@Article{egusphere-2026-3515,
AUTHOR = {Lyle, M. and Olivarez Lyle, A.},
TITLE = {Why does the Northwest Pacific Ocean (Kamchatka Margin) have a different carbonate time series than the rest of the Pacific? Regional carbonate production is greater than deep Pacific dissolution at the start of interglacials},
JOURNAL = {EGUsphere},
VOLUME = {2026},
YEAR = {2026},
PAGES = {1--27},
URL = {https://egusphere.copernicus.org/preprints/2026/egusphere-2026-3515/},
DOI = {10.5194/egusphere-2026-3515}
}