Detailed correlation tiepoints for cores Sun 2-1 and SM 16 4-3 based upon clr Ca and clr (Ni + Cu + inc). DOI: https://doi.org/10.1525/elementa.2020.00150.t5
| Year . | Event . | Depth in Sun 2-1 . | Depth in SM 16 4-3 . |
|---|---|---|---|
| 2010.17 | Organic 1 | 42 mm | 16 mm |
| 2009.85 | Organic 2 | 55 mm | 47 mm |
| 2009.60 | Morakot Typhoon | 65 mm | |
| 2008.54 | Kalmaegi Typhoon | 108 mm | |
| 2005.24 | Organic 3 | 131 mm | 169 mm |
| 2000.50 | Repair of hotels | 164 mm | |
| 1999.87 | Organic 4 | 177 mm | 267 mm |
| 1999.72 | Chi-Chi earthquake | 180 mm | |
| 1996.57 | Herb Typhoon | 232 mm | |
| 1996.97 | Organic 5 | 225 mm | 355 mm |
| 1994.61 | Doug Typhoon | 262 mm | |
| 1991.34 | Organic 6 | 287 mm | 443 mm |
| 1978.67 | Organic 7 | 380 mm | 590 mm |
| 1963.69 | Gloria Typhoon | 490 mm | |
| 1960.58 | Shirley Typhoon | 538 mm | |
| 1959.59 | August 7 Flood | 550 mm | |
| 1959.25 | Organic 8 | 555 mm | 868 mm |
| 1955.78 | Organic 9 | 618 mm | 982 mm |
| 1951.86 | Organic 10 | 688 mm | 1,068 mm |
| 1934.50 | Damming | 998 mm | 1,577 mm |
| Year . | Event . | Depth in Sun 2-1 . | Depth in SM 16 4-3 . |
|---|---|---|---|
| 2010.17 | Organic 1 | 42 mm | 16 mm |
| 2009.85 | Organic 2 | 55 mm | 47 mm |
| 2009.60 | Morakot Typhoon | 65 mm | |
| 2008.54 | Kalmaegi Typhoon | 108 mm | |
| 2005.24 | Organic 3 | 131 mm | 169 mm |
| 2000.50 | Repair of hotels | 164 mm | |
| 1999.87 | Organic 4 | 177 mm | 267 mm |
| 1999.72 | Chi-Chi earthquake | 180 mm | |
| 1996.57 | Herb Typhoon | 232 mm | |
| 1996.97 | Organic 5 | 225 mm | 355 mm |
| 1994.61 | Doug Typhoon | 262 mm | |
| 1991.34 | Organic 6 | 287 mm | 443 mm |
| 1978.67 | Organic 7 | 380 mm | 590 mm |
| 1963.69 | Gloria Typhoon | 490 mm | |
| 1960.58 | Shirley Typhoon | 538 mm | |
| 1959.59 | August 7 Flood | 550 mm | |
| 1959.25 | Organic 8 | 555 mm | 868 mm |
| 1955.78 | Organic 9 | 618 mm | 982 mm |
| 1951.86 | Organic 10 | 688 mm | 1,068 mm |
| 1934.50 | Damming | 998 mm | 1,577 mm |
The underlined dates are those used to build the initial age model of Sun 2-1, and the ages of the organic-enriched layers in Sun 2-1 can be calculated by interpolation from the Ca-based chronology and then transferred to core SM 16 4-3 by correlation based on clr (Ni + Cu + inc). The ages of events are expressed in terms of Julian days in each year converted into decimal numbers for detailed fine tuning the chronology of the last 90 years.