272 1.0421 1.1091 1.0383 0.9751 1.0931 1.0151 1.1907 0.9618 0.9737 0.9845 1.2174 NaN 1.0231 0.8427 19 1993 1.08 1.2545 0.8945 0.93 0.9507 1.3128 1.1925 1.2272 0.9458 1.0001 1.349 0.8988 0.9386 1.267 1.0399 1.1276 1.0547 1.3824 1.1647 0.9904 0.7153 0.846 20 1994 1.031 1.1326 0.9237 1.0791 1.1822 1.1017 1.0201 1.0453 1.1297 1.0562 1.0666 1.1009 0.9071 0.8741 0.9809 0.9845 0.8973 1.0787 1.0869 0.9696 1.0511 0.7824 20 1995 0.91 0.9442 1.0058 0.7373 1.1547 0.871 0.7489 0.821 0.7011 1.0568 0.9707 0.6825 0.8156 1.1125 1.0647 0.9498 0.985 0.9322 0.8492 0.8279 1.066 0.7576 20 1996 1.118 1.465 1.1376 1.1718 1.1572 1.1029 1.127 1.1331 1.0217 1.1074 0.9308 1.1721 0.8234 1.1347 1.2854 1.0892 1.1538 0.8443 1.0809 1.0779 1.0568 0.7736 20 1997 1.014 1.2194 0.8346 1.2061 1.2869 0.5993 1.0568 1.0518 1.0288 0.8693 1.0323 1.196 0.8476 0.8703 1.1099 0.9365 1.1312 1.0621 1.0127 1.1182 0.8369 0.9133 20 1998 0.971 1.0599 0.8316 1.0792 0.956 0.9949 0.8204 0.8881 0.8302 0.927 0.9101 1.062 1.0519 1.0494 1.0277 1.1948 0.9465 0.9957 0.8757 1.4656 1.0197 0.9141 20 1999 1.105 1.2001 1.1523 1.1705 1.3287 0.6097 0.8851 1.0303 0.749 1.0303 1.1515 1.0891 1.1596 1.3129 1.1631 1.1087 1.054 1.2402 0.9518 0.9691 1.0852 0.9178 20 2000 0.813 0.6766 0.9271 0.7351 0.932 0.818 0.6532 0.8767 0.5586 0.7247 0.8598 0.8622 0.9291 0.9684 0.6282 0.9124 0.9899 0.8262 0.7818 0.6589 0.8919 0.8845 20 2001 1.051 0.9503 1.0841 1.2651 1.2567 0.8571 0.7583 1.0886 1.0316 1.1494 1.109 1.1664 1.1167 0.7877 1.2221 0.8674 1.1031 1.0271 1.0335 1.0325 1.0366 0.87 20 2002 0.884 0.9835 0.9965 0.6858 0.9251 0.8614 0.7407 0.8838 0.9827 0.9567 1.038 0.6035 1.0084 0.8366 1.0771 0.8012 0.8899 0.76 0.7956 0.8408 1.0197 0.8831 20 2003 0.905 0.7628 0.7317 0.7282 1.2539 0.832 0.7502 1.1582 1.0146 0.8897 0.7413 0.8612 1.2575 0.5466 0.7703 0.8028 1.0773 1.0676 1.0075 1.0302 0.9567 0.9029 20 2004 0.921 0.8845 0.5497 1.0578 0.7385 0.9754 1.0515 1.0009 0.9476 0.9682 0.9435 1.0555 1.2048 0.7831 0.6123 1.225 1.0122 0.9421 0.9634 0.7021 0.631 0.8396 20 2005 1.017 1.0385 1.0036 1.2218 1.1213 0.9796 0.894 0.9823 0.9092 1.0618 1.0755 1.1668 0.7863 0.9417 0.8739 1.0767 1.0125 1.1534 0.9108 1.0439 1.1454 0.8506 20 2006 1.103 0.8002 1.1729 1.2966 1.1056 1.2013 0.9241 1.1157 1.2361 1.129 1.186 1.2011 0.9872 1.1128 1.091 1.0865 0.9951 1.1528 0.9961 1.1151 1.0288 0.909 20 2007 1.026 0.859 1.0492 1.3037 0.9664 1.0551 1.0224 1.057 1.0633 0.9342 1.1586 1.3418 1.0618 0.9151 0.9123 1.003 0.8123 1.1122 1.1039 1.0657 0.9545 0.9355 20 2008 1.073 1.114 1.1996 1.0923 0.9817 1.2171 1.0894 1.2134 1.1445 1.0832 1.0054 1.0878 0.8839 1.0431 1.05 0.932 0.7861 1.0221 0.9899 1.1542 1.2312 0.9527 20 2009 0.821 0.7788 1.0012 0.4491 0.7432 0.7639 0.7732 0.5306 0.881 0.878 1.0223 0.5379 0.8622 0.9367 0.7463 0.841 0.6078 0.8783 0.7991 1.047 0.8828 0.9531 20 2010 0.804 0.5921 0.8322 0.6435 0.7514 0.9994 0.9832 0.6102 0.9291 1.039 0.5515 0.657 0.7769 0.5866 0.9066 0.8641 0.7245 0.6819 0.9798 0.9557 0.866 0.9368 20 2011 1.056 1.0265 0.7712 1.0955 1.1073 1.1084 1.1824 1.0637 1.2889 1.0149 0.9107 1.1402 1.1913 1.1885 1.0343 0.9242 0.9706 0.9099 1.0502 0.9929 1.0132 0.9382 20 2012 1.006 0.9467 1.1273 0.9326 1.1143 1.0982 1.1205 1.1771 1.1467 1.0378 0.8514 0.9048 1.1304 1.2362 0.8991 1.0049 0.7818 0.8426 0.9959 0.8034 0.9038 0.9466 20 2013 0.99 0.9003 0.9555 0.8675 0.5497 1.092 0.939 0.9606 0.9666 0.9 1.0148 0.9492 0.8913 1.1839 1.0092 0.9232 1.1075 0.9635 1.0127 1.003 1.1695 0.9197 20 2014 1.105 1.3749 1.0258 1.2026 1.0489 1.0097 1.2537 1.1217 1.0641 0.8158 0.968 1.0773 1.0522 1.1465 1.1842 1.23 1.3392 1.0206 1.0506 1.051 1.0785 NaN 20 2015 1.187 1.1558 1.1688 1.0787 1.4496 1.0562 1.0679 0.9277 1.1359 1.1955 NaN NaN 1.2417 1.1202 1.3125 1.1026 1.168 1.0715 1.117 NaN NaN NaN 18